DIR Return Create A Forum - Home
---------------------------------------------------------
FUNDAY
HTML https://funday.createaforum.com
---------------------------------------------------------
*****************************************************
DIR Return to: Updates
*****************************************************
#Post#: 235--------------------------------------------------
Mathis on Velikovsky +
By: Admin Date: December 16, 2018, 6:51 pm
---------------------------------------------------------
1. Mathis on Velikovsky
HTML http://funday.createaforum.com/mike-messages/1-110/msg235/#msg235
2. Youthful Atmosphere of Venus
HTML http://funday.createaforum.com/mike-messages/1-110/?message=237
3. Nature of Venus' Heat
HTML http://funday.createaforum.com/mike-messages/1-110/?message=238
4. Surface Of Venus -- "A Newborn Babe"
HTML http://funday.createaforum.com/mike-messages/1-110/?message=239
5. Evidence for the Extreme Youth of Venus
HTML http://funday.createaforum.com/mike-messages/1-110/?message=240
6. CutFog Forum Discussion
HTML http://funday.createaforum.com/mike-messages/1-110/?message=332
Paraphrasing + Comments on Miles' recent paper, Beyond
Velikovsky, at
HTML http://milesmathis.com/vel2.pdf
(Vel. means
Velikovsky.)
_MM -- Vel. is from prominent Jewish families who faked all
recent history, their modus operandi being to tell only as much
truth as a project will bear, so where the truth ends,
misdirection begins.
_MM -- The intent of Worlds in Collision is "eyes-off", which is
to give a partial reading of data to prevent a fuller reading,
like Robin Gardiner's Titanic project, which misdirected
attention from Lloyd's of London, Astor et al, and the Titanic
never sank at all. (LK -- Did the Olympic sink in its place?)
_MM -- Vel. claims Venus was ejected from Jupiter, then appeared
as a comet and came close to Earth before settling into its
present orbit. (LK -- And he said Venus is hot because it's a
new planet.)
_MM -- The mainstream doesn't admit that Venus must have
recently experienced a catastrophe; Venus and its spin are very
round, so there was no collision, but maybe a close pass with
Earth or another body.
_MM -- Vel. admits all planets have excess heat, but he gives
the wrong reason; it's because Venus' poles and/or spin are
reversed, causing a magnetic effect that spins incoming photons
up in polar through-charge, causing more heat, and Venus' spin
will reverse and go in the same direction as other planets, but
it takes a long time for the Sun's charge field to reverse the
spin of such a large planet.
_MM -- Vel. is wrong about Venus nearly colliding with Earth,
because Earth did not heat up significantly, but only suffered
darkness and other minor changes, and he's wrong about Venus'
heat coming from recent formation and the mainstream is wrong
about the greenhouse effect, because as Vel. said, thick
Venusian clouds would block solar heat, causing cooling, not
heating, and Venus reflects most of the light it receives, which
also prevents heating.
_MM -- In reality Venus' heat comes up from below via the charge
field. (LK -- But the charge field comes from the Sun, doesn't
it, which means it comes from above, not below? If Venus were
newly formed, as Vel. said, its heat would come up from below.
It seems more likely that Venus was heated some other way. Maybe
the flipping of its axis heated it at least partly. Talbott and
Cardona thought Venus, Mars and Earth were formerly satellites
of Saturn, that Saturn was a brown dwarf star that flared as a
nova, and Venus was closest to Saturn, so the nova may have
heated Venus too.)
_MM -- The mainstream avoids seriuosly discussing why Venus'
data is so unusual; evidence indicates Venus has flipped its
axis recently, but Miles can't yet calculate how recently. (LK
-- Catastrophists have discussed this and have shown that the
present rate of heat loss on Venus indicates that it should cool
to normal levels within a few centuries or millennia.)
_MM -- It's unlikely that, as per Vel., Venus was ejected from
Jupiter as a comet. (LK -- I think Vel. thought Jupiter's Great
Red Spot could have been the birthplace of Venus. John Ackerman
still thinks so. I think that's unlikely, but I recently noticed
this article: An exoplanet loses its atmosphere in the form of a
tail
HTML https://phys.org/news/2018-12-exoplanet-atmosphere-tail.html
.
So, even if Venus wasn't ejected from Jupiter as a new planet,
it seems entirely plausible that it could have looked like a
comet, if it lost some of its atmosphere in the form of a tail.
Mythology around the world says Venus was a comet, which is
where Vel. got the idea. And it's likely that Earth lost much of
its atmosphere recently too, because large land animals needed
the extra buoyancy in order to move under the present gravity
conditions. And dinosaur bones have been C14 dated to only tens
of thousands of years, not millions.)
_MM -- It's also unlikely that Venus was ejected as a moon from
the Jupiter or Saturn systems (LK -- or others), because the
present moons of those systems would still be in turmoil. (LK --
That depends on how long it takes orbits to normalize. Iapetus
has a 2 million mile radius orbit around Saturn inclined at
nearly 16 degrees from Saturn's equatorial plane. Dust, gases
and ions earlier in the systems may have caused the
circularization of orbits much quicker than without that debris.
The same applies to Venus' orbit circularization.)
_MM -- Bode's law corrected explains that smaller planets should
orbit nearer than large ones, thus Saturn (LK -- etc) tends to
move below Jupiter's orbit (LK -- and Mars below Earth's).
_MM -- The asteroid belt was likely caused by close planetary
encounters in that way, and a similar recent encounter likely
involved Venus moving from a farther orbit past Earth to its
present orbit and flipping on its axis while passing.
_MM -- Mars was probably involved in the asteroid belt event, as
it's close to the belt, and there's plenty of room above Earth's
orbit for Venus to have come from there, and Mars appears to be
moving toward the gap that Venus left.
_MM -- The moon of Mars is getting closer to it because Mars is
moving inward, while Earth's Moon is moving farther from Earth
because Earth is moving outward and Earth's period was likely
shorter. (LK -- Some ancient records say it was 360 days.)
_MM -- Venus and Earth did not dance together in Biblical times,
but they may have much earlier. (LK -- Talbott and Cardona
independently concluded that indeed the encounter between Earth
and Venus was at least a thousand years earlier than Vel.
thought and was not mentioned in the Biblical record. I think
they expressed perplexity as to how Vel. concluded that Venus
was involved in the plagues of the Exodus event.)
_MM -- The Moon may have previously orbited Venus, or it may
have been on the far side of Earth as Venus passed etc. (LK --
Some ancient records seem to say Earth initially had no Moon.)
_MM -- Vel. was likely misdirecting readers away from evidence
of the photonic charge field. (LK -- I don't know if the ruling
class's experts knew about the charge field then, in 1950. Vel.
and his successors, Thunderbolts, have favored electrical forces
as having major effects. I'm not sure yet that Vel. was trying
to misdirect. It's possible, but I need better evidence. I know
some of the Thunderbolts people and it seems they just haven't
been able to follow Miles' explanations well enough. Some of
their forum members like many of Miles' ideas, including me, and
we discuss them there sometimes. But I'm open-minded on whether
there has been intentional misdirection.)
_MM -- Thunderbolts is claiming that there are no photons. (LK
-- I haven't heard that. I'd say most of them consider photons
as massless. If they've said there are no photons, I'd like to
see where they say that. On this page
HTML https://www.thunderbolts.inf
o/wp/2011/09/02/essential-guide-to-eu-introduction/
they say: "Electric fields are detectable in two ways: when
they accelerate electrons, which emit observable photons as
synchrotron and Bremsstrahlung radiation, and by accelerating
charged particles as electric currents which are accompanied by
magnetic fields, detected through Faraday rotation of polarized
light." So I think Miles needs to correct the statement.)
_MM -- The governors wanted to keep the charge field secret,
except for a few military scientists. (LK -- That would be more
plausible if there's evidence that military scientists have done
anything that would likely have only been possible if they knew
about the charge field.)
_MM -- Vel. followed the pattern of Ignaeius Donnelly who also
divulged a lot of good data, but then blackwashing it. (LK --
I'm interested in what data was blackwashed.)
_MM -- By burying the data from both of them, the governors
squelched discussion and research. (LK -- That's very plausible,
that they intended to make anyone who discussed such subjects
pariahs. However, they could have done that even if Vel. and
Donnelly were not controlled opposition.)
_MM -- To keep control of science, they had to keep everyone in
the gravity-only, math-based, relativity/QED fog; if the average
scientist understood the charge field, a real revolution would
have been quick.
_MM -- Vel. was wrong on specifics, but right in general, e.g.
(LK -- cataclysmic) events weren't caused by Venus, since it
passed Earth earlier, but they may have been caused by comets,
asteroids and meteors, even according to his evidence.
_MM -- Vel's theory that Venus and later Mars caused the
cataclysms is fanciful and unnecessarily complicated. (LK --
Thunderbolts tries to interpret the mythological records
accurately and they do seem to indicate that Venus and Mars were
inner moons of Saturn, which eventually destabilized and the
pair caused some havoc in the inner solar system, not
necessarily directly on Earth.)
_MM -- Vel. was paid to blackwash the truth, i.e. the charge
field, ancient texts, amateur scientists and the public. (LK --
Maybe, but the evidence seems slim, and it seems that Vel.
believed in what he found, and I don't know of evidence that
anyone else guided or controlled him. He claimed that he made
his discovery about Venus etc in 1939, I think, when he had the
theory that Moses, not Akhenaten, was the original monotheist.)
_MM -- Before WW2 the public had considerable knowledge of
science, but less and less thereafter.
_MM -- The Vel. affair pre-blackwashed Miles' findings with help
from Thunderbolts. (LK -- Miles said almost nothing is said
about Thunderbolts this time. I wouldn't be surprised if some of
the moneyed supporters of Thunderbolts are working for the
governors, but I'd be very surprised if Talbott, Thornhill,
Scott, Cochrane, Cardona, van der Sluijs and others are working
for them.)
_MM -- The governors weren't prepared for someone like Miles,
because his methods are unprecedented and he has taken advantage
of their own tools, like the internet. (LK -- I'd like to know
how Miles was educated. There's an organization called the
Institutes for the Advancement of Human Potential, which found
that almost all kids have genius potential, and they've been
trying to help parents learn how to help their kids develop that
potential. So I think genius would be common if society would
learn how to develop it, like IAHP teaches.)
#Post#: 237--------------------------------------------------
Re: Mathis on Velikovsky +
By: Admin Date: December 24, 2018, 5:53 pm
---------------------------------------------------------
The Youthful Atmosphere of Venus [Aeon Journal]
From: Aeon I:6 (1988)
_The Youthful Atmosphere Of Venus, Charles Ginenthal
_In Worlds in Collision Immanuel Velikovsky claimed that Venus
is a new planet. (1) Analysing mythological and historical
evidence, Velikovsky concluded that less than ten thousand years
ago Venus was expelled from the gas giant Jupiter, roamed the
solar system as a comet, nearly collided with the Earth around
1500 B.C., and only later settled into its present, highly
circular orbit. While subsequent research by other
catastrophists has raised questions about certain specifics of
Velikovsky's theory, this research has, on the whole, only
reinforced Velikovsky's original and most fundamental claim that
Venus appeared in historical times as a comet. Velikovsky's
thesis concerning Venus' recent birth and cometary past can be
tested against considerable evidence gathered since the thesis
was first published in 1950. Among other things, it implies
that-- contrary to the expectations of astronomers-- the
atmosphere of the planet should exhibit evidence of extreme
youth. In this paper I will show that a great deal of
"surprising" data indicates that Venus' atmosphere is that of a
very young planet; in fact, according to previously accepted
tests, this atmosphere suggests the planet has been in existence
far less than four eons. In 1985 Lawrence Colin stated flatly:
"The chemical composition of the air [of Venus remains the most
controversial aspect of our knowledge of the Venusian
atmosphere." (2) As will be shown, the reason for the
controversy is that the data simply do not fit the conventional
model.
_ABUNDANCE OF SULPHURIC ACID
_In the course of a decades-long debate, one of the most
often-cited arguments raised against Velikovsky has involved the
finding that the clouds of Venus are composed of sulphuric acid.
Extrapolating from historical sources, Velikovsky himself had
anticipated a dominance of hydrocarbons, something which has not
found support in the new data. But the more recent discoveries
raise entirely new questions. One that has yet to be answered
satisfactorily is this: can sulphuric acid remain stable in the
atmosphere of Venus over the time required by the usual models
of the planet's history? Peter R. Ballinger, a researcher in
organic chemistry, raised this question in 1965, when he wrote:
It is likely that sulphuric acid would be gradually decomposed
by solar radiation of ultraviolet and shorter wavelength,
particularly in the presence of iron compounds... to give
hydrogen and oxygen. This process would also be expected to
result in the preferential retention of deuterium, as discussed
in another context... Because of this and and other chemical
reactions, sulphuric acid might well have a relatively short
lifetime, consistent with a recent installation of the planet in
its present orbit. (3) There is indeed iron in the Venusian
atmosphere, as reported in Science in 1979. (4) And if the
prevailing sulphuric acid model of the clouds is accepted, Venus
could not be 4.6 billion years old: solar radiation would have
long ago decomposed its sulphuric acid. Hence, the very presence
of sulphuric acid is telling evidence of a recently-constituted
atmosphere.
_NOT ENOUGH CARBON MONOXIDE
_Ballinger noted in passing that there were "other chemical
reactions" indicating the same result, and these too are of
significance. It is known that ultraviolet rays break down
carbon dioxide into carbon monoxide and oxygen molecules, O 2-
Once these molecules of carbon monoxide and O 2 form, they do
not recombine again easily. Since Venus' atmosphere is about 97
percent carbon dioxide, one would expect to find a great deal of
carbon monoxide and oxygen in the upper and middle atmospheric
layers of Venus. This would be so especially if Venus is
billions of years old. Thus U. von Zahn et al., emphasised this
very problem when they wrote-- The central problem of the
photochemistry of Venus' middle atmosphere is to account for the
exceedingly low abundance of CO [carbon monoxide and O 2
[molecular oxygen observed at the bottom of the middle
atmosphere. In fact, O 2 has not been detected even at 1 ppm
[part per million level. Due to low abundance Of O 2 and O 3
[ozone which absorbs ultraviolet radiation solar ultraviolet of
sufficient energy to photolyse CO 2 penetrates down to 65 km [or
39 miles above the surface of Venus. The 3-body recombination
reaction with a rate constant K b [based on temperature is,
however, spin-forbidden. Consequently, at typical temperatures
of the Venus middle atmosphere (200K) this [recombination
reaction has a very small rate...[But at this temperature oxygen
is convened to molecular oxygen...with a rate constant K c which
is 5 orders of magnitude higher than K b. Neglecting for a
moment the effect of trace gases in Venus' atmosphere, CO 2, CO
and O 2 are nonreactive with each other and we therefore expect
a fairly rapid transition (on geologic time scales) of the CO 2
atmosphere to one dominated by CO and O 2, CO 2 would disappear
from the upper atmosphere within a few weeks and from the entire
middle atmosphere in a few thousand years. Indeed these
arguments describe the situation correctly for the upper
atmosphere of Venus, provided we take account also the various
dynamic processes exchanging gas between the upper and middle
atmosphere. The above arguments, however, fall short in
explaining the composition of the middle atmosphere which at
least close to its lower boundary is characterised by an extreme
dearth of CO 2 photolysis [break down that is CO and O 2. (5)
There is at present no observed or reasonably deduced process to
explain this situation. So there is an interesting dilemma for
conventional theorists. In order for the abundance of carbon
dioxide to persist in the middle atmosphere of Venus, the planet
must be only a "few thousand years" old.
_ABSENCE OF WATER
_Velikovsky pointed out long ago that Venus contains practically
no water in its atmosphere. Andrew and Louise Young reported in
1975 that studies at radio wave lengths "have established once
again that there is no more than .1 or .2 percent water vapour
in the lower atmosphere, and the true value is probably close to
.01 [l/l00 of a percent. The cloud tops are drier still." (6)
But if Venus went through the same early evolution as the Earth
billions of years ago, it should have, over time, out-gassed an
ocean of water at least comparable to that of the Earth. Young
and Young tell us that, "If one assumes that Venus once had as
much water as the earth has now, it is necessary to explain how
all but one part per million of it was lost. There is a known
mechanism by which a planet with abundant water could lose a
large portion of it: Water vapour in the upper atmosphere could
be dissociated by ultraviolet radiation and the hydrogen could
be lost to space, either by thermal escape or through the
influence of the solar wind. That effect however could not
produce an atmosphere so thoroughly desiccated as Venus' is. Of
the water Venus has today, very little reaches the upper
atmosphere and therefore it is not dissociated; at the present
rate Venus would not have lost a significant amount [of water in
the history of the solar system." (7) Venus has either lost
water inexplicably, or it has simply not yet had time to
generate the abundance of atmospheric and surface water the
conventional models would predict (over the assumed billions of
years). The presently accepted notion for the development of
oceans is the "outgassing hypothesis" presented by W. W. Rubey
in 1951. The hypothesis is based on the fact that gases expelled
by volcanoes and hot springs contain steam, carbon dioxide,
nitrogen and carbon monoxide. It is believed that this process,
operating throughout the 4.6 billion year history of the Earth,
can account for major atmospheric constituents of the earth.
Also, the depth of the oceans would, under this process,
steadily increases over the eons. If this is so, even if Venus
had lost its first atmosphere and oceans, say 3 or 4 billion
years ago (after the first atmosphere and water of the planet
were removed by the solar wind and a new atmosphere of carbon
dioxide had baked out of the surface rock), then outgassing
during the subsequent 3 or 4 billion years would have produced a
new ocean of shallower depth. Protected by the new, dense
atmosphere, this ocean would not have escaped from the planet.
Thus Lawrence Colin tells us: "Overwhelming evidence suggests
that in its past Venus had much more water, perhaps as much as
the Earth today-- a whole ocean." ( 8 ) The same question is
asked by Kelly J. Beatty in an article titled "Venus: the
Mystery Continues." Beatty wonders, "Where has all of Venus'
water gone? Theorists have asked this question for years. It
doesn't make sense to them that a planet so like the earth in
size and distance from the sun should have 10,000 to 100,000
times less water. After all, the pair have comparable amounts of
carbon dioxide and nitrogen, so the water was probably there at
the outset but has somehow disappeared." (9) What ever water
Venus possessed was apparently burned off when Venus was a
stupendously hot, brilliant comet. The established view, holding
that Venus is as old as the Earth, requires enormous amounts of
water vapour in its atmosphere. Why, then, is the required water
missing? If, as Velikovsky claimed, Venus is a new planet, then
it has not had time to outgas sufficient water vapour into the
atmosphere and therefore it should have very little, or
practically none. In fact, if the amount of Venusian water is
one-one hundredth of one percent of Earth's (the "more likely"
estimate of Young and Young), then holding that Venus is as old
as the Earth, requires enormous amounts of water vapour in its
atmosphere. Why, then, is the required water missing? If, as
Velikovsky claimed, Venus is a new planet, then it has not had
time to outgas sufficient water vapour into the atmosphere and
therefore it should have very little, or practically none. In
fact, if the amount of Venusian water is one-one hundredth of
one percent of Earth's (the "more likely" estimate of Young and
Young), then Venus could be no older than 10,000 to 20,000
years.
_MISSING OXYGEN
_An added problem is the dearth of oxygen in Venus' atmosphere,
a condition inexplicable under the present view that Venus is an
ancient planet. Eric Burgess in his book, Venus an Errant Twin,
informs us that the missing oxygen is vital to the question of
what happened to the water: "If water molecules were broken down
into hydrogen and oxygen, the disappearance of the oxygen has to
be explained, since very little of this gas is present in the
atmosphere today. No completely satisfactory explanation is yet
available for what happened to the oxygen." (10) This particular
dilemma is aggravated by the problem of photodissociation of
carbon dioxide into carbon monoxide and oxygen discussed
earlier, and also by the photodissociation of sulphuric acid
into hydrogen and oxygen. If Venus' atmosphere is ancient,
photodissociation of water (into oxygen and hydrogen) in
conjunction with photodissociation of carbon dioxide (into
carbon monoxide and oxygen) and sulphuric acid (into water and
hydrogen) should have given Venus an abundant supply of oxygen.
However, if Venus is extremely young the absence of oxygen from
its atmosphere is fully explained. Perhaps a brief analysis of
the evolution of the Earth will make this concept clearer. It is
generally held by both geophysicists and biologists that our
planet's primitive atmosphere lacked oxygen. The reason is the
well known chemical fact that oxygen would have been fatal to
any incipient life forms emerging during Earth's early history.
Jeremy Rifkin gives this overview of the principle: To begin
with, most scientists agree that life could not have formed in
an oxygen atmosphere. If the chemicals of life are subjected to
an oxidising atmosphere, they will decompose into carbon
dioxide, water, and nitrogen. For this reason it has long been
assumed that the first precursors of life must have evolved in a
reducing [oxygen free atmosphere, since an oxidising atmosphere
would have been lethal. (11) From this reasonable principle it
follows that, if Venus is a young planet, it should lack
appreciable oxygen-- as, in fact, it does. The historical
implication is quite clear and points unambiguously to the novel
concept first set forth by Velikovsky.
_HYDROCHLORIC AND HYDROFLUORIC ACID
_In his well-known attempts to discredit Velikovsky's theory of
a former cometary Venus, Carl Sagan has stated that the
sulphuric acid cloud model for Venus, "is consistent with the
chemistry of the Venus atmosphere, in which hydrofluoric and
hydrochloric acid have also been found." (12) What Sagan did not
mention is that these acids, when they react with rocks, are
quickly neutralised. Thus these gasses, interacting with new
(volcanic) surface rock, should have been completely neutralised
over its four to six billion year history. Young and Young
report that-- Among the more exotic materials proposed for the
clouds only one has been detected spectroscopically. It is
hydrogen chloride, and it was found along with hydrogen fluoride
by William S. Benedict of the University of Maryland in the
spectra reported by the Connesses. Both gases are highly
corrosive; when they are dissolved in water, they yield
hydrochloric acid and hydrofluoric acid. Their abundance is too
low for them to be the clouds, but that they should be present
in the atmosphere at all is a surprise. (13) The chart supplied
by Young and Young shows hydrochloric and hydrofluoric acid
moving to and from the surface of Venus. It is clear, therefore,
that these acids interact with the surface rock. The authors go
on to say, "Such strong acids could not survive for long in the
Earth's atmosphere; they would react with rocks and other
materials and soon be neutralized." (14) The amount of water
vapour in the Venus atmosphere, though small, is sufficient to
convert hydrogen floride and hydrogen chloride into acids. It is
therefore assumed ad hoc that the high temperature cooks
hydrogen chloride and hydrogen fluoride out of the surface rock.
But this theory assumes that these gases would not be
neutralised as they formed acids in the rocks. As stated by
Young and Young, "A number of assumptions are implicit in this
hypothesis: that the rates of chemical reactions at the surface
are high, that the atmosphere and the surface are in chemical
equilibrium and that the effects of circulation in the
atmosphere are small enough to be neglected." (15) Perhaps with
enough "ifs" one can fit anything into the gradualist picture of
Venus' atmosphere and surface. But if one or more of these ad
hoc explanations is incorrect (and out of three variables this
is quite probable) then there is no accounting for the existence
of these gases in Venus' atmosphere-- apart from the possibility
that a very youthful Venus has not had sufficient time to
neutralise them. Issues such as noted above must be addressed
alongside other considerations pointing in the same direction.
Anthony Feldman informs us of a "recent discovery about the
composition of the Venusian atmosphere [which has cast doubt on
the popular theory accounting for the formation of the solar
system." He writes-- The innermost planets-- Mercury, Venus,
Earth and Mars-- are thought to be small and rocky because the
sun drew their light constituents away. If this idea is correct,
the closer a planet is to the sun the less likely there is to be
lighter gases in the atmosphere. But in the atmosphere of Venus
the opposite is true. In particular, there seems to be 500 times
as much argon gas and 2700 times as much neon as in the
atmosphere of Earth. So far scientists cannot explain why these
gases were not drawn away from the planet during the birth of
the solar system...Further discoveries about Venus may soon
force a revision of the most basic ideas about how the Sun and
the planets were formed. (16) Feldman's remarks are specifically
corroborated by the finding of argon-36 in Venus' atmosphere.
Dr. Michael McElroy, a scientist involved with Pioneer
spacecraft exploration of Venus, is quoted in the Washington
Post as stating, "The atmosphere of Venus contains as much
argon-36 as you would expect from a planet's original
atmosphere." (17) Here, then, is another piece of evidence which
Velikovsky's critics have let slip under the rug. This
evidence-- together with the principles of photodissociation of
sulphuric acid and of carbon dioxide, the extreme dearth of
water vapour, the extreme dearth of oxygen, and the
unneutralised hydrochloric and hydrofluoric acid-- point in
unison to the youth of Venus' atmosphere and provide dramatic
support for Velikovksy's claim that Venus is a new planet.
_FRESHLY STREWN ROCK
_Yet still other lines of evidence are available. Since Venus is
supposedly as ancient as Earth and has an atmosphere of highly
corrosive gases, most of its surface rocks should show erosion.
Eric Burgess informs us that "the rocks of Venus undergo
different types of weathering. Chemical weathering would be
expected to decompose olivines, pyroxenes, quartz and feldspars
into magnesite, tremolite, dolomite and sulphides and sulphates.
Mechanical weathering would be expected to disintegrate rocks by
spalding and preferential chemical weathering and possibly by
wind erosion. "Although winds on Venus near the surface do not
blow at high velocity they represent the movement of extremely
dense air by terrestrial standards, sufficiently dense to move
particles up to several millimetres diameter across the surface
of Venus." (18) Needless to say, these winds, operating over
great spans of time, should have drastically eroded surface rock
materials and blown the resulting debris into basins, forming
vast sand dunes. To the contrary, however, Burgess tells us that
"the radar data are...inconsistent with Venus being covered by
vast areas of windblown debris." (19) Just how rapidly do the
winds blow on Venus? Isaac Asimov explains that on Venus
"surface winds were recorded that weren't very fast, only a
little over 11 kilometres (7 miles) an hour. Since the
atmosphere of Venus is so dense, however, such winds would have
the energy of earthly winds blowing at 105 kilometres (65 miles)
an hour. The 'gentle' wind is just about equivalent to a
hurricane on earth." (20) These winds of Venus are blowing
continuously over its entire surface. For an idea of the
effects, I ask the reader to imagine terrestrial surface winds
blowing day in and day out at 65 miles an hour. Imagine this
hurricane blowing for 3 or 4 billion years, remembering also
that the gases rushing over the surface rock are highly
corrosive. Based on any reasonable, gradualist suppositions, the
result would be a global, sandy Sahara! While one might wonder
if the absence of sand dunes was in the eye of the beholder, due
to poor resolution of the radar pictures, the undeniable state
of surface rock was noted in a 1975 Science News article titled
"Grand Unveiling of the Rocks of Venus." Here the author
described Venera 9 photographs of the surface: The initial
photo, apparently taken with the camera looking almost straight
down (suggesting that mission officials wanted to ensure at
least one picture before moving anything), contains a remarkably
clear view of some sharp-edged angular rocks. According to Boris
Nepoklonov, one of the mission scientists quoted by the Soviet
news agency Tass, 'This seems to knock the bottom out of the
existing hypothesis by which the surface was expected to look
like a desert covered with sand dunes because of constant wind
and temperature erosion.' In fact, he says, 'even the moon does
not have such rocks. We thought there couldn't be rocks on
Venus-they would all be annihilated by erosion --but here they
are, with edges absolutely not blunted. This picture makes us
reconsider all our concepts of Venus. (21)
_THE ENERGY PROBLEM
_Nor is there a clear explanation for the tremendous energy that
is moving the dense atmosphere. According to Billy P. Glass,
"The pressure at the surface [of Venus is approximately 90 bars,
which is equivalent to the pressure in the ocean on earth at a
depth of nearly 1 km [3,000 feet below sea level." (22) This
energy problem ties in with the enigma of Venus' rapid flow
pattern of its upper atmosphere. Atmosphere flows on Earth take
weeks to circle our planet at the equator. Though Venus rotates
much slower (its rotation period is 243 days), its atmospheric
cloud-- rising 39 miles above the surface-- flows at 100 m/sec
(about 330 feet per second), circling the planet in only 4 to
six days. Young and Young thus report: In the earth's atmosphere
such winds are encountered only in narrow jet streams. Jet
streams could not, however, account for the rapid atmospheric
movements observed on Venus, since the Venusian winds seem to
involve larger regions of the planet... Theoretical attempts to
explain the generation of the winds have produced several
possible mechanisms, such as convection caused by the uneven
heating of the day and night sides of the planet. None of them,
however, have been shown to be capable of explaining velocities
greater than a few metres per second. (23) Velikovsky's youthful
Venus, however, fits this bizarre atmospheric behaviour
remarkably well. Since Venus was a comet-like body, its tail
gases and coma atmospheric gases would still have great inertia
after Venus entered its orbit, the momentum of its massive tail
being transformed into a dense planetary atmosphere. Thus the
high velocity still persists in the Venusian upper (lighter)
atmosphere, while at the surface, where the atmosphere is most
dense, the gases move more slowly.
_TEMPERATURE
_This finally brings us to the oft-discussed matter of Venus'
atmospheric temperature. One of the major problems with the
"greenhouse" explanation is the process of convection. Stated
simply-- hot air rises. Clark R. Chapman explains what is
basically wrong with the thinking of the meteorologists who
resort to a supposed greenhouse effect to account for the
anomalous high temperature of the Venusian atmosphere. It was
recently pointed out to embarrassed meteorologists who have
debated the relevance of their greenhouse calculations that this
effect may not even be important for greenhouses. Outside ground
warmed by the sun heats adjacent air, which then floats upward
to where the barometric pressure is less. The air parcel
expands, cools and settles into equilibrium. Meanwhile at the
ground the warmed air is replaced by cooler parcels from above.
This process...warms upper regions and keeps the air near the
ground from getting too hot. Air on earth begins to convect
whenever the temperature begins to drop with altitude more
quickly than about 6 degrees C per kilometre [of altitude. So
except in an inversion, when the upper air is relatively warm
[warmer than the surface air convection maintains the 6 degree C
per kilometre profile which is why mountain tops are cool. The
reason it is warmer inside than outside a greenhouse is mainly
that the [glass roof keeps the warmed-up air inside from
floating away {by} is no lid on Venus and the dense carbon
dioxide is free to convect. (24) The super hot air of Venus,
therefore, must rise and carry away the surface heat of the
planet to the upper atmosphere where there is no covering. There
the heat will radiate into space. This upward motion or
convection of gas by heat will allow it to pass right through
the clouds. Hence, the reality is that Venus would convect and
radiate its surface heat into space long before its surface
reached anything like 750 degrees K. Achieving a relatively high
surface temperature for Venus would require a cover
encapsulating the entire planet to keep the hot air at the
surface from mixing with the cold air of the upper atmosphere.
No such mechanism is available, and this simple fact poses an
immense problem for the greenhouse theory. The problem becomes
fatal when it is discovered that Venus' atmosphere actually
rises and expands over the entire surface and then falls and
contracts periodically like a pulsating star. A 1973 article in
the New Scientist noted the work of four scientists at Caltech's
Jet Propulsion Laboratory demonstrating that Venus shows
"regular changes in the spectrum of its atmosphere," with marked
variations in the carbon dioxide lines on a four-day cycle: Over
20 years ago Gerard Kuiper noted day-to-day fluctuations in the
infrared spectrum of Venus, but no one has yet got to the bottom
of the basic cause of these changes. In order to study the
oscillations A.T., L.G., and J.W. Young and J. I Gerstrahl
obtained spectra nightly during the autumn of last year [1972.
Their data on the carbon dioxide line show an unmistakable
oscillation. The observed variation is not exactly periodic, but
more akin to a relaxation oscillation in which the amplitude
builds up on successive cycles and then suddenly collapses. In
order to produce the observed changes the cloud deck of Venus
must be moving up and down by as much as one kilometre,
simultaneously over the entire surface of the planet. Such a
large atmosphere oscillation requires a high input of mechanical
energy. This condition is difficult to account for in the case
of a slowly rotating planet heated uniformly by the Sun's rays
[Greenhouse effect. Therefore the cycle variations point to some
unexplained deep-seated property of the atmospheric dynamics."
(25) Gases expand when heated and contract when cooled. What is
very apparent is that the surface heat is building up so
strongly that it cannot be convected away as rapidly as it
builds up. The superhot air therefore expands and rises, pushing
the layers above it which also expand and rise. This process
goes on until the upper air layers have risen sufficiently high
to permit heat to dissipate more rapidly in the freezing
altitudes of space, following which the entire atmosphere
contracts to repeat the process. The amount of energy required
to accomplish such a feat is far greater than could be produced
by any "greenhouse" that lacks a cover! It is thus impossible to
reconcile the observed condition with a thermally balanced
atmosphere: an ancient planet would have achieved a thermal
equilibrium long ago. Hence, the fact that the Venusian
atmosphere is not in equilibrium makes the "greenhouse" effect a
charade and points to the same conclusion as the other
considerations reviewed above. In sum, the evidence we have
presented regarding Venus' atmosphere disputes the
uniformitarian view that Venus is an ancient member of the solar
system; in every instance, however, this evidence is completely
en rapport with Velikovsky's view that Venus is a newcomer to
the planetary system.
_References
#Post#: 238--------------------------------------------------
Re: Mathis on Velikovsky +
By: Admin Date: December 24, 2018, 5:57 pm
---------------------------------------------------------
The Nature of Venus' Heat [The Velikovskian]
... From: The Velikovskian Vol 1 No 3 (1993)
The Nature of Venus' Heat, Charles Ginenthal
_Ever since 1956, when the American team of radio astronomers
from the U.S. Naval Research laboratory, headed by Cornell H.
Meyer, discovered that "the surface of Venus is hot --far hotter
than anyone had previously imagined," (1) (Emphasis added.)
which fits Immanuel Velikovsky's hypothesis that Venus was a
newborn planet in the early cool-down stages of its development,
the scientific community --and, in particular, the astronomers
--sought a non-Velikovskian, non-catastrophist explanation for
this surprising finding. It was and still is unthinkable to
these upholders of a stable solar system that Venus could be a
recently born, newly acquired member of the solar system's
family. Ultimately, the only other explanation for the planet's
high temperature was the hypothesis that Venus was in the grip
of a runaway greenhouse effect. The early greenhouse model was
promoted by Carl Sagan in 1960 and 1962. (2)
_In 1970, S. I. Rasool and C. de Bergh added the "runaway"
aspect to the model. (3) Thus, the runaway greenhouse theory was
born and was expected to explain the high temperature of Venus
by straightforward uniformitarian processes. This model worked
its way into both scientific thought and nearly every astronomy
textbook, becoming the only other theory about Venus' high
temperature besides the catastrophist model presented by
Velikovsky, in spite of the fact that 20 years after the runaway
greenhouse model was proposed, Werhner von Braun openly admitted
that "scientists would like to be sure that the greenhouse
effect is indeed the cause of the hot surface and lower
atmosphere [of Venus. So far it is only a theory not yet proven
by experiment." (4)
_In the ensuing years, Soviet and American space probes to Venus
measured and collected evidence which has been used by
greenhouse advocates to show that Venus is heated by a runaway
greenhouse effect and that Velikovsky and his followers are
gravely mistaken to have imagined otherwise regarding its high
thermal emission. Nevertheless, with respect to Venus' high
temperature, I will show that the evidence clearly contradicts
the runaway greenhouse theory and is fully congruent with
Velikovsky's concept that Venus is a newborn planet still
shedding its primordial heat. I will show that, on many levels,
evidence investigated and proposed as supportive by the
greenhouse advocates is, at best, extremely weak and often
contradicts the underlying assumptions. The runaway greenhouse
model is, fundamentally, in direct opposition to physics,
observations, measurements and the historical theory of
planetary formation, which is one of the cornerstones of
science's uniformitarian thinking. The reader will be able to
understand how impoverished the claimed evidence for the runaway
greenhouse theory is, how deeply flawed the case for the runaway
greenhouse mechanism is, upon examination, and how it, in
effect, strengthens Velikovsky's theory: that Venus' heat is
derived from its interior.
_THE ORIGIN OF VENUS' GREENHOUSE
_A scientific theory that purports to explain Venus' high
temperature must also explain how and why the process began.
David Morrison and Tobias Owen explain the origin of Venus'
runaway greenhouse: The runaway greenhouse is a process through
which a planet can fundamentally alter the state of its surface
and atmosphere. Imagine what would happen if we could move the
Earth into the orbit of Venus. Our planet would suddenly be
closer to the Sun at 72% of its present distance. Sunlight would
[deliver about twice as much energy to every square meter of the
Earth's surface. Most of the Earth is covered by oceans, so the
immediate result would be an increase in [their
temperatures....The increase in temperature would lead to
increased evaporation. More water vapor would be present in the
atmosphere, which would trap more infrared radiation from the
Earth's surface. In other words, we would have increased the
greenhouse effect. This, in turn, leads to a further increase in
the planet's surface temperature, resulting in more evaporation
of water and a continuation of the cycle. We have established a
positive feedback loop, in which the initial disturbance
--increasing the Earth's surface temperature --produces
consequences which lead to an enhancement of that disturbance!
The cycle continues until the oceans literally boil away and all
water is converted to vapor, [producing an exceedingly hot
atmosphere. This is the runaway greenhouse effect. (5)
_This is the concept that must stand up to the evidence. What
Morrison and Owen have omitted from their discussion is the
nature of stellar evolution. They have analyzed the behavior of
ancient Venus in its early evolution by invoking the present
heat of the Sun upon Venus. Venus must be analyzed with respect
to the Sun as the Sun actually existed in its early evolutionary
development. Once done, an entirely different picture emerges
with respect to this process. Zdenek Kopal makes this clear: The
entire argument defended by some planetologists [regarding the
origin of the greenhouse effect contains one fatal flaw --an
implicit assumption that, in the early days of the solar system,
the youthful Sun was as bright as it is now. Actually, as a
zero-age [new Main Sequence star, our Sun should have been
approximately 40% less luminous than we see it today and its
surface temperature 10% lower. Venus is 28% closer to the Sun
than [the Earth is and any element of its surface receives
almost twice as much heat as we do on the Earth. Even so, the
early climactic conditions on Venus could not have been much
warmer than they are in the terrestrial tropics today, and, had
there once been oceans on Venus, very little of their waters
could have evaporated. Therefore, we are back where we started.
(6)
_The greenhouse theorists are well aware of this problem. What
is their explanation? James B. Pollack, Sagan's former pupil
and, later, collaborator says: Over the age of the solar
system...the Sun's total luminosity...increases by several tens
of percent --a long-term trend that would have induced dramatic
changes in the climates of the terrestrial planets.... [This
suggests that Venus' surface temperature was just on the
borderline of not being in a runaway state in the early solar
system, when the Sun's total energy output was [25% to 30% less
than it is today. The likelihood that Venus had oceans in its
early history, (albeit) hot ones, improves further when the
possible effect of water clouds are considered. Clouds reflect
sunlight back to space better than they trap thermal radiation,
so early Venus may have experienced a "moist" greenhouse (hot
oceans) rather than a runaway greenhouse (no oceans) [vaporized
oceans. (7) (Emphasis added.)
_The reader will notice two things: Pollack says the Sun's
temperature was "several tens of percent" cooler than at
present, but uses figures of 25% to 30% less than present, while
Kopal uses 40% less luminosity. Pollack also admits that clouds
would tend to cool Venus, but, on page 101 of his book, tells us
that his analysis was based on Venus having "cloudless skies."
Thus, with cloud cover over Venus, its temperature would be even
cooler than Pollack has computed. It would be below the
threshold of a "moist" greenhouse. Significantly, his statement
that "early Venus may have experienced a `moist' greenhouse" is
tantamount to an admission that it may not have had a moist
greenhouse. James E. Oberg tells us that Pollack does not
believe Venus had an early, runaway greenhouse effect. He states
that, "[ according to Dr. James Pollack, any guesses about the
early climate of Venus depend strongly on what kind of
atmosphere the planet possessed." ( 8 )
_Taking into account the 30% lower solar brightness,
computations show that a reasonable atmosphere on Venus would
have led to "` quite moderate temperatures' for more than a
billion years ...." (9) This means that Venus had a moderate
climate for a billion years or more and then started its runaway
greenhouse effect. Let us, nevertheless, allow the assumption
that the Sun, in its early history or thereafter, was just
sufficiently hot so as to generate a greenhouse effect on Venus.
What must follow? Morrison and Owen explain: At this point, the
atmosphere is so hot that water vapor can easily rise to great
heights, where it becomes exposed to solar ultraviolet light.
This is a crucial step. On Earth, water is protected by the
natural cold trap in the atmosphere. The air at the top of the
troposphere is so cold that water cannot diffuse upward to
levels where it could be attacked by ultraviolet light. A
runaway greenhouse can raise the temperature throughout the
lower atmosphere, giving water free access to high altitudes.
Because of the large mass of Venus, only the light hydrogen
atoms escape into space. The oxygen remains behind to combine
with rocks on the planet's surface and with other gases that
have been produced by the intense heating. The runaway
greenhouse leads to elimination of water from the planet in a
perfectly natural way....Quantitative studies of this phenomenon
indicate that water simply cannot remain on the surface of a
planet at [Venus' distance from the Sun. (10)
_The escape of hydrogen from the H 2 O molecule into space is
fundamental to all concepts for the removal of water from Venus'
atmosphere. Thomas M. Donahue and James B. Pollack state this
explicitly: "A common feature of all...[water loss mechanisms is
the implicit requirement that molecular hydrogen readily escape.
Otherwise, they would be incompatible with the trace amount of
molecular hydrogen that characterizes Venus' current atmosphere
of, at most, 10 ppm v/v." (11) The problem of ridding Venus of
its photodissociated hydrogen is far from simple, due to the
cold nature of Venus' exosphere. An exosphere is the upper
region of an atmosphere which has become so thin that atoms and
molecules rarely, if ever, collide. From here, hydrogen must
escape from Venus into space. Sagan explains that, "[ if the
exosphere temperature is very high, then the rate of escape of a
planetary atmosphere would be very high." (12)
_What happens to molecules in an extremely cold atmosphere? On
Earth, the temperature of the exosphere is between 950 K
[degrees Kelvin to 1,050 K, while the exosphere of Venus is
about 285 K, or 665 K cooler. On Earth, the temperature of the
upper atmosphere becomes hot; part of this region is called a
thermosphere, or hot atmosphere; however, on Venus, the
temperature of the upper atmosphere falls with altitude and is
thus called a cryosphere, or cold atmosphere. William K.
Hartmann states: The H 2 O [water is too heavy to escape
thermally in the lifetime of the solar system. Thermal escape of
H [hydrogen produced by photodissociation of the H 2 O was
thought to have caused the loss of H 2 O from Venus. However,
Pioneer discovered the [285 K exosphere temperature and
calculations show that the [hydrogen escape time from such an
exosphere is 20 Gy [20 giga, or billion, years. So how could H,
and, hence, H 2 O, have been depleted? If the exosphere had once
been heated to 1,000 K or so, the [hydrogen escape time could be
brought to a tiny fraction of the age of the solar system. In
any case, Pioneer scientists (Stewart A. [et al, 1979
"Ultraviolet Spectroscopy of Venus: Initial Results from the
Pioneer Venus Orbiter," Science 203, p. 777) concluded, "If
Venus ever possessed a large amount of water, it cannot have
lost it by escape mechanisms known to be operating now." (13)
_The results, when more fully analyzed, showed that the hydrogen
loss rate is presently only about 10 7 H cm -2s-1 (ten million
hydrogen molecules per one hundredth of a centimeter per second
squared). (14) "At this rate," Donahue and Pollack explain,
"only...[about 9 meters [30 feet of water could be eliminated
from Venus over its lifetime." (15) In order to generate a
greenhouse effect on a body as large as Venus, it becomes
apparent that a great amount of water, or of some other
material, must be vaporized in its atmosphere to create a
greenhouse powerful enough to literally cook the planet's carbon
dioxide out of its surface rock. But Pollack has also told us
that the early solar radiation would, if Venus had an ocean,
produce only a moist greenhouse, or a very moderate one at best.
Thirty feet, or so, of water on Venus will produce thousands of
lakes similar to those on the Earth. Most of Venus' surface
would be land and the moist or moderate greenhouse that Pollack
proposes under these conditions means no greenhouse, because
Venus had no oceans. The nightside of the planet's land surface
would quickly cool and the lost heat derived from the dayside by
convection would keep the planet cool, so that no runaway
greenhouse could get started. In the same way that Pollack
assumed that the Sun must be just sufficiently hot on ancient
Venus so as to start the greenhouse mechanism, he and the other
advocates of this heat phenomenon must also assume that the
escape rate of hydrogen from Venus in the early solar system was
immensely greater than at present. This is stated by Pollack: "[
It will be assumed that hydrogen can readily escape to space,
although, as we have seen, this remains to be demonstrated."
(16) (Emphasis added.)
_Furthermore, one cannot remove the remaining water of an ocean
by having it form hydrate compounds with surface materials.
Under such circumstances over time, the water would be recycled
volcanically back into Venus' atmosphere. So far, two
assumptions have been put forth to establish the credibility of
the origin of the greenhouse effect. The first assumption posits
that the Sun was just hot enough to heat Venus' oceans. The
second assumption posits that an escape mechanism, shown by the
data to contradict the hydrogen removal processes for escape
into space, is wrong. What must be pointed out is that a newborn
planet would be born with little or no water. Zdenek Kopal makes
this clear: "We are fairly sure that the newly-formed Earth
contained no water on its surface. It was born dry and its
oceans have since been exuded from the interior by thermal
`cracking' [heat removal of water of the hydrates [water-bearing
minerals." (17) Absolutely no assumption must be made regarding
the lack of water in newborn Venus' atmosphere. If Venus is a
newborn planet, as Velikovsky claimed, its lack of water is
completely in harmony with its present waterless condition.
_The other problem related to the photodissociation of water and
the escape of hydrogen is, Where did the residual oxygen go that
cannot escape into space? After an entire planet's ocean rose
into the upper regions of Venus' atmosphere and was dissociated
by ultraviolet light from which hydrogen escaped, the planet was
left with a lot of oxygen. Morrison and Owen have informed us
that "[ the oxygen remained behind to combine with the rocks on
the planet's surface." (18) Billy P. Glass addresses the same
question, asking, "[ Where is the oxygen? Pioneer Venus probes
only detected 70 ppm [parts per million oxygen in the lower
atmosphere. Some of the oxygen to account for a vanished `ocean'
of water would require that several kilometers of rock be
oxidized. This would require an extremely geologically active
planet." (19) Most scientists are skeptical that early Venus
had, for its first billion years of existence, immense volcanic
activity. On the Earth, it took an exceedingly long time before
enough water was vented volcanically from the interior prior to
ocean formation. The same is also expected for Venus. In this
respect, Venus would have had to exude its water vapor more
rapidly and much earlier than the Earth, so as to allow its
oxygen to unite with molten surface material. In fact, there is
no such scenario to suggest that, after the Earth formed oceans
on its surface, the crust --for some inexplicable reason --began
to ooze giant flows of lava. Hence, this is also a problem
needing explanation.
_Barrie William Jones deals with this question, saying that
oxygen would not escape to space in appreciable quantities, and
so [the combination [of oxygen with surface materials provides
the only repository. However, it is difficult to believe that
sufficient quantities of suitable substances could have appeared
at the cytherean [Venusian surface to mop up anywhere near the
amount of water. Indeed, chemical evidence from the
sulfur-bearing gases in the lower atmosphere of Venus...indicate
that the surface rock today does not contain the maximum amount
of oxygen possible. (20) The germane question is, How much
crustal rock material must be exuded as molten lava to mop up
the residual oxygen of a planet's oceans? What must be
emphasized is that this turning over of Venus' surface crustal
material had to occur over a billion years or more after the
planet cooled and its crust had become solid. According to
Oberg, "Pollack suggests that `runaway conditions were not
reached on Venus until halfway through its history.'" (21) J.
Kelly Beatty tells us that to remove all of Venus' atmospheric
oxygen, as suggested, requires no less than "remnant oxygen
combined [with materials to a depth of perhaps 450 kilometers"
(22) [279 miles. Such a depth of volcanic turnover is simply not
believable. It would require that, after Venus formed a crust
like that of the early Earth and outgassed an ocean of water,
the entire crust and mantle remelted to a depth of 280 miles, or
451 kilometers. But even at a depth of 100 miles, or 161
kilometers, of melt, there is no geological method presently
known that would remelt the entire surface of a planet that
much, particularly that of a planet believed to have a similar,
early geological history as that of the Earth. What is required
is based on a uniformitarian geology that is impossible. The
entire concept lacks support.
_James Oberg deals with a similar problem --getting rid of all
the oxygen in Venus' present atmosphere --and concludes that
this concept simply will not work: Imagine that all the carbon
dioxide [CO 2 could be converted, in the wink of an eye, into
free oxygen and carbon soot [as Morrison, Owen and others
suggest happened to H 2 O on ancient Venus. Now, instead of 90
bars of carbon dioxide, we have only 60 bars of free oxygen,
still three hundred times as much as on Earth. To get rid of it,
we may try to lock it up in surface rocks (the hotter the rocks,
the faster the reaction); but calculations show that the mass of
rock needed to absorb that excess mass of oxygen (assuming even
that the rock was not already partially or, even, predominantly
oxidized) would cover the planet to a depth of 100 kilometers
[62 miles or more. That means that the top 100 kilometers of the
surface of the entire planet would have to be gardened [turned
over or selectively exposed to air so as to absorb the oxygen.
On Earth, this process is accomplished by water erosion of
mountains raised by tectonism over eons of geologic time.
Something different would be needed on Venus. (23) To remove an
ocean's oxygen content from Venus by ordinary volcanic processes
would take much longer than the lifetime of the solar system.
There is no uniformitarian process by which to rid Venus of an
ocean! Without water turned to stupendously hot vapor, how does
one cook the carbon dioxide which had formed carbonates out of
the Venusian crust?!
_Some greenhouse advocates claim that the heating of Venus'
crust and mantle to a great depth would, nevertheless, release
an enormous amount of carbon monoxide. If the oxygen in the
atmosphere united with this additional carbon monoxide as well
as with surface materials, it would generate much of the carbon
dioxide presently found on Venus. However, Beatty explains that
"[ excess oxygen probably combined with carbon monoxide driven
from the interior, although University of Michigan's Thomas
Donahue admits it would take a `stochastic miracle' [a highly
improbable set of conditions to match the gases [oxygen with
carbon monoxide easily." (24) If this process actually occurred,
there would be, in overwhelming probability, a large, noticeable
amount of either excess oxygen or carbon monoxide in Venus'
atmosphere. This, of course, is not the case. The geophysical
processes employed by the astronomers to remove Venus'
atmospheric oxygen are either impossible or generally
implausible or require a stochastic miracle. In this respect,
Donahue and Pollack admit that "[ even if a vigorous recycling
of crustal material did occur in Venus' past, the incorporation
of water into the subducted material is not assured." (25) This
means that, even with plate tectonic crustal movement, the water
on Venus would probably still remain on the surface. According
to Eric Burgess, "[ no completely satisfactory explanation is
yet available for what happened to the [Venusian oxygen." (26)
_Let us assume that Venus did have an ocean. In recent articles,
some astronomers claim that they can see the region where Venus'
ocean lay. J. Kelly Beatty explains what would be left of the
Venusian topography after an ocean became vapor: Venus receives
twice the sunlight we do, enough to have converted all its
oceans to vapor --the equivalent of 250-300 bars of atmosphere
on top of its 90 bars of carbon dioxide. At that point, the
greenhouse effect would have run rampant; calculations show the
surface temperature would reach 1,500 K. Venus' surface melted
its lithosphere transformed [to lava into a churning cauldron
that continuously exposed fresh magma to its atmosphere. (27)
Simply melting the upper layer of surface rock would not churn
280 miles, or 451 kilometers, of material. What would happen,
however, is that all ocean basins and continents would flatten
at the surface and neither the original oceanic basins nor the
continents could survive.
_Modern astronomers are grasping at straws to suggest that they
can locate the original ocean basins on Venus. As far as I know,
the greatest problem involved in the removal of Venusian oxygen,
ozone formation, is never discussed by greenhouse theorists.
This problem is ignored every time one of the greenhouse
advocates discusses ultraviolet photodissociation of water
molecules in Venus' high atmosphere. Morrison and Owen had told
us that the origin of the greenhouse effect requires "the
atmosphere...[to become so hot that water vapor can easily rise
to great heights where it becomes exposed to solar ultraviolet
light." (28) Of course, greenhouse advocates tell us that
ultraviolet radiation will photodissociate water into oxygen and
hydrogen. What these same advocates fail to tell us is that
ultraviolet light, in Venus' high atmosphere, must generate
ozone! And every astronomer knows this simple fact. Morrison and
Owen state: In the upper part of the stratosphere [of Earth, the
absorption of solar ultraviolet light creates a layer of ozone
(O 3 ), an unusual form of oxygen with three atoms per molecule
instead of two. The ozone layer, sometimes called the
ozonosphere, extends from approximately 20 [kilometers to 50
kilometers [12 miles to 31 miles. Without it, solar ultraviolet
light would penetrate to the surface. (29) Valentin A. Firsoff
focused on the nub of the entire problem as long ago as 1973:
The mechanism by which Venus is supposed to have lost its water
is... unconvincing. [Water may be dissociated to hydrogen and
oxygen by the short [wave ultraviolet, the former [hydrogen
escaping to space. But the oxygen will not be lost. The
formaldehyde reaction: CO 2+ H 2 O= H+ CHO+ O 2, also mediated
by the ultraviolet, should further contribute to the supply of
atmospheric oxygen while radiation below 160Å [160 Angstroms
dissociates CO 2. Thus, by any reckoning, free oxygen should
have evolved in the [Venusian atmosphere, which would shelter
[water against further dissociation even if there had been no
clouds and no cold trap to keep it in the lower atmosphere. (30)
One simply cannot expect to photodissociate an immense amount of
water vapor into hydrogen and oxygen without creating an
ozonosphere. Once the ozonosphere forms, it stops the
dissociation of water vapor dead in its tracks and whatever
water remained in Venus' atmosphere or oceans could never be
further dissociated by ultraviolet because ozone has stopped the
"feedback loop." Based on this evidence, Venus would have lost
very little water. There is no way around this problem. That is
probably why it is evaded.
_What scientists have done is play a game of hide-and-seek with
ultraviolet radiation processes. Ultraviolet is invoked to
dissociate water into hydrogen and oxygen. This is the process
in which ultraviolet is scientifically observed. The fact that
oxygen, acted upon by ultraviolet, generates ozone is kept
hidden, conveniently ignored. In order to make the oceans of
Venus disappear, greenhouse theorists must deny the reality of a
well-known scientific process. Morrison and Owen state that [the
most important cloud-forming process on Venus is probably
photochemistry, chemical reactions driven by the energy of
ultraviolet sunlight. Photochemical reactions are important in
the upper atmosphere of planets, including the Earth, where the
production of ozone from oxygen is an example of a photochemical
process. (31) But there is never any discussion of the
photochemical formation of ozone from an ocean of oxygen in the
early Venus atmosphere. Why does ultraviolet dissociate water in
Venus' atmosphere but somehow fail to generate ozone? As far as
I know, neither Morrison, Owen, nor anyone else has addressed
this question. When discussing Mars, Eric Burgess points out
that Firsoff's analysis regarding an ozonosphere's ability to
halt the escape of oxygen is quite correct: "[ A fairly dense
atmosphere of oxygen might have accumulated on Mars in a period
of a million years....Incoming solar ultraviolet radiation would
have further restricted the escape of oxygen into space." (32)
If ozone restricts the escape of oxygen on Mars, of course, it
will do precisely the same on Venus.
_This phenomenon of a lack of oxygen or ozone on ancient Venus
is unexplained by the runaway greenhouse effect and is further
evidence in support of Velikovsky's theory. What must be pointed
out is that, as a newborn planet, Venus would be expected to
possess little or no oxygen and, therefore, no ozonosphere. This
is clarified by L. V. Berkner and L. C. Marshall in their paper,
"The History and Growth of Oxygen in the Earth's Atmosphere":
The absence of a significant content of oxygen in the primitive
secondary atmosphere is confirmed by several lines of evidence.
First, there is no suitable source....Second, the incomplete
oxidation [oxygen joined with other substances of early
sedimentary materials [on Earth (three billion years of age) as
demonstrated Raukama, Ramdohr, Lepp and Goldich, and
others...suggests very early lithospheric [crustal sedimentation
in a reducing [oxygen-free atmosphere....Finally, the rapidly
growing evidence on the origin of life on planet Earth appears
to forbid significant oxygen concentration. (33) Absolutely no
specialized process must be invoked regarding the lack of oxygen
in Venus' atmosphere, based on Velikovsky's hypothesis. Barrie
William Jones has said that there is no indication that the
surface rock is saturated with oxygen. Thus, the lack of water
and oxygen on Venus is evidence one would expect to find on a
newborn planet and is in full harmony with Velikovsky's concept.
_Nevertheless, one may raise the argument that we don't need
water at all in Venus' atmosphere. Venus was simply born without
it, or very little of it, and that solves the problem. Oberg
states: Alternately, of course, the ocean theory may be
completely wrong, and Venus may never have had much water. The
oceans may never have had much water. Different theories of
solar system formation can give different ratios of Venusian
water to terrestrial water. The ocean may never have been there,
or the temperatures may always have been too high (but then
another agent for high temperatures would have had to be
invented). (34) But this suggestion is not a solution. If there
was no water in Venus' ancient atmosphere, how does the planet
start the greenhouse effect? One needs either water or an
inordinate amount of some gas to hold sufficient heat to cook
the carbon dioxide out of the surface rock. Methane does that
job well. But methane is a light gas, like water vapor, and, if
Venus was endowed with methane, it would also have been endowed
with water. Furthermore, astronomers do not seriously suggest
that the two planets, Earth and Venus, situated so close to each
other in the inner solar system, created from the same
processes, would have totally different inventories of water.
Morrison and Owen state that "if all the carbon [of the Earth
were put back into the atmosphere in the form of carbon dioxide,
the atmosphere would have a pressure of about 70 bars [70 times
more pressure than at present and a composition [consisting of
more than 98% carbon dioxide and little more than 1% nitrogen."
(35) According to Pollack, Venus' 90 bar atmosphere is 96%
carbon dioxide and 3.5% nitrogen. (36)
_Pollack also states that "[ when all these reservoirs [of gases
are taken into account, we find that Earth and Venus have very
comparable amounts of [carbon and [nitrogen. This similarity
implies that the two planets initially had comparable amounts of
water." (37) He concludes that, "[ regardless of the sources,
these worlds [terrestrial planets obtained comparable initial
endowments of volatiles. Specially in the cases of Earth and
Venus." (38) There is no reason to argue whether or not Venus
lacked water based on all geophysical concepts. To do so is to
negate the fundamental theories of solar system formation. Oberg
adds these telling remarks: Even with great amounts of carbon
dioxide, Venus could have a moderate climate if water was in
short supply but present in enough amounts to form pools within
which carbonate rocks could be formed to absorb some carbon
dioxide. The addition of off-planet substances in trace amounts
(Pollack suggests "collisions with volatile-rich comets and
asteroids") may also have had catastrophic climactic effects by
blocking off hitherto open "windows" in the "greenhouse effect."
(39) In essence, no natural processes, using Venus' gases alone,
would lead to a runaway greenhouse effect. Pollack was finally
forced to invent additional gases from the ad hoc concept that
comets or asteroids must have brought these additional
constituents. But this simply will not do! All theories of
planetary formation suggest that the early planetesimals that
formed the planets were made of comets and asteroids. So the
same materials had to exist inside the planets Earth and Venus.
_This being the case, for Venus to start a greenhouse, some
other gas or gases must be invoked. And this is precisely what
Carl Sagan has been attempting to do. To save the process, he
has sought some other gas to enhance the action of water vapor.
According to Pollack: Sagan and George Mullen have suggested
that as little as 10 parts per million of ammonia (NH 3) may
have produced the desired greenhouse enhancement. However,
practically no ammonia should have been outgassed by volcanoes
into the early atmosphere. Moreover, NH 3 is easily broken down
by ultraviolet radiation into nitrogen and hydrogen, and it is
very difficult to recombine these two back into the parent
molecule. Therefore, ammonia is probably not the agent involved
in the early greenhouse enhancement. (40) It has been more than
30 years since the greenhouse effect arose as an explanation for
Venus' high temperature. For over 30 years, the scientists who
have diligently worked on this mechanism have failed to find a
valid process that will get it started. In order to begin the
phenomenon, they have had to turn to exotic enhancement gases
that are not believed to have existed in the early atmosphere of
Venus and that cannot survive for very long in the presence of
ultraviolet light.
_When a theory is correct, over time, it finds suitable answers
and the various problems and questions begin to be resolved,
each element falling into place. This is not the case with the
evidence regarding the runaway greenhouse effect. Its origin is
still widely unknown and highly problematic. Its advocates are
seeking new gases to enhance water vapor and suggest that the
entire crust of the planet somehow remelted long after it
solidified so as to remove its oxygen. Its supporters have
stubbornly failed to come to grips with Firsoff's objection
regarding the formation of an ozonosphere. These theorists don't
even know if the early Sun was hot enough to start such a
process and simply wave their hands in order to make hydrogen
escape the planet rapidly. None of their processes have been
validated in any way other than by taking theoretical
assumptions as facts. As stated earlier, a phenomenon like the
greenhouse effect has to have an origin. If there is no origin
for a theoretical concept, it becomes exceedingly difficult to
accept the hypothesis that is proposed. This is the case for the
runaway greenhouse effect on Venus: No beginning, no greenhouse.
Nevertheless, its advocates suggest that, since the process is
ongoing, we simply have to assume that our knowledge of the
precise ancient history of planetology is flawed; and, even with
these difficulties, we can see Venus today in the full throes of
a runaway greenhouse effect. That the early history of the solar
system is nebulous is a reasonable, cautious suggestion, but
before passing such a favorable judgement on this heating
mechanism, one must be able to demonstrate, fully, that Venus is
in the midst of a runaway greenhouse effect. The question in
this instance is, Does the evidence fully support this
conclusion? Let us investigate this claim, remembering Werhner
von Braun's admonition regarding the greenhouse model: "So far,
it is only a theory not yet proven by experiment." (41) What is
the evidence for a runaway greenhouse effect on Venus?
_EVIDENCE OF A VENUSIAN GREENHOUSE?
_Morrison and Owen explain how the greenhouse effect works: Why
is Venus hot? The answer comes from a phenomenon known as the
greenhouse effect....In a typical greenhouse, the glass in the
roof allows visible sunlight to enter and be absorbed by the
plants and soil within. These objects then heat up and radiate
at infrared wavelengths just like the Earth itself. The glass of
a greenhouse, however, is largely opaque to infrared radiation.
It acts as a color filter, letting short wavelengths [of
sunlight in through [the glass, but limiting passage of longer
wave [infrared thermal radiation [out. Since most of the heat
cannot escape the interior of the greenhouse, it warms the glass
to balance the energy coming in. A similar effect occurs in a
car left out in the Sun on a hot day.... The gases in a planet's
atmosphere can play the same role as the glass in a greenhouse,
if they have the same property of transparency to visible light
and opacity to infrared. (42) Therefore, one would expect that
the gases in Venus' atmosphere can act as does the glass in the
greenhouse, but, more importantly, that these gases are found in
sufficient quantities to permit short-wave sunlight to pass
through them, then act to block infrared thermal radiation from
escaping. When discussing the composition of the constituents of
Venus' atmosphere, I pointed out that the components of Venus'
atmosphere were carbon dioxide, which comprises 96%, and
nitrogen, which comprises 3.5%, with other gases making up the
rest of Venus' inventory. The greenhouse theorists insist that
the three component gases for their greenhouse model are carbon
dioxide, water vapor and sulfur dioxide. And, indeed, there can
be no doubt that there is sufficient carbon dioxide to carry out
this greenhouse function. However, carbon dioxide, even in the
abundance found on Venus, will not produce the opacity necessary
to generate a runaway greenhouse. According to Barrie William
Jones: efficient trapping [of heat cannot be produced by CO 2
[carbon dioxide alone, in spite of the enormous mass of CO 2 in
the Venusian atmosphere. This is because CO 2 is fairly
transparent over certain [short wavelengths [to escape in
infrared, thermal wavelength ranges [and to [escape in planetary
[infrared wavelengths. Radiation could escape through these
"windows" in sufficient quantities [so as to greatly reduce the
greenhouse effect below that which [presently
exists....[Additional...windows [closed by SO 2 [sulfur dioxide
and H 2 O, and by the clouds [and hazes, [are what greatly
increases the greenhouse effect. (43) Carbon dioxide needs the
assistance of water vapor, sulfur dioxide, clouds and hazes to
complete the job that it began. Of significance, then, is the
contribution each of these gases makes to the greenhouse effect.
Gary Hunt and Patrick Moore have outlined these contributions:
CO 2 is responsible for about 55% of the trapped heat [in Venus'
atmosphere. A further 25% is due to the presence of water vapor,
while SO 2, which constitutes only 0.02 [2/100 of a percent of
the atmosphere, traps 5% of the remaining infrared radiation.
The remaining 15% is due to the clouds and hazes which surround
the planet. (44) Let us examine the closing of windows with
respect to the amount of hazes, clouds and sulfur dioxide in
Venus' atmosphere. These constituents are responsible for
shutting off the escape of 20% of the thermal radiation left
open by carbon dioxide and water vapor. According to Larry W.
Esposito, Pioneer Venus has continued to monitor these
constituents [haze and sulfur dioxide above the clouds. Over the
years, a remarkable discovery has emerged: Both the sulfur
dioxide and the haze have been gradually disappearing. By now,
only about 10% of the 1978 amount remains. This disappearance
has also been confirmed by the Earth-orbiting International
Ultraviolet Explorer [satellite between 1979 and 1987 and by
other Earth-based observations. The haze and the sulfur dioxide
are now approaching their pre-1978 values. Analysis of recent
Earth-based radio observations, by Paul Steffes and his
colleagues, [also shows less sulfur dioxide below the clouds.
[Emphasis added than was measured by Pioneer Venus and Venera
landers, which is also consistent with the decrease of sulfur
dioxide. (45) Pollack concurs with this observation:
"Measurements by the Pioneer Venus orbiter show that the amount
of sulfur dioxide present near the cloud tops declined from
approximately 200 parts per billion (ppb) in 1978 to about 10
[parts per billion...in 1986." (46) Morrison and Owen also
concur, stating that "[ observations over the past [20 years
have indicated that large fluctuations occur in the
concentration of sulfur dioxide (SO 2) in the atmosphere of
Venus above the clouds." (47) The proponents of the greenhouse
effect admit that the components responsible for 20% of the
opacity of sulfur dioxide and hazes decline by up to 90% above
the clouds and, to some lesser percentage, below the clouds. If
the levels of the hazes and sulfur dioxide in the atmosphere
fall to significantly lower concentrations above, as well as
below, the clouds from their former levels, they cannot act as
influentially to block the entire 20% of the greenhouse windows.
This evidence could be a blow to the runaway aspect of the
greenhouse effect. Consider the suggestion that particles in the
clouds also act as does the glass in a greenhouse. These
particles are either liquid droplets or tiny, solid particles.
Therefore, the composition of the Venusian clouds ought to be
known, so as to determine how influential these particles are in
blocking heat escape. Greenhouse advocates believe that they
know the composition of the clouds and use that assumption in
their calculations. According to A. Seiff, "Pollack and Young
(1975) assumed 75% H 2 SO 4 [sulfuric acid clouds." (48) This
is, indeed, the conclusion Carl Sagan proposed when he said:
Moreover, the question of the composition of the Venus clouds
--a major enigma for centuries --has recently been solved (Young
and Young, 1973; Sill, 1972; Young, 1973; Pollack et al., 1974).
The clouds of Venus are composed of approximately 75% solution
of sulfuric acid. This identification is consistent with the
chemistry of the Venus atmosphere, in which hydrofluoric and
hydrochloric acid have also been found; with the real part of
the refractive index deduced from polarimetry, which is known to
three significant figures (1.44), with the 11.2 (and now far
infrared) absorption features; and with the discontinuity in the
abundance of water vapor above and below the clouds. (49) This
statement by Sagan, for all its impressive spectroscopic,
analytical evidence, is disingenuous to say the least. Zdenek
Kopal explains why: The reader should, however, be encouraged
not to take these current cosmochemical scenarios as gospel
truth. Although the sulfuric acid hypothesis accounts
satisfactorily for many optical properties of the clouds
surrounding Venus, it cannot explain one important property
--the yellowish colors of the planet. The color must be produced
by some substance that absorbs in the blue and ultraviolet
regions of the spectrum. Sulfuric acid does not meet the
requirement, nor does any other likely substance which could be
considered in this connection. (50) Oberg admits, "The light
yellow clouds seen from Earth are almost certainly droplets of
sulfuric acid....The actual cause of the yellow tinge and the
variable ultraviolet absorption is still unexplained." (51) But
this assertion proves nothing. It is merely an attempt to evade
facing the implication that the yellow tinge of the clouds
denies that they are sulfuric acid in composition. Jones further
explains: Detailed studies, mainly by spacecraft, have revealed
the existence of at least three types of cloud particles. First,
there are the tiny particles....The observations indicate they
probably (Emphasis added.) consist of nearly pure sulfuric
acid....These are present in the main cloud and in the hazes
above and below, but though they are the dominant constituent of
the haze they are a minor constituent of the main cloud. Second,
there are larger particles...largely confined to the cloud, each
particle probably (Emphasis added.) consisting of a liquid
droplet of rather impure H 2 SO 4 [sulfuric acid with up to 20%
of other substances. [Third, there are solid particles...largely
confined to the lower half of the main cloud....This third type
is the dominant constituent of the main cloud and also accounts
for most of the opacity. (52) Jones tells us that this third
constituent produces most of the opacity of the clouds.
Greenhouse theorists base their conclusions regarding cloud
opacity upon this third constituent. One cannot, as Sagan seems
to suggest, derive a spectroscopic analysis of this deeper cloud
material for two reasons: One, this material is located much
deeper in the clouds and light from this region is very
difficult to see. Two, even if one sees down to these depths,
these particles do not produce spectroscopic lines. Kopal asks,
What do the clouds of Venus really consist of? To determine
their composition is far more difficult than to identify the
gases constituting the atmosphere, because these clouds must
consist of particles which are either solid or liquid. Such
materials, unlike gases, do not produce spectral lines that can
identify them. (53) Since I am dealing with Sagan's claim that
the clouds of Venus are composed of sulfuric acid, I will
complete this discussion using additional information. Billy P.
Glass shows that Sagan's pronouncement regarding the composition
of Venusian clouds is highly speculative. He informs us,
contrary to Sagan, that [the nature of the clouds [of Venus has
been a question of great interest for a long time. Speculative
interpretations [regarding the principal constituent of the
clouds include: water drops, ice, frozen carbon dioxide, carbon
suboxide, mercury, halite, ammonium nitrate, ammonium chloride,
silicate, dust particles, carbonate particles, formaldehyde,
hydrocarbon droplets (Emphasis added.), partially hydrated
ferric chloride and hydrochloric acid. (54) What becomes
apparent is that the makeup of the clouds' principal liquid or
solid component is still in question, no matter how often
Velikovsky's critics suggest otherwise. Is it, therefore,
possible that Sagan is still unaware that the composition of
clouds is disputed? In their book, The Planetary System, David
Morrison and Tobias Owen have a foreword written by Carl Sagan.
He lauds the authors as "pioneers in the modern exploration of
the solar system" whose book is "marked by a judicious and
comprehensive selection of topics [with clear qualitative
explanations." (55) What do Morrison and Owen say regarding the
makeup of the Venusian clouds? Space probes that have passed
through the clouds have given us a picture...of discrete cloud
layers. Clouds are seen extending from 30 kilometers to 60
kilometers [19 miles to 38 miles above the surface. But what are
the various clouds made of? Are they all sulfuric acid, as are
the visible [topmost layers? Only the Soviet probes have
attempted compositional measurements and their results have been
contradictory. Sulfur or, possibly, chlorine compounds of some
sort are indicated, but their exact identities are unknown. (56)
(Emphasis added.) Thus, Sagan's sulfuric acid clouds are nothing
of the sort. Sagan has disqualified himself from any meaningful
discussion of Velikovsky's work. Furthermore, with respect to
the greenhouse effect, one cannot assume anything about the
opacity of the clouds because their chemical makeup is simply
not known. With the ability of the hazes, clouds and sulfur
dioxide to block 20% of the greenhouse windows in question
because the hazes and sulfur dioxide levels fall to 10% of their
earlier measured values over periods of years, their efficiency
in blocking infrared from escaping Venus must also be reduced to
some level below the full efficiency of 20%. This being the
case, it becomes critical for the runaway greenhouse theory that
water vapor be found in sufficient quantity so as to block the
remaining 25% greenhouse window. The question is, How much water
vapor is needed to do this? Originally, when Sagan first began
his work, he believed the surface pressure on Venus was only 4
bars. From this, he calculated a required water vapor fraction
of the atmosphere, between 5% and 23%, to close this greenhouse
window and permit a surface temperature of 600 K. (57) As time
went on, space probes made more precise measurements of Venus'
chemical makeup and solar heating values. The parameters of
pressure changed and, with these changes, the water vapor
requirement changed. In essence, the greenhouse investigators
did not know what each of the parameters really was and, thus,
had to adjust their theoretical requirements accordingly.
Nevertheless, these parameters are now very well measured,
though they may vary slightly, and the greenhouse theorists have
a good idea of the amount of water vapor necessary to reach the
full 25% window closure needed to support the theory. Yet, years
of searching for this water vapor constituent on Venus have
failed to find anything like this necessary component at the
required level. As recently as September, 1991, it was still
reported that a research team [had focused on a greenhouse
puzzle....The absence of water vapor above Venus' clouds
mystifie[d scientists because models of the planet's strong
greenhouse effect suggest[ed that vapor play[ed a key role in
maintaining the warming. Researchers ha[d...looked below the
cloud deck and down to the surface --and their search ha[d come
up dry.... Evidence of a dry Venus may force researchers to
consider whether other chemicals could create and sustain the
planet's greenhouse effect, said David Crisp of the Jet
Propulsion Laboratory,...who co-authored the report. (58) Hence,
the critical, second most important constituent for closing the
25% greenhouse window is clearly known to be insufficient to do
its job. As with the problem discussed earlier about finding
another enhancement gas besides water vapor to start the
greenhouse mechanism on ancient Venus, we are faced with
scientists searching for another gas besides water vapor to
assist in mopping up 25% of the escaping infrared radiation on
present-day Venus. The composition of the gases in Venus'
atmosphere is very well-known, except for the constituents of
the clouds. The constituents of the clouds are what greenhouse
advocates have at their disposal as enhancement gases. As we
already know, ammonia cannot be invoked for primordial Venus
because Pollack has shown that photodissociation by ultraviolet
radiation of ammonia, into nitrogen and hydrogen, would readily
occur in the clouds --and these gases are difficult to
recombine. Earlier, I mentioned that methane could have been
invoked in the ancient atmosphere as an enhancement gas because
it is an excellent greenhouse gas. And, in fact, there is
evidence for methane in Venus' present atmosphere. (59) But, if
the greenhouse theorists wish to turn to methane as the enhancer
to close their 25% greenhouse window, they will be opening a
door for Velikovsky's theory. Based on the research done,
Velikovsky assumed "that Venus must be rich in petroleum gases.
If, and as long as, Venus is too hot for the liquefaction of
petroleum, the hydrocarbons will circulate in gaseous form."
(60) Methane is the simplest of the hydrocarbon gases. The
reader will recall Zdenek Kopal's statement that the yellowish
color of the clouds, as seen in ultraviolet, denies that the
clouds are composed of sulfuric acid. The question is, Can
methane account for the yellowish color of Venus' deeper clouds?
The answer may lie in the nature of a solar system body known to
have much methane. Kenneth R. Lang and Charles A. Whitney
discuss Titan, a giant satellite of Saturn: In 1944, Gerard
Kuiper discovered signs of methane in the spectrum of Titan's
atmosphere. The presence of nitrogen was firmly established in
1980, when the ultraviolet detectors aboard Voyager I showed
that nitrogen molecules account for the bulk of Titan's
atmosphere. Visible light cannot penetrate Titan's atmosphere,
for it is covered by an obscuring veil of orange smog (Emphasis
added.) produced by photochemical reactions as ultraviolet
sunlight breaks methane and nitrogen molecules apart. Some of
these fragments then recombine to create the smog, and, in
Titan's dry cold atmosphere, the smog builds to an impenetrable
haze. (On Earth, smog also forms by the action of sunlight on
hydrocarbon molecules in the air.) (61) If Venus' clouds contain
hydrocarbons, then the same photochemistry occurring in Titan's
clouds may be occurring in Venus' clouds. Venus has nitrogen
comparable to that of the Earth; its atmosphere is dry,
ultraviolet is available and the clouds are very dark at a
deeper level, as with Titan. Hence, with perhaps fewer reactions
taking place where there is less methane to create smog, the
number of reactions may create a yellowish smog rather than an
orange one. One still cannot dismiss Velikovsky's hydrocarbon
cloud composition for Venus, because the clouds' chemical
composition is still not known. Returning to the greenhouse, if
the clouds of Venus are made up of significant amounts of
hydrocarbons, just as Velikovsky claimed, then the greenhouse
advocates may be able to better secure their theory because
methane --in abundance --may shut all the greenhouse windows
that may be open. It is a fascinating catch-22 situation;
Velikovsky's greenhouse critics refuse to claim that the
Venusian clouds are made of hydrocarbons, because Velikovsky
would have been right all along respecting this prediction. On
the other hand, these greenhouse advocates may fail in their
campaign if they reject hydrocarbon clouds, because their
greenhouse enhancement gas may not be available. For those
suggesting that, for Venus, no scientists would propose that an
early-age planet would possess methane in its atmosphere, I cite
James Oberg. Discussing how Mars, in its early day, maintained
water on its surface at a time when the Sun produced 30% to 40%
less radiation than it does now, he writes: According to [James
B. Pollack, a Martian greenhouse of carbon dioxide alone would
not produce a very efficient "greenhouse effect." In fact, a
surface pressure of 2 bars [double the Earth's atmospheric
pressure would be required for the globally- and
annually-averaged surface temperatures to be above freezing.
However, if the atmosphere were predominantly methane with
admixtures of ammonia and water vapor, a very effective
"greenhouse effect" would have been created which would have
allowed liquid water to form...." (62) (Emphasis added.) If
scientists suggest the possibility of methane, a hydrocarbon, in
the early atmosphere of Mars, there is no compelling reason to
deny that the same exists in Venus' atmosphere, presently, if
Venus is an extremely young planet. At this stage of analysis,
it is evident that all the component gases necessary to fully
generate a runaway greenhouse effect on Venus are not found in
appropriate amounts to sustain this effect --except for carbon
dioxide. The amount of water vapor stands as a major obstacle to
the solution of this problem. To argue that the water is there,
except that we can't find it, is assuming what must be proven.
Furthermore, much of the evidence regarding the hazes and clouds
is simply assumed to be correct, as is, for example, the
conclusion that they are composed of a 75% solution of sulfuric
acid; when, in fact, there is enormous disagreement among
scientists about the composition of the clouds. As we can see,
all the assumptions must be taken as facts and, even with these,
one cannot be confident that the greenhouse is a runaway
greenhouse. But the assumptions are only assumptions "still to
be proven by experiment," as von Braun stated. Therefore, the
view that the runaway greenhouse is correct is simply not
conclusive, and, therefore, ought not be promulgated. The
conclusion that these gases are doing all that is claimed for
them (except carbon dioxide) in Venus' atmosphere is tenuous at
best.
_ATMOSPHERIC CIRCULATION
_There are two sources of energy that can circulate air masses
in a planetary atmosphere. The first source of energy is the
rotation of the planet. The Earth's winds generally blow in a
west-to-east direction because of the Earth's rapid west-to-east
rotation on its axis. Surface topography in contact with the
atmosphere causes the bottom layer of air to move in the
direction of the Earth's rotation. This motion at the bottom of
the atmosphere is transferred by air currents to the rest of the
atmosphere and imparts the west-to-east motion throughout.
East-to-west or west-to-east motions are designated as zonal
motion or zonal circulation. The second source of energy that
imparts motion in a planet's atmosphere is solar heat. The sun's
radiant energy heats the dayside of a planet, more so in the
equatorial regions than in the polar regions. This form of
radiant input causes the hot air to rise at the equator and, in
the upper atmosphere, to move toward the cooler polar regions.
When the air becomes sufficiently cooled, it sinks to the
surface and then returns, along this surface route, to the hot
equatorial regions where it is heated to rise and repeat the
cycle. George Hadley, who explained this motion, has had this
atmospheric circulation named for him. Such heat-driven motions
are called Hadley cells. North-to-south and south-to-north
motions are designated as meridional motion or meridional
circulation. On the Earth, which is rotating rapidly and is also
heated by solar radiation, a combination of these two motions
develops. Air, heated at the equator, rises and blows
meridionally north in the northern hemisphere and south in the
southern hemisphere. But the air masses are also feeling the
influence of the Earth's rotation and, thereby, are forced to
veer toward the east in both hemispheres as they leave the
equatorial regions. Because the air masses at the equator are
moving zonally at 1,000 miles per hour while those air masses
farther north and south are moving more slowly in relation with
the Earth's rotation, a pseudo-force is created which causes air
masses to circulate in a broad, counterclockwise movement in the
northern hemisphere and to circulate clockwise in the southern
hemisphere. For example, if we were to slow down the Earth's
rotation to a sidereal rotation period of 100 days, the Earth's
air masses would receive almost no push from the surface
topography and the west-to-east zonal motion would, over time,
dissipate and almost come to a stop. The Sun would still be
heating the equatorial regions on such a slowly rotating Earth,
on the dayside, for longer time periods. This solar heat force
would generate very powerful Hadley cells and the dominant form
of atmospheric circulation would be meridional, north and south
motions. There would be practically no zonal motion in the
Earth's atmosphere under such conditions. On Venus, we encounter
the same two forces: planetary rotation and solar radiation.
However, there is a singular difference between the two planets.
Venus' rotation rate is 243 times slower than that of the Earth.
There is no compelling rotational force on Venus to cause its
atmosphere to rotate zonally, that is east to west. Because of
this one fact, the other force --solar radiation --becomes the
only significant, driving mechanism in Venus' atmosphere and
should induce two giant, hemispheric, meridional Hadley cells.
This, then, is an excellent way with which to test Velikovsky's
concept that Venus is heated uniformly from its hot molten core
not far below its crust and compare it to the concept of solar
greenhouse heating. If the solar-induced runaway greenhouse
effect is the dominant source of heat for Venus' atmospheric
circulation, its atmosphere should exhibit clearly observable,
directly measurable Hadley cells. In Pioneer Venus we read that
[thermal contrasts provide the driving mechanism for the general
circulation, since they set up the pressure differences to drive
[air flow. The absence of large thermal contrasts in the
atmosphere of Venus means that there is a very effective
transport of heat from equator to poles and from the subsolar to
antisolar points by means of atmospheric circulation; the
atmosphere must be able to transport heat from the region below
the Sun to the rest of the planet. (63) If such a circulation is
not found, or the atmosphere shows practically no or extremely
small, meridional motions, one may be confident that the
greenhouse mechanism is not the generating force in Venus'
atmosphere. If Velikovsky is correct and the entire planet is
heated fairly uniformly from its subsurface, then Hadley cells
are not required so as to circulate the air masses. Velikovsky's
theory requires no such circulation pattern. If Venus' heat is
derived from below its hot crust, then all that the Venusian
atmospheric gases have to do is either radiate, conduct or
convect heat upward. There is no requirement to circulate hot
air masses from the equator to the poles and back to the
equator. If the runaway greenhouse effect is correct, there will
be definite Hadley cells circulating the atmosphere. If
Velikovsky is correct, few or no Hadley cell motions will be
observed or measured. Gerald Schubert explains how this Hadley
circulation works and why it is necessarily expected for the
Venus greenhouse theory: The basic drive for atmospheric
circulation is latitudinal imbalance between absorbed solar
radiation....In equatorial latitudes, more energy is absorbed
than is reradiated to space. The opposite is true in polar
latitudes. The atmosphere must redress this imbalance by
transporting heat poleward. Meridional transport of heat in the
Earth's atmosphere is accomplished by a Hadley circulation in
low latitudes and by baroclinic [pressure change eddies in
mid-latitudes....However, baroclinic heat transport would not be
expected to dominate in the mid-latitudes of an atmosphere on a
slowly rotating planet like Venus and a Hadley circulation, on
Venus, would be expected to extend to high polar latitudes.
Thus, it would be anticipated that the primary circulation
mechanism on Venus would be a pair of [north and south
hemispheric Hadley cells symmetric about the equator, with
rising motions over the equatorial latitudes, poleward flow at
high latitudes sinking over the polar regions and equatorward
flow near the surface. It is, therefore, remarkable that Venus'
dominant atmospheric circulation is a westward super-rotation.
However, zonal winds cannot transfer heat poleward, so there
MUST BE a weaker meridional circulation as well. (64)
(Capitalization added.) Gerald Schubert fully agrees that the
greenhouse mechanism requires Hadley cells as the dominant form
of circulation. To the chagrin of the greenhouse theorists,
instead of discovering a circulation pattern in harmony with the
greenhouse theory, one featuring the opposite was found.
Westward blowing winds, Schubert admits, do not transport heat
toward the poles and super-rotation means that, at all latitudes
and altitudes, the wind is moving zonally east to west on Venus.
Thus, where is the meridional circulation carrying hot air to
the poles and cooler air back to the equator, if the greenhouse
effect dominates Venus' atmosphere?! According to Schubert,
somehow a weak meridional circulation must exist. By saying that
such a circulation must be proves absolutely nothing. What is
the evidence for this circulation pattern? Let us examine the
bottom layers of the atmosphere to see if any turnover Hadley
cells are operating there. Pioneer Venus reported the following:
A surprising discovery is that much of the deep atmosphere is
stably stratified like the Earth's stratosphere or like air in
the Los Angeles basin on a smoggy day. (Emphasis added.) From
the clouds down to 30 [kilometers altitude (a layer 23
kilometers deep) [14 miles and in the lower layer [at the
surface between 15 kilometers and 20 kilometers[ 9 miles to 12
miles altitude, the atmosphere is stratified and free of
convective activity. It does not rise and overturn in the way
that air does over hot farm or desert land on Earth, or in
cumulus clouds. This was unexpected, because the high
temperatures in the deep atmosphere were thought to be a source
of hot rising gas which would lead to deep convective cells
[Hadley cells and turbulence. Also, before Pioneer Venus,
theoretical studies had indicated that, at radiative equilibrium
much of the lower atmosphere would be unstable and would be
overturning. (65) (Emphasis added.) There is no Hadley
circulation in atmospheric layers; one being, from the surface,
up to 12 miles high and the other from the clouds down, a layer
14 miles thick. This lack of circulation in the lower atmosphere
is a fundamental contradiction to the greenhouse mechanism and
Schubert specifically makes this point: "A direct meridional
circulation in the deep atmosphere is...needed to balance the
observed increase in infrared cooling with latitude." (66) If
there is more heat at the equator and less toward the poles, as
Schubert claims, where is the circulation of air toward the
equator that should support this statement? These conclusions
exist nowhere, except in theory and on paper. For example, on
the basis of certain readings from one Pioneer Venus Night
probe, it was quickly determined that there were three layers of
air in Venus' atmosphere below 40 kilometers (25 miles) where
winds blow north and south, away from the equator, as giant air
flows, distributing hot air from the equator very near to the
poles and the returned cooler air back to the equator. (67)
Nevertheless, Pioneer Venus probes measured the wind directions
at other points on the planet and found that "the meridional
winds below 40 kilometers at the other Pioneer Venus probe
sites...are not consistent with a three-layer mean circulation
pattern and probably represent eddies." (68) There is no
evidence for Hadley cell circulation in the lower atmosphere. Is
there any solid evidence for air descending at or around the
poles to the surface, as the greenhouse model requires? We do
know that the data at all sites showed that the lowest 20
kilometers of air is stable over the entire planet. That should
have been enough to eliminate that idea, but we find Hunt and
Moore suggesting: Infrared observations from Pioneer Orbiter
have led to the discovery of a significant cloud morphology in
the north polar region of Venus, which appears as a dipole
structure. It consists of two clearings in the clouds, in
locations straddling the pole and rotating around it in about
2.7 days. The clearings are thought to be evidence for
subsidence of the atmosphere at the center of the polar vortex.
(Emphasis added.) The absence of descending [air motions
elsewhere suggests that a large, single circulation [Hadley cell
may fill the northern hemisphere at levels near the cloud tops.
(69) On the other hand, Schubert states that these hot spots may
be lowering, in the cloud tops associated with descending motion
near the center of the polar vortex. However, other prominent
thermal features of the cloud level polar atmosphere are not so
obviously related to the descending motions of a polar vortex.
"[ Radiometer measurements at the poles [of Venus appeared to
confirm theories of a downward-moving polar vortex. But the belt
of atmosphere above the cloud tops proved to be about 10 C (18
F) hotter than similar regions at the equator." (71) Therefore,
cooler equatorial cloud top air masses that are hotter than
polar air masses, at the same altitude, should not blow toward
the poles. This type of motion would defy the Second Law of
Thermodynamics! There are other similar, supposed thermal
features in other areas of Venus' atmosphere, like those at the
poles, which show no signs that air is descending. Schubert
remarks that the "interpretation of the meridional wind
velocities measured by P.V. [Pioneer Venus probes in terms of
the mean meridional circulations...is only speculative and is
guided by other observations of wind speed and atmospheric
structure and theoretical ideas about the nature of the mean
circulation." (72) (Emphasis added.) Clark R. Chapman put the
situation into the clearest perspective when he said that "[
theorists began to expect there might be traditional Hadley cell
winds, with greenhouse-warmed air rising in the Venusian
tropics. But, after Pioneer Venus, the Hadley model remains a
plausible hypothesis in search of confirmation." (73) All the
evidence contradicts the notion that solar radiation is moving
heat to the poles or that cooler polar air is moving to the
equator. Why, then, are the scientists driven to find some
meridional Hadley cell circulation? Schubert reasons that, "[
while there is not actual evidence of indirect meridional cells,
there are strong theoretical reasons to expect that they exist."
(74) Chapman stated that greenhouse theorists expect Hadley cell
circulation. Schubert stated that there are strong, theoretical
reasons for their existence. This means that the greenhouse
effect requires them to exist, therefore they must exist. The
theory is determining what the evidence must say. In the
following segment of this paper, the reader will see the lengths
to which the astronomers have gone to make the evidence that
fully contradicts the greenhouse fit this theoretical belief.
Here, too, we see the same dismissal of evidence! Pollack sums
up the case being made: "The east-west winds on Venus blow in
the direction of the planet's rotation at all latitudes." (75)
The question that must be answered is, Why is the atmospheric
circulation on Venus zonal rather than meridional? Velikovsky
has proposed that this east-to-west circulation is caused by the
angular momentum of Venus' enormous tail of gas that fell to the
planet a few thousand years ago when it achieved its present
orbit. The enormous mass of that body of gas in the tail
descended, in a sweeping orbit, down and around the planet,
moving in one direction as it wrapped and enveloped Venus. The
great, angular momentum created is still moving the Venusian
atmosphere in a powerful super-rotation at all latitudes and
altitudes, east to west. According to Schubert: From the
dynamical viewpoint, the major challenge of the Venus atmosphere
is to explain its bulk super-rotation. We have seen that this is
westward at all latitudes and at altitudes between 10 kilometers
and 100 kilometers. Zonal wind velocity increases steadily with
height above the surface....The angular momentum density of the
atmosphere's rotation increases with height from the surface to
20 kilometers and decreases with height above this level. Most
of the atmospheric angular momentum is contained in the layer
between 10 kilometers and 40 kilometers....The problem facing
the dynamicist is to find the source of the excess atmospheric
angular momentum, and the processes which transport this
momentum both vertically and horizontally. (76) Venus' total
atmospheric angular momentum is greater than that of the Earth
by almost a factor of 200. This angular momentum would be able
to change the rotation of the solid planet by several hours.
This amount of angular momentum, 3.6 X 10 28 kg M 2 S -1, (77)
does not dissipate quickly. But, over millions, not to say
billions, of years, it should have dissipated if the greenhouse
heating effect was operating. The bulk of the atmosphere's
momentum is found some 10 kilometers (6.2 miles) above the
surface, up to 40 kilometers (25 miles) high, with an air flow
that is 19 miles thick. Like an air stream, the greatest force
of the current is in the region above the stream bed and below
the upper regions. This region on Venus is where the atmosphere
is as dense as possible, where the bulk of the atmosphere's mass
is found, where there is practically no topographical
obstruction below and where there are the fewest eddy motions.
As Schubert explained above, only one of the four Pioneer Venus
probes encountered eddy currents below 40 kilometers. (78) What
is, therefore, observed is a gravitational force like that found
in an oceanic stream. This is fully congruent with Velikovsky's
theory because Venus' tail, as it fell, would create such a
stream. The air masses below and above the stream are forced, by
contact with it, to move in the same direction, while, at the
very bottom of the atmosphere, the dense air is harder to move.
According to Jonathan Weiner, loops or rings of water break off
from the Gulf Stream into the Atlantic Ocean. These rings flow
in circles which are many miles in diameter, but they are not
whirlpools. The water inside and outside the rings is not
rotating at all. The depth of water rotating in the rings is 900
feet deep and these rings of motion may continue to flow from
four months up to several years. (79) If a ring of water flowing
in the ocean can last for several years, a shallow ocean flowing
in one direction would flow for tens of thousands of years. How
do the atmospheric scientists explain this motion? They have
only two forces with which to create super-zonal rotation. One
is the rotation of Venus, which is too slow to generate this
kind of circulation. The other is the Sun, which should produce
meridional Hadley cell circulation. What these scientists
suggest is that the very force which will generate Hadley cell
circulation --the Sun --can create eddies in the upper
atmosphere that move east to west predominantly and act as a
torque to create the same east-to-west motions below them. Of
course, no one believes that the Sun, which has sufficient
influence to produce super-zonal rotation, is doing this;
because, if it can do this, its influence would and should
generate super-meridional Hadley cell circulation by the very
same process, specially when that is the very nature of the
circulation that should be generated by the Sun. Oberg sums up
the unreality of the interpretation of super-zonal atmospheric
rotation. He finds it is a: puzzle [that awaits explanation, the
wind velocities in Venus' atmosphere.... Venus rotates at a
speed of only five mph [miles per hour at its equator, but these
cloud markings are traveling at a velocity 100 times that. On
Earth, jet streams in the outer atmosphere may occasionally
travel [20% or 30% faster than Earth's spin.... How could Venus'
upper atmosphere be propelled around the planet at such
disproportionate velocities? Initial meteorological computer
simulations could not account for speeds [anywhere near as high.
The dynamics of this atmosphere, which should have been so
simple, were increasingly puzzling. Although recent computer
models have been able to simulate the effect thought to have
been seen on Venus, they are rather strained and artificial.
(80) In essence, the scientists have explained super-zonal
rotation by the very force that explains super-meridional Hadley
cell circulation. The contradiction is so apparent that it
requires no further attention. As stated by S. S. Limaye, the
greenhouse model has still failed to explain the super-rotation
of Venus'atmosphere. (81) Once again, there is a fundamental
contradiction in what the scientists are proposing and none with
respect to Velikovsky's concept. After billions of years of
having greenhouse solar heat pump hot air to the poles from the
equator, on a slowly rotating planet, and back to the equator
via Hadley cell circulation, Venus' atmosphere should not
exhibit any significant zonal circulation at all. The entire
process, created by the scientists to have the Sun create
atmospheric zonal motion, is the complete antithesis to its
action. It is a futile operation, strained and artificial,
reminiscent of the inventions of Rube Goldberg.
_BALANCING THERMAL IMBALANCE
_Ultimately, what is the reason given for support of this
theory? The answer is that Venus must have a runaway greenhouse
effect operating because the planet is in thermal balance. If
Velikovsky was right, Venus, as a newborn planet in the early
cool down stages of it development, should be emitting much more
heat than is supplied to it by the Sun. It should have a thermal
imbalance; the nearer to the planet one measures infrared
emissions, the greater this imbalance should be between solar
input and infrared planetary output. Venus is not heated from
below its surface, we are informed by greenhouse advocates, but
by the greenhouse effect. It is made clear that measurements
prove, conclusively, that Venus is known to be in thermal
balance at all levels in its atmosphere and, therefore,
Velikovsky is wrong. As Carl Sagan stated: What I think
Velikovsky is trying to say here is that his Venus...is giving
off more heat than it receives from the Sun and that the
observed temperatures, on both the night and day sides, are due
more to the "candescence" of Venus than to the radiation it now
receives from the Sun. But this is a serious error. The
bolometric albedo (the fraction of sunlight reflected by an
observed infrared temperature of the clouds of Venus of about
240 K) that is to say, the clouds of Venus, are precisely at the
temperature expected on the basis of the amount of sunlight that
is absorbed there. (82) If Sagan's conclusion and analysis of
the measured data is correct, then, certainly, Velikovsky's
theory is dead. But Sagan's claim that Venus is in thermal
balance is contradicted by a series of measurements that show
that there is no thermal balance observed anywhere in Venus'
atmosphere, from its cloud tops to its surface!
_In 1978, George R. Talbott, a physicist whose specialty is
thermodynamics, carried out a fundamental calculation regarding
Venus' surface temperature. He did something quite commonly done
in laboratories all over the world. If a substance is heated to
candescence and then left to cool, a thermal analysis of its
properties with regard to heat conduction, radiation, etc., can
tell how long ago the substance was candescent. Talbott started
with a candescent Venus, 3,500 years ago, and determined what
its surface temperature would be after 3,500 years of cooling.
Of course, Talbott's calculations were much more complicated
than the simple analysis carried out in laboratories. What he
discovered after setting up all the possible parameters on a
computer and running the program was a surprise and a shock. He
started with a molten Venus with a surface temperature of 1,500
K and 2,000 K, allowed for heat transfer, internally, by flowing
cells of magma radiating into a heavy atmosphere, and found that
Venus' surface temperature, presently, was exactly 750 K --just
what the surface temperature presently is. (83) Some individuals
claimed that Talbott could not have reckoned correctly, because
the parameters governing Venus 3,500 years ago could not be
known with precision. On the other hand, overestimates of some
parameters could have been balanced by underestimates of others.
However, for Talbott to be wrong, as is --supposedly
--Velikovsky, Talbott's work would have had to be in error by
100%. Other than that, Venus is in thermal imbalance.
_As I will show below, the actual measurements of infrared
emissions from Venus, compared to solar radiation input at the
Venusian surface, do not contradict Talbott's work. By taking
the known surface temperature of the Sun and calculating the
distance to Venus, Venus' thermal balance or imbalance is
determined. At Venus' distance, the solar radiation will be
diminished to a particular value. One then calculates the
diameter of the planet with its atmosphere to determine how much
area intercepts this solar radiation value. What is most
important for the rest of the calculations is to determine, as
precisely as possible, how much light is reflected by the
planet's clouds and how much light or radiant energy is
absorbed. This ability of clouds to reflect light is called its
albedo. The higher the percentage of albedo, the more light is
reflected; the lower the percentage of albedo, the more light is
absorbed. This albedo figure must be known precisely, before it
can be determined, at the cloud top temperature of 240 K,
whether or not Venus is in thermal balance. Only a few
percentages of difference, say, 0.76 and 0.78, or 2%, at the
cloud tops, would have a pronounced effect on Venus and would
indicate about 10% more heat coming from the planet than is
supplied by sunlight. What do the measurements actually show? V.
I. Moroz presented some of the earlier measurement of Venus'
albedo. G. Muller measured it to be 0.878, or 87.8%, in 1893.
Andre Danjon derived a spherical albedo for Venus of 0.815 in
1949, while C. F. Knuckles, M. K. Sinton and W. M. Sinton
derived a spherical albedo for Venus, of 0.815, in 1961. (84)
What Moroz did was average the readings to get the best possible
indication of the actual albedo. The more acceptable
measurements are the most recent and use the latest technical
developments, specially those taken from spacecraft orbiting
Venus. These are fully discussed by F. W. Taylor et al. in an
article titled, "The Thermal Balance of the Middle and Upper
Atmosphere of Venus." The albedo found does not indicate thermal
balance, but thermal imbalance. The reader will learn that these
readings and their implications of a thermal imbalance were so
distressing to the investigators that they rejected all the
measurements showing that Venus was emitting more heat than the
sunlight was delivering. F. W. Taylor states: Measurements of
albedo are more difficult to calibrate than those of thermal
flux, because of the problem of obtaining an accurate reference
source. Using earth-based measurements, Irvine (1968) calculated
a (1968) calculated a value for A [albedo of 0.77 0.07, which
was later revised upward to 0.80 0.07 by Travis (1975). The
Pioneer Venus infrared radiometer had a 0.4 to 4.0 µm channel
calibrated by a lamp from which Tomasko et al. (1980b) obtained
a preliminary albedo for Venus of 0.80 0.02. Another approach to
determining the albedo is simply to assume that the atmosphere
is in net radiative balance...[by equation. In this way, a value
of 0.79+ 0.02- 0.01 has been obtained from Venera radiometry
(Ksanfomality, 1977, 1980b) and [a value of 0.76 0.006 [has been
obtained from Pioneer Venus emission measurements (Schofield et
al., 1982). Clearly the Pioneer measurements of emission and
reflection are not consistent with each other if net radiative
balance applies. (Emphasis added.) A source inside Venus equal
in magnitude to 20% of the solar input (i.e., accounting for the
difference between A= 0.76 and A= 0.80) is very unlikely, since
Venus is thought to have an Earth-like makeup, which would imply
internal heat sources several orders of magnitude less than
this. Also, even if such sources were postulated, it is
difficult to construct a model in which these fairly large
amounts of heat can be transported from the core to the
atmosphere via a rocky crust without the latter becoming
sufficiently plastic to collapse of the observed surface relief.
This could be avoided if the transport was very localized, i.e.,
via a relatively small number of giant volcanoes. Although
large, fresh-looking volcanoes do appear to exist on Venus...and
the composition of the atmosphere is consistent with vigorous
output from these, a simple comparison with terrestrial
volcanism shows that the volcanic activity on Venus would have
to be on an awesome scale to account for the missing 5 X 10 15 W
[watts, or so, of power. A more acceptable alternative is that
the preliminary estimate of 0.80 0.2 for the albedo from the P.
V. [Pioneer Venus measurements is too high, since the
uncertainty limit is now known from further work to be too
conservative. (J. V. Martonchik, personal communication.) A
fuller analysis of the P. V. [Pioneer Venus albedo data --still
the best, in terms of wavelength, spacial and phase coverage,
and radiometric precision, which is likely to be obtained for
the foreseeable future --is likely to resolve this puzzle. In
conclusion, then, the best thermal measurements of Venus WITH
THE ASSUMPTION OF GLOBAL ENERGY BALANCE yield a value for the
albedo of 0.76 0.1; this is the most probable value. (85)
(Capitalization added. Let us examine what was assumed as the
truth regarding the reasons for Venus being in radiative
balance. First, Taylor and his colleagues assumed that each of
the albedos measured by all the other investigators was wrong or
that the instrumental error range in every other investigator's
case was always on the minus side. There were three
measurements: one by Irvine of 0.77 0.07, revised upward by
Travis to around 0.80 0.07; another by Tomasko et al., using
Pioneer Venus instruments to obtain a value of 0.80 0.02; and
another, based on the assumption that Venus was in thermal
balance, by Ksanfomality, who used Venera instrumentation to
calculate an albedo of 0.79+ 0.02- 0.01. Thus, three albedo
measurements indicated that the reflection of light, in terms of
albedo, clustered around 0.80, the last two with tolerance
levels plus or minus well above 0.76, accepted as the emission
albedo by Taylor and his colleagues. If Venus reflected 80% of
the light incident to it, but allowed 4% more light than was
found by the emission albedo of 0.76, then the planet was
emitting 20% more heat than sunlight delivered. Usually when a
group of scientific measurements cluster around a particular
value, as the 80% albedo did, scientists assume that the
averaged value of these readings is a fairly good indication of
the actual figure. By averaging the measurements, scientists
achieve the best approximate value. However, since it was
unthinkable that Venus could be in radiative imbalance, even
based on one measurement that assumed balance but arrived at a
figure of A= 79%, J. V. Martonchik reevaluated the Pioneer Venus
data that gave an albedo of 80% .02% and recalculated the
possible instrument error to make it large enough so that, on
the minus side, it would agree with the lower 76% emission
albedo. This was presented in a private communication that could
not be analyzed by other investigators to determine whether or
not Martonchik's correction was itself without error. Second,
Taylor and his colleagues assumed that Venus must possess an
internal heat source almost equivalent to that of the Earth.
Since the Earth generates an internal heat value much smaller
than the value that suggests a 20% imbalance on Venus, they
concluded that Venus, itself, could not be responsible for this
additional heat. If Venus' emissions were actually this much
greater, they said, Venus would have to be enormously volcanic,
and --in the next breath --said Venus appears to exhibit a
highly volcanic surface. They also admit that the Venusian
atmosphere appears to contain the gases consistent with
vigorous, volcanic outgassing. But all these correlations mean
nothing. Taylor and his collleagues say such agreement between
thermal imbalance and Venus' volcanic surface and atmosphere is
too incredible to accept, and reject all of this on the one
assumption that Venus must be in thermal balance. Yet their
conclusion states that the 0.76 0.01 albedo is the most probable
value. There is no evidence to suggest this. Nevertheless, if
this assumption is correct, it should be corroborated by all the
other readings taken by Venera and Pioneer Venus probes. These
readings should exhibit demonstrable evidence of radiative
balance throughout the rest of the Venusian atmosphere. This, in
fact, is not the case. In fact, all the other readings deliver a
death blow to any assertion that Venus ' atmosphere is in
thermal balance. If the runaway greenhouse effect is correct,
not only must the cloud tops exhibit thermal balance between
solar input and infrared thermal output, but the lower
atmosphere must show the same. If, as Velikovsky claims, the
greenhouse effect presents only a minor contribution to Venus'
high thermal emission, then as one gets closer to the surface of
the planet, the measurements should show an even greater
radiative imbalance than the 20% suggested by the cloud top
readings. The nature of establishing radiative balance in an
atmosphere is explained thus, "Radiative balance occurs [on a
planet at every level when the amount of downward, directed
solar radiation that is absorbed is equal to the amount of
infrared radiation that is emitted upward. When local
temperature satisfies this balance, the atmosphere temperature
is maintained." (86) (Emphasis added.) M. G. Tomasko further
reinforces this concept: In a steady state, the algebraic sum of
the atmospheric heating and cooling rates due to all physical
processes should [equal zero at each location. At a given
location, the heating and cooling rates depend on the state of
the atmosphere: its temperature, pressure, composition,
radiation and wind fields. A successful steady-state model for
the thermal balance of Venus' lower atmosphere will include the
relationship of the heating and cooling rates to the atmospheric
state, and show that the atmospheric structure leading to net
zero heating or cooling at each location is equal to the
observed structure. (87) What, then, do the Pioneer Venus probes
that entered the atmosphere show regarding this? According to
Tomasko, "Among the most accurate measurements of the
temperature-pressure structure of the lower atmosphere of Venus
[we find those made by the four Pioneer Venus (PV) probes....The
probe entry locations...vary in latitude from 30 South to 60
North [and measure Day and Night...temperature profiles...."
(88) According to Richard A. Kerr, the editor of Science: When
Pioneer Venus probes looked at the temperature, each one found
more energy being radiated up from the lower atmosphere than
enters it as sunlight....To further complicate the situation,
the size of the apparent upward flow of energy varies from place
to place by a factor of [two, which was a disturbing discovery.
(89) It is impossible to believe that in one area the greenhouse
effect is twice as efficient as in others. From Velikovsky's
theoretical viewpoint, parts of Venus' surface, known to the
scientists as coronea, or hot spots, are much hotter than other
areas of the surface. This would clearly explain these
measurements. From the National Aeronautics and Space
Administration (NASA) publication, Pioneer Venus, we have the
following: The measured, infrared fluxes [upward from Venus show
several anomalies, the origin of which is still being debated.
Taken at face value, the anomalies suggest that parts of the
atmosphere are transmitting about twice the energy upward than
is available from solar radiation at the same level. (90) It is
obvious that wind motions, pressures and all the other
atmospheric conditions in Venus' atmosphere will not create a
50% imbalance. While the cloud top indicated a 20% thermal
imbalance farther down in the atmosphere, the Pioneer Venus
probes revealed a 50% radiative imbalance. This, of course, is
in full agreement with Velikovsky's concept that the extremely
hot planet's surface is the major heat source, indicated by
greater fluxes of infrared closer to the thermal source. This
finding was anathema to the investigators, as was the imbalance
measured at the top of the cloud cover; but, What was to be done
about these most accurate readings? Tomasko tells us exactly
what some scientists did and why: The thermal flux profiles are
surprisingly variable from site to site, in view of the great
similarity in temperature profiles measured at these sites. In
addition, at both the Night and North probes sites, they are
much greater than the globally averaged solar net profile at low
altitudes, implying a substantive radiative imbalance in the
lower atmosphere. (Emphasis added.) In view of the large and
variable nature of these flux measurements, the investigators
have searched for instrumental problems which could have
affected the measurements and have found one that could have
systematically increased the measured thermal net fluxes....The
authors believe that they understand the vertical dependence of
the flux errors, and by adjusting the fluxes to reasonable
values, at low altitudes, they have derived corrected fluxes.
(91) (Emphasis added.) Corrected values are not really valid
values. Not only did the scientists correct the two highest
readings to "reasonable values," meaning thermal balance values,
they corrected every probe reading because every probe showed
strong radiative imbalance at all levels of the atmosphere
--much as was found for the cloud tops. Based on the
investigators' beliefs, they simply made the data fit the theory
of a greenhouse in radiative balance. However, one may be quite
sure that, if the readings corroborated their beliefs of thermal
balance, we would be showered by this direct confirmation of
theory. But these measurements did not exhibit any evidence for
balance. As Kerr admitted, "The much ballyhooed greenhouse
effect of Venus' carbon dioxide atmosphere can account for only
part of the heating, and heating, for other mechanisms is now in
turmoil." (92) In essence, the thermal imbalance at the cloud
tops was corroborated by Pioneer Venus probes below the clouds,
so one can be confident that such is also the case throughout
the entire Venusian atmosphere. What must also be pointed out is
that the Pioneer Venus probes did not measure radiation all the
way down to the surface. According to Seiff, "[ temperature data
were not obtained by the Pioneer probes below 12 kilometers [7
miles altitude." (93) Tomasko indicates that "[ the data from
the temperature sensors of all four [Pioneer Venus probes
terminated at 13 kilometers altitude." (94) From this fact, one
would expect that, based on Velikovsky's concept, the Venera
probes that did approach the surface, measuring the solar fluxes
in and infrared thermal fluxes emitted from the surface, would
show an even greater radiative imbalance than did the Pioneer
probes. In fact, that is what they did! Seiff states: The
heating rates needed to warm the atmosphere from the Day probe
[Pioneer Venus profile to that of Venera 9 integrated over
altitude...is 45 times the midday solar heat absorbed at 30
latitude....This is also true for the Venera 10, 11 and 12 data
relative to the large probe data, for which necessary heating
rates integrated over altitude are> [somewhat less than 40 times
the mean dayside solar input for the albedo of 0.71. (95)
(Emphasis added.) On page 219 of his article in Venus, Seiff
essentially admits the same thing. The average reading from the
Venera probes showed solar radiation absorbed by Venus. The
surface infrared fluxes emitted were around 40 times more than
enters Venus' atmosphere as sunlight. The tremendous rise in
infrared heat nearer to the surface is similar to the heat
emitted by a white-hot block of metal, in that, as one puts
one's hand near the block, the heat rises, but, at a certain
closer distance to the block, the heat rises immensely. This
makes sense in terms of the greenhouse effect as well. The
regions where most of the Sun's radiant energy is absorbed
would, at those altitudes, generate the strongest greenhouse
effect. Bruce Murray points out that On Venus,...a smaller
fraction of the incident solar energy penetrates the atmosphere
all the way to the surface. Most of it is scattered back into
space to provide the bright image that is seen through the
telescope; much of the remainder is absorbed within the
atmosphere. Thus, Venus' atmosphere is heated more at the top
and middle than at the bottom, and, in this sense, resembles
more the shallow seas on Earth than its atmosphere. (96) The
ocean is an excellent greenhouse, but sunlight is primarily
absorbed at the upper 300 feet and this is the warmest region of
the oceans. This explains why the solar greenhouse effect is
greater at the cloud tops compared to Venus' output --by 80% of
infrared heat energy, while the greenhouse effect's energy
becomes reduced to 50% well below the clouds, and to 2.44% of
infrared emissions given off by the planet at the surface. The
regions of greatest solar absorption have the strongest
greenhouse effect, compared to that emitted by the planet. The
regions of least solar absorption have the weakest greenhouse
effect, compared to that emitted by the planet. This apparently
is true at Venus. Furthermore, all the readings showed the same
clustering of values, of nearly 40 times greater than the solar
radiation input, which strongly suggests that the readings were
basically correct. The scientists found these measurements so
repugnant to their theoretical greenhouse concept that they were
dismissed. Seiff tells us that "it is clear that the Venera 9
Day probe differences cannot be induced by solar heating but
must be ascribed to other processes or to measurement
uncertainties." (97) All, and I stress, all of the measurements,
from the cloud tops to the lower atmosphere to the surface, gave
consistent readings of radiative imbalance --contrary to
everything greenhouse advocates claim. No single set of probe
readings by Pioneer Venus or Venera suggests, in any way, that
scientists have clear measurements supporting their contention
of thermal balance. Every reading is another nail in the coffin
of their theory. Realizing this, their actions to ignore or deny
these findings point to a rigidity that has no place in science.
This rigidity of thought is expounded in Pioneer Venus, a NASA
publication. Let us remember von Braun's admonition that the
greenhouse effect is unproven by experiment. One of the primary
objectives of the Pioneer Venus Multiprobe mission was to test
thoroughly the belief that the "greenhouse effect" is
responsible for the high surface temperature. (Emphasis added.)
[After describing the measured thermal imbalance described
above, they continue. Possible instrumental errors in this
difficult measurement may be responsible. A possibility is that
two of the probes entered regions that are unusually transparent
to thermal radiation, but this is rather unlikely because much
of the absorption [of infrared is due to ubiquitous carbon
dioxide, which makes up nearly all the atmospheric gas. The
suggestion has been made that heat balance oscillates around an
average state and that the anomalous measurements were made
during the heating phase [Venus' temperature goes up and down
over time with respect to its balance temperature and the
probes, just by coincidence, descended on Venus during the
heating period. In spite of these difficulties in interpreting
some of these observations, the greenhouse effect, coupled with
global dynamics, is now well-established as the basic
explanation of the high surface temperature. (98) At every step
of the investigation, every measurement showed radiative
imbalance wherever readings were taken in the Venus atmosphere;
and, at every step, every measurement that contradicted the
runaway greenhouse effect concept of thermal balance was either
changed, culled or set side based solely on a theoretical belief
that Venus must be in thermal balance. We have observed this
irrational behavior, of setting aside evidence negative to
greenhouse assumptions, from the beginning of this investigation
right up to the end, based only on the theoretical greenhouse
consideration. Why take measurements if the scientists are not
willing to accept any that contradict their theory? Needless to
say, one can fully comprehend the nature of what has been going
on with the evidence as handled by the greenhouse theorists and
its advocates. It is sheer hypocrisy to suggest that the rules
of science governed the way this data has been handled. But,
finally, let us return to George Talbott's analysis of the
cooling of Venus from a molten state to its present 750 K
temperature. When we apply the findings of the Venera probe's
surface measurements to analyze what contribution the greenhouse
effect makes and what is contributed by the planet, a most
interesting set of figures emerges. The Venera surface readings
indicate that Venus emits about 40 times more heat than sunlight
imparts. Simple algebra shows that X= solar radiation plus 40 X=
the internal planetary radiation together= 750 K, the surface
temperature. X+ 40 X= 750 K 41 X= 750 K X= 18.3 K, solar
radiation input 40 X= 731.7 K, planetary internal heat
Therefore, Talbott's analysis of the cooling of Venus, to derive
its present surface temperature from a molten state, illustrates
a high degree of accuracy. The 18.3 K solar input to the 731.7 K
planet's internal heat shows that Talbott's percentage of error
is no more than 2.44%, which is an extremely small value. But
even if we double this error range, or triple it or quadruple
it, Venus clearly appears to have an enormous radiative
imbalance. The entire concept of the runaway greenhouse is
supported by expediently using procedures that accountants and
economists call "smoke and mirrors," not to say, pure denial of
the facts. Velikovsky's theory regarding the thermal nature of
Venus is in complete harmony with the real evidence and the
actual measurements. The history of the advocates of the runaway
greenhouse mechanism has been to give the theory a presumptive
status precluding the notion that it must stand or fall on the
basis of the evidence. But, as has been demonstrated, whatever
the evidence indicates plays little or no role in the status of
the theory. I suggest that such methods employed to support the
runaway greenhouse theory are antithetical to any science and
reflect, instead, the rigid thought processes of its advocates
rather than inductive science. How else could so much negative,
inconvenient data be changed or remain unrecognized? At every
level at which the theory is examined or analyzed, it fails on
the basis of the evidence. One is forced to assume that no
conceivable, negative finding that sorely contradicts the theory
will ever find acceptance by these investigators. Such an
adherence to theory, as dominant in science, is really only
dogmatism in disguise. It is extraordinary that scientists can
allow theory to blind them to the facts. James E. Oberg, a
strong advocate of the runaway greenhouse effect and vocal
critic of Velikovsky, stated that "the `runaway greenhouse
effect' is still in the running." (99) However, Professor Irving
Wolfe, in a recent telephone conversation, told me what
Velikovsky claimed would eventually happen. "The greenhouse vill
go avay," he said. (100) The reader is left to draw his own
conclusions about whether the runaway greenhouse effect is still
in the running or will go away. It is quite clear that there is
a greenhouse effect on Venus --not a runaway greenhouse effect
--and that Velikovsky's concept is well-supported by the
evidence.
_References
#Post#: 239--------------------------------------------------
Re: Mathis on Velikovsky +
By: Admin Date: December 24, 2018, 6:02 pm
---------------------------------------------------------
The Surface Of Venus -- "A Newborn Babe" [Aeon Journal]
From: Aeon III:1 (Nov 1992)
_The Surface Of Venus-- "A Newborn Babe", Charles Ginenthal
_Strange, when you think about it, how a lack of information so
often grows by leaps and bounds into a belief that has no
scientific basis but becomes "accepted fact" simply because
enough people want to believe it. Few things irk men of science
(and they aren't all that honest) more than having to respond to
questions with a puzzled look on their faces and a a collective
shrug of shoulders. People have a nasty habit of assuming that
scientists should know about those matters on which they're
questioned-- if for no other reason than that scientists spread
this belief and spend great sums of money collecting
information. But with all his instruments and a lifetime of
study, the scientist doesn't really have the faintest idea of
what it may be like on Venus. Oh, he's got ideas (most of them
horribly wrong), but he does not know. If you don't know-- at
least say something. Don't quite make up out of thin air.
Deduce. If you have only a shred of cloth, weave yourself a
magnificent set of clothes by mixing liberal amounts of
imagination with that shred. That's just about what happened
with what we thought we knew about Venus. The theories were both
serious and preposterous. They were sincere and they were
outlandish. They were well intended and they were based on
everything we knew about Venus, but people couldn't separate
minimum fact from maximum imagination, and what emerged was
gibberish. Martin Caiden, Planetfall (New York, 1974), p. 138 In
1950, Immanuel Velikovsky claimed that the testimony of ancient
peoples from all parts of the globe described Venus as a giant,
brilliant comet. Based on Velikovsky's analysis of this data he
drew the conclusion that Venus was a newborn planet in the early
cool-down stage of its development. Therefore, if his
understanding of the evidence was correct then Venus' surface
should exhibit all the conditions of a world that was very
recently molten and is most likely still volcanic and
geologically active. In 1985, Dr. Lawrence Colin, Chief of the
Space Science Division at nasa's Ames Research Center and
co-editor of Venus, wrote:...Our knowledge of Venus was still
seriously limited in the early 1960s prior to mankind's first
rendezvous by spacecraft. In 1961 competing views of Venus could
be classified in seven broad categories: 1. moist, swampy,
teeming with life. 2. warm, enveloped by a global carbonic-acid
ocean. 3. cool, Earth-like, with surface water and a dense
ionosphere. 4. water, massive precipitating clouds of water
droplets with intense lightning. 5. cold, polar regions with ice
caps 10 kilometers thick and a hot equatorial region far above
the boiling point of water. 6. hot, dusty, dry, windy global
desert. 7. extremely hot and cloudy, with molten lead and zinc
puddles at the equator, seas of bromine, butyric acid and
phenols at the poles. From this list it is not obvious that
scientists were all describing the same planet. For those who
are impatient about the outcome, speculation 6 appears to
represent most closely what we now think Venus is like. (1)
Reinforcing the sixth option Ernest J. Opik, the internationally
known astronomer of Armagh Observatory in Northern Ireland,
stated in 1960: The modern picture of Venus...[is a borderless
desert extending over an area one hundred times that of the
Sahara...[The Sahara itself would appear a paradise compared
with the dry and suffocating dust storms raging behind the
brilliant deceitful face of the Evening Star. (2) Nowhere was it
ever suggested by establishment scientists that Venus would be
found to be a volcanic cauldron covered by immense lava flows.
In fact, as recent as 1989, Isaac Asimov, the late popular
science writer, remarked: For years astronomers had believed
that Venus was a geologically dead place. Although quakes,
volcanoes and other activity surely wracked the planet at one
time, it seemed certain that Venus was quiet today. (3)
Therefore, if Velikovsky's analysis of the ancient testimony is
correct the observations by the Magellan spacecraft should not
only contradict the previous models of the Venusian surface but
should also show overwhelming evidence of recent stupendous
volcanism on a surface that appears to be pristine. One of the
first indications of this excessive volcanism was presented in
May 1990 in the Journal of Geophysical Research which analyzed
the sulfur content of the Venusian clouds. There Na Y. Chan et
al. state: Results of recent International Ultraviolet Explorer
(IUE) observations of Venus made on January 20, 1987, and April
2 and 3, 1988, along with a re-analysis of the 1979
observations...are presented. The observations indicate that the
amount of sulfur dioxide at the cloud tops of Venus declined by
a factor of 84 from 38070 ppb [parts per billion to 5020 ppb in
1987 and 1988. (4) One of the researchers of this phenomenon,
Larry Esposito from the University of Boulder Colorado,
elaborated on this decrease of SO 2 and SO two months later in
Astronomy: Pioneer Venus has continued to monitor these
constituents above the clouds. Over the years a remarkable
discovery has emerged: both sulfur dioxide and the haze have
been gradually disappearing. By now only about 10 percent of the
1978 amount remains. This disappearance has also been confirmed
by the Earth-orbiting International Ultraviolet Explorer between
1979 and 1987 and other Earth-based observations. The haze and
the sulfur dioxide are now approaching their pre-1978 values.
Analysis of recent Earth-based radio observations by Paul
Steffes and his colleagues show less sulfur dioxide below the
clouds than was measured by Pioneer Venus and Venera landers,
which is also consistent with the decrease of sulfur dioxide.
Inclusive Earth-based data show that a similar phenomenon may
also have occurred in the late 1950s. The best explanation right
now for the decrease is that from time to time major volcanic
eruptions inject sulfur dioxide gas to high altitudes. The haze
comes from particles of sulfuric acid, which is created by the
action of sunlight on sulfur dioxide...Being heavy the particles
gradually fall out of the upper atmosphere, letting conditions
up there return to normal between eruptions. My calculations
show that this eruption of the late 1970s was at least as large
as the 1883 eruption of Krakatoa. The explosion, equal to a
500-megaton H-bomb, was the most violent of the last century or
so shooting vast quantities of gas into the Earth's
stratosphere. (5) Some scientists have already drawn the same
tentative conclusion posited by Esposito. Thus James Pollock
states: Measurements by the Pioneer Venus Orbiter show that the
amount of sulfur dioxide present near the cloud tops declined
from approximately 100 parts per billion (ppb) in 1978 to about
10 ppb in 1986. There is also fragmentary evidence of similar
increases and decreases at earlier times. Such fluctuations
might be due to episodic injections of SO 2 high in the
atmosphere by powerful volcanic explosions. (6) David Morrison
and Tobias Owen put the case even more strongly: Observations
over the past twenty years have indicated that large
fluctuations occur in the concentration of sulfur dioxide (SO 2)
in the atmosphere of Venus above the clouds. When these
observations are combined with indications of volcanic
topography and lightning discharges for possible volcanism, the
case for erupting volcanoes on Venus becomes rather strong. (7)
This appears to be indirect evidence that at least twice in the
1950s and 1970s there were major volcanic eruptions on Venus'
surface.
_There are, of course, questions and objections related to this
analysis; nevertheless, the Magellan spacecraft may have already
observed explosive volcanism. In the December 1990 issue of
Scientific American appears a photograph made by Magellan which
appears to exhibit exploded material from one of its craters.
The caption accompanying the picture states: Explosive volcanism
may be responsible for the radar-bright deposit that extends
roughly 10 kilometers from the kilometer-wide volcanic crater at
the center of the image. The etched pattern of the surrounding
plains becomes more obscure closer to the crater, which
indicates that the deposit is thickest near the crater. The
shape of the deposit suggests that local winds either carried
the plume southward or else gradually eroded away the plume
material except for that part located in the volcano's wind
shadow. These bits of information, though consistent with
volcanic activity, need to be corroborated by other information
that will give a more comprehensive picture of a planetary
surface formed by massive volcanic processes. In this respect,
we turn our attention to another body in the solar system that
is in the throes of massive, violent, ongoing volcanism and
exhibits several notable features related to this Venusian
phenomenon. That body is Io, the inner Galilean satellite of
Jupiter. As Io orbits around Jupiter it is constantly being
distorted in shape by its tidal interactions with the very
massive Jupiter and its three outer Galilean satellites. As Io
is distorted and flexed, like the action produced by bending a
spoon, enormous heat is generated producing volcanism.
Therefore, Io is molten at a relatively low depth of its surface
and its thin crust is floating on an ocean of molten magma. The
amount of heat emitted by Io, according to David Morrison (a
member of the imaging science team for the Voyager spacecraft)
shows: "[ An internal heat source-- estimated at 10 14 W--
needed to drive this volcanism is two to three orders of
magnitude [100 to 1000 times greater than that expected from
normal radionucleides..." ( 8 ) Io is the most volcanic body in
the solar system. According to Billy Glass: The volcanic
eruptions [on Io appear to be comparable in intensity to the
greatest terrestrial eruptions which are rare on the Earth...Io
appears to be volcanically more active than the Earth. This has
made mapping Io difficult because the active regions undergo
radical changes in short periods of time. In the four month
interval between Voyager 1 and Voyager 2, for example, one of
the largest (200 km diameter) [122 miles eruptive centers on Io
known as Prometheus was transformed from a heart shaped feature
to a circular one. (9) Hence, if Venus was an incandescent body
3500 years ago and then cooled to the point where it became
molten before it arrived at its present state, it should exhibit
a topography quite similar to that of Io. In essence the
volcanic forms observed on Io should generally be representative
of the surface features seen on Venus. There should, of course,
be differences between the bodies because Io's temperature is
not decreasing whereas we presume that Venus' temperature is.
Furthermore, there will be differences in the materials each
body contains which will also affect the appearance of their
surfaces. Before comparing Io and Venus we wish to point out
that many of the volcanic craters on Io do give the appearance
of impact craters. According to Carr et al.: Calderas occur in
every region of Io so far photographed. They are generally
recognizable by their strong resemblance to terrestrial and
Martian calderas. In many cases no relief can be detected and a
caldera is inferred from the presence of a dark circular
feature....Over 5% of the Ionian surface seems to be part of a
caldera, either dormant or active. Where relief is discernible
the calderas are recognized as rimless depressions with steep,
inward-facing scarps and relatively flat floors. (10)
_Plains Vulcanism
_David Morrison describes Io's volcanic features as follows:
Some of Io's volcanic features look a great deal like their
terrestrial counterparts: low shield-shaped constructs with
calderas at their peaks and flows of erupted materials on their
sides. However, most of Io's calderas are not at the tops of
mountains but instead appear to be scattered amid the plains.
(11) Io exudes its magma in this manner because it is
tremendously hot internally and has an extremely thin crust.
Therefore if Velikovsky was right that Venus was hot internally
just below its thin crust it too should pour forth its magma
after the fashion of Io. Observations should show evidence that
lava is either presently or has very recently been exuded from
circular vents on the plains of the Venusian surface. In New
Scientist we learn that radar shows lava flows on Venus are
indeed very much like those on Io: The flat plains of Venus
consist of lava that has flowed from the planet comparatively
recently, according to latest radar results. And an appreciable
amount of the planet's heat may escape through these lava flows,
rather than through large volcanoes and rift valleys that
geologists have known for some years. In the plains the
researchers found dozens of small vents, which oozed lava
without forming volcanic cones. The researchers say, "The large
number and wide distribution of vents in the lowlands strongly
suggest that plains volcanism is an important aspect of surface
evolution and contributed to heat loss on Venus". (12) Thus,
there is a basic similarity that strongly suggests that Venus is
venting its internal heat through plains volcanism. This implies
that Venus, like Io, has a thin crust and is extremely hot not
far beneath that crust.
_The Nature of Io's and Venus' Craters
_Since Io possesses such a thin crust floating on a bed of
magma, that crust can become deformed. Io's craters are situated
over the upwellings of the hottest magmatic flows and,
therefore, distortion of the crust should be in evidence most
strongly at these sites of upwelling. This, indeed, has been
well observed by Voyagers 1 and 2. Carr, et al., describe the
crater caldera shapes in this manner: "Although most [craters
are nearly circular, they range widely in shape; some have
scalloped walls suggesting collapse about different centers,
others have rectilinear outlines, and others have elongate,
slot-like shapes." (13) One of the first reports from Magellan
respecting non circular craters on Venus was presented in the
New York Times for Sept. 18, 1990. There it was reported that a
kidney-shaped crater had been observed. The explanation given to
explain this unusually shaped structure was that the
"kidney-shaped crater appeared unlike any other in the solar
system. Perhaps an incoming meteor broke up as it passed through
the dense Venusian atmosphere, causing several large chunks of
material to strike almost simultaneously in an irregular
pattern." (14) However, over time more and more irregular shaped
craters were observed so that the first example could no longer
be considered unique. Thus an article in Discover states, "Even
Venus' meteorite craters are intriguing. Some have strange and
irregular shapes, in puzzling contrast to the round outline
typical of most impact craters in the solar system." (15) So far
as is known only two worlds-- Venus and Io-- exhibit very large
numbers of misshapen craters. This again strongly implies that
they were created in the same way under similar conditions. That
is, both Venus and Io are highly volcanic and have thin crusts
floating on magma: "Lunar craters, like terrestrial impact
craters tend to be circular, whereas calderas do not." (16)
Geophysicists have generally considered misshapen craters as
volcanic structures on the Moon and on Io. However, when they
observe misshapen craters on Venus in which nearly all craters
over 12 miles in diameter are observed to be filled with lava
and in which a percentage have lava rivers emanating from them,
the scientists have changed their interpretation to suggest that
the craters are no longer of volcanic origin but of impact
origin. If Io's and Venus' craters were, indeed, generated by
similar processes then they should also show common features
other than their non-circular shapes. For example some of Venus'
craters are quite deep. Thus Dr. Gordon H. Pettengill, a leader
of the Magellan radar team, reported that the spacecraft's first
altimeter measurements were defining the texture of the planet's
topography. One surprise, he said, "was discovering that a
previously surveyed impact crater named Colette is more than two
miles deep-- far deeper than any crater seen on the Earth or any
other planet." (17) On Io, too, we find that "some calderas are
several kilometers deep" (18) Moreover, there is another level
of resemblance between the craters of Io and Venus that strongly
suggests that Venus' craters are of volcanic rather than impact
origin. Because Io's craters are accepted as having been
produced by volcanism the outflows of rivers of lava from them
is not considered enigmatic to the space scientists. In this
regard it is reported: One of the most striking aspects of Io's
calderas is the associated albedo patterns. The floors of most
are very dark and the low reflectivity of many is accentuated by
bright haloes around the craters....[Sulfur rendered molten by
heat from silicate magmas...may be the source of some of the
river like features that snake across Io's surface...The flows
from one of Io's craters are very long stretching for hundreds
of kilometers. (19) R. Stephen Saunders reports of one Venusian
crater: "The crater's flat, smooth floor hints that it has been
flooded with lava." (20) Saunders exhibits photographs of
Venusian craters which show dark floors with bright halos around
them and then informs us that: "River-like erosion features
running from the largest crater in the image are as yet
unexplained." (21) The reason for this difficulty is, of course,
that the interpretation of these long river-like structures from
the craters suggests that the craters are not impact formations
but volcanic creations. With respect to this long river, Andrew
Chaikin writes: One of the most bizarre features yet identified
on Venus is a remarkably long and narrow channel that Magellan
scientists have nicknamed the river Styx. Although it is only
half a mile wide, Styx is 4,800 miles long. What could have
caused such a channel is unclear. Water, of course, is out of
the question. Flowing lava is a possibility but it would have to
have been extremely hot, thin and fluid. (22) One further
resemblance between the craters of Io and Venus is their general
size or diameter. Billy Glass observed that the craters
depressions on Io are "up to 200 km in diameter." (23) On Venus
it is assumed that any crater larger than 300 km would settle by
rheological flow in about one billion years. (24) Sulfur is the
fluid suggested as being responsible for river structures on Io.
However, the River Styx runs up as well as downhill. What is
clearly implied, if this feature is a flow, is that the surface
topography has shifted greatly since the flow ceased.
Furthermore, Science News reports recent changes on Venus that
have been attributed to wind blown debris but a deep regolith
has not been seen anywhere on Venus and the scientist who
discovered the changes also suggests that the differences
between the 1991 image and another taken months later "may stem
from an actual surface change." (25) The largest craters so far
observed are about 275 km in diameter. This implies that a
molten body like either Io or possibly Venus would produce
craters of this size and smaller. This, of course, is still to
be determined by the full scale observation of Venus by
Magellan. If this evidence holds up it will again imply that
Venus is molten at shallow depth. This however, does not negate
the possibility that tidal forces on solid bodies such as the
Moon may generate larger craters such as the Maria basins. In
summarizing the information about craters one notes that their
shape, depth, size, and bright halos around craters and dark
flat centers bearing river-like lava flows on both Io and Venus
are strong indications that volcanism is the cause of these
surface features. One can also add that both Io and Venus
possess craters with central peaks and craters without central
peaks which can be seen in any good collection of photographs
made of these bodies. To some extent confusion reigns in the
analysis of Venus' craters as impact structures. Consider the
problems posed by the crater known as Cleopatra. Here Burnham
points out: Cleopatra is an impact crater surrounded by terrain
that has been extensively modified by volcanism, probably
induced by the impact. According to present thinking, if there
was enough volcanic material available close to the surface so
that it could spill out after the impact, then Maxwell [a nearby
mount itself would have softened and slumped to a much lower
elevation. What is the answer? No one knows yet. (26) In no
manner at all does impact cratering explain Cleopatra. Rather,
as is the case with most volcanic craters, a vent made its way
up to the slopes of Maxwell Montes and broke through the surface
creating a large crater and pouring lava over the surface.
Significantly, Burnham reports that, "All craters larger than
about 20 kilometers across have interiors at least partially
flooded with lava." (27) [italics added. From this it is quite
clear that volcanism rather than impact is the dominant cause of
cratering on Venus.
_Pancake-Shaped Domes and Other Anomalies
_Among the strangest features found on Venus is a series of
pancake-shaped domes. This surprising discovery was recounted in
the New York Times as follows: At the news conference yesterday,
Dr. R. Stephen Saunders, the [Magellan project's chief
scientist, showed pictures of...pancake-shaped domes which he
said were "features never seen before" on any planet. In one
region, seven domes remarkably similar in size stretch out in a
line remarkably straight for nature...They were presumably
formed by extreme viscous lava pouring out of volcanic vents.
The pattern "is telling us something about the eruption
mechanism, the viscosity and the eruption rate.' But that was as
far as geologists ventured in the interpretation. (28) The
unusual shape of these features should have struck a chord
somewhere among the planetary geologists because pancake-shaped
domes have also been observed on Io. Thus Carr et al., inform
us: While most calderas [on Io do not seem to be within sharply
defined edifices, a variety of positive relief features are
recognizable. Most are puzzling and difficult to relate to
terrestrial landforms. Among the more comprehensible because of
their resemblance to low volcanic cones, are two pancake-like
constructions...They are nearly circular, and surrounded by low
escarpments. Each has a bright-floored small crater in the
middle. The albedo [reflection of light by the material of the
main edifice is uniform and close to that of the surroundings.
(emphasis added) (29) Once again two worlds-- Venus and Io--
share a unique feature seen nowhere else. Of course, normal
volcanic domes have also been observed on Venus. Here Eberhart
reported: Beneath Venus' acrid clouds which perpetually shield
its surface from the eyes of Earth-bound observers, lie tens of
thousands of low dome-shaped features. For several years
planetary scientists have pondered the origin and significance
of these gentle mounds, which have appeared in radar images made
of the planet since 1983. Apparently the result of volcanism,
the domes constitute "the most abundant geological feature on
the planet" says Jayne C. Aubele of Brown University: "I'm
excited about the domes and other scientists are beginning to be
also" Aubele says "the presence of a volcano on the surface of a
planet always tells us something about the planet. The presence
of tens of thousands of volcanoes overwhelms me". (30) Although
the number of domes on Venus of volcanic origin may turn out to
be smaller in number when Magellan completes its survey, the
great number clearly indicates how abundantly volcanic Venus
must be. One researcher sums it up this way: "Magellan's radar
survey of Venus found thousands of small volcanoes dotting the
mostly flat landscape, as well as mountainous volcanic
structures several hundred kilometers in diameter and evidence
of massive outpourings of lava." (31) Later we are informed
that, "Magellan has found no evidence of gradual resurfacing."
This suggests that Venus lava flows were immense in scale, which
is what Velikovsky's concept requires.
_Hot Spots
_For some time now it has been known that certain areas on Io
are far hotter than the surrounding surface terrain. Such areas
are described as "hot spots." Here Morrison tells us, "In Io's
case nature has aided us by channeling much of the heat flow
into a few small areas resulting in hot-spots with temperatures
far higher than the ambient background." (32) Alfred McEwen et
al., suggest that, "Observations...show that most of the hot
spots [on Io have remained relatively stable in temperature,
location and total power output at least since the Voyager
encounters and possibly for the last decade." (33) Hotspots have
been associated with surface features on Venus for a very long
time; they were originally found by Earth-bound radar and
confirmed by Venera spacecraft. (34) James Head asks: The
question with arguably the broadest implications is simply how
has Venus chosen to get rid of its internal heat (emphasis in
original). Does Venus cool itself by sending magma directly from
the interior to the surface? Then we would expect to see
widespread volcanic deposits and numerous "hot spots," like
those on Jupiter's satellite Io. (35) Thus the presence of
hot-spots suggests that Venus-- like Io-- is venting its heat
via hot-spot volcanism. This, in turn, suggests that Venus--
similar to Io-- is molten at a shallow depth. One of the great
enigmas of the "runaway greenhouse effect" is the problem of
explaining the source of Venus' high surface temperature. Based
on this analysis it now seems highly probable that the high
surface temperature has little if anything to do with a
greenhouse effect. Velikovsky's conclusion that Venus' surface
heat is derived from its molten core appears to be correct.
_The Age of Venus' Surface
_In Worlds in Collision Velikovsky suggested that Venus' age was
to be measured in thousands of years rather than billions. In a
recent article in Science a leading astronomer offered the
following observation regarding the age of Venus' surface: The
planetary geologists who are studying the radar images streaming
back from Magellan find that they have an enigma on their hands.
When they read the geologic clock that tells them how old the
Venusian surface is they find a planet on the brink of
adolescence. But when they look at the surface itself, they see
a newborn babe...(emphasis added) Magellan scientists have been
struck by the newly minted appearances of the craters
formed...Only one of the 75 craters identified on the 5% of the
planet mapped shows any of the typical signs of aging, such as
filling in with lava of volcanic eruptions or being torn by the
faulting of tectonic disruption. But by geologists usual measure
these fresh-looking craters had plenty of time to fall prey to
the ravages of geologic change. (36) Based on the assumption
that Venus is an ancient body the scientists estimate the
surface of Venus to be on the order of 100 million to 1 billion
years old. In short, even though they are confronted with a
surface that is pristine scientists nevertheless interpret the
evidence according to the theory that Venus is 4.5 billion years
old. Thus Billy Glass tells us that in analyzing Venus' history
planetary scientists accept, "the geologic history of
Venus...based primarily on what we have learned about the other
planets and is necessarily highly speculative. We assume that
Venus was formed 4.5 x 10 9 y ago." (4.5 billion years ago) (37)
_The Missing Venusian Regolith
_Geophysicists, in order to explain the physical nature of the
Venusian surface, offer the supposition that between 100 million
and a billion years ago the entire planet turned itself inside
out. If one were to accept this assumption it would require that
over that period of time between the covering of the surface
with lava flows and the present, erosional forces would break
down the surface rock into detritus to form a regolith. The
problem for the space scientists is that there is no evidence of
a regolith covering the Venusian surface. Moreover, in view of
the nature of the highly acidic nature of the atmosphere it is
obvious that there has been significant erosion of the surface.
According to Bruce Murray et al., "there can be little doubt
that chemical weathering must be very effective on Venus'
surface." (38) Venus' atmosphere is known to contain
hydrochloric and hydrofluoric acid, both of which are very
corrosive. Paolo Maffei explains further that, "the atmosphere
of Venus also contains-- although in small amounts-- hydrogen
chloride and hydrogen fluoride, which reacting with sulfuric
acid [known to exist in Venus' atmosphere could form
fluosulfuric acid, a very strong acid capable of attacking and
dissolving almost all common materials including most rocks."
(39) According to the scientists, Venus has been subjected to
this intense weathering of its surface for at least 100 million
years. Over this period of time the planet should have developed
a covering of weathered material. Nevertheless, George McGill et
al., inform us that: Radar and Venera lander observations imply
that most of the surface of Venus cannot be covered by
unconsolidated wind blown deposits; bulk densities on near
surface materials are not consistent with aeolian sediments.
Thus present-day wind-blown sediments cannot form a continuous
layer over the entire planet. (40) Thus, despite the fact that
erosional processes are clearly at work on Venus' surface, there
is no evidence of a regolith. Bruce Murray, in dealing with this
enigma wonders: Russian close-ups of Venus were surprising. I
had presumed that its surface was buried under a uniform blanket
of soil and dust. Chemical weathering should be intense in such
a hot and acid environment. Unknown processes of topographic
renewal evidently manage to outstrip degradation and burial (41)
[emphasis added. In order to explain the lack of a Venusian
regolith the scientists imagine a process that has no scientific
basis for its action to reconsolidate the detritus on Venus.
Nevertheless, let us assume that Venus' erosion rate is
extremely weak and that it is not turned back into rock at the
surface by unknown processes. What do we find? If we allow a
tiny erosion rate of one millimeter per hundred years, then in
100 thousand years we produce one meter of loose material on the
surface of Venus, which is equal to about 40 inches. However, in
100 million years we generate a kilometer of detritus, which is
over 3000 feet of this loose material. Under no known condition
can this much matter at the surface be turned to solid rock, and
this is admitted by the scientists. What we find at the surface
of Venus is the detritus of an erosion rate that is only a few
thousand years old. Only by ignoring this clear evidence can the
astronomers support the view that Venus' surface reflects events
tracing to processes occurring between 100 million and one
billion years ago. Although Magellan has cast doubt upon most of
the scientific establishment's predictions regarding the nature
of Venus' surface, a belief in a 4.5 billion year old age of the
planet Venus is still enshrined as dogma. In accordance with
this theory, it is believed by the space scientists that the
degradation of craters on Venus' surface must have occurred over
hundreds of millions of years. As the situation on Io proves,
however, degradation does not require long time periods. Io's
craters decay over extraordinarily short time periods measured
in weeks or months. On Venus this period might take years. Based
on the indications (cited above) that both Venus and Io are
molten at shallow depth and are highly volcanic, Venus' craters
would by no stretch of the imagination require millions of years
to degrade. How then do scientists explain the fact that Venus'
craters look so pristine? Here Kerr observes: Magellan
scientists strove to explain the paradox of young looking
craters on a relatively old surface. They raised the possibility
that several hundred million years ago, a planet-wide outpouring
wiped the slate clean, drowning any existing craters in a flood
of lava. Then the flood would have had to turn off fairly
abruptly so the craters formed by subsequent impacts would
remain pristine. But such a global episode of volcanism
generates another mystery. How could Venusian volcanic activity
ebb so abruptly? (42) No doubt there will be other, equally
imaginative, scenarios advanced in order to explain away this
dilemma of so few craters showing signs of decay. To return to
Kerr: But surface remodeling is going on after all, Magellan
scientists told a large crowd at the AGU [American Geological
Union meeting. More recent images show the ravages of time, but
in a fashion that leaves few aged craters."(emphasis added) This
is not so much an explanation of the findings as a directive
that the evidence is to be interpreted as such. This is not the
only problem, however. Again we cite Kerr: The expanded view
reveals four nearly continent-sized areas, ranging from a few
million to 5 million square kilometers, that have no impact
craters at all. According to Magellan team member Roger Phillips
of Southern Methodist University in Dallas, the absence of
impact craters-- despite a steady rain of asteroids and comets
onto the Venusian surface-- means that in the recent geologic
past the craters were wiped out either by lava flooding across
these areas or by tectonic faulting, stretching and compression.
The volcanic activity required to resurface the crater-free
regions would be impressive by any standards, Phillips says. For
example, it took at least a million cubic kilometers of lava
over a few million years to produce the 66-million-year-old
Deccan Traps of India. But the lava-covered areas already
uncovered on a small part of Venus by Magellan must have all
formed within the past few tens of millions of years to have
escaped being marked by impact craters. (43) So Magellan
scientists are still left with an enigma. What is clearly
implied by the radar and photographic evidence is that immense
outpourings of lava have occurred over huge areas of Venus'
surface, covering over everything including craters. The
scientists still cannot explain why there are so few craters
that are degraded or flooded or why Venus suddenly poured out
its lava in oceanic amounts. But all of this is clearly what one
would expect to find from the theory that Velikovsky advanced in
Worlds in Collision whereby Venus was only recently subjected to
tremendous stresses and participated in numerous clashes with
other planets.
_Iron
_As a newborn planet, Venus would not have fully differentiated
so it remains possible that all its iron has yet to sink to its
core. Accordingly, it was reported in Astronomy that: Maxwell
Montes...poses a big problem in interpretation. Parts have
electrical properties that indicate the surface contains
"flakes" of some unknown mineral, most likely iron sulfides,
iron oxides, or magnetite. Iron sulfides (" fool's gold") fit
the observations best, but studies have shown that they would be
quickly destroyed by the corrosive Venusian atmosphere. Iron
oxides (such as hematite) and magnetite are also possible, but
the presence of either is not easy to account for. (44) If
indeed iron is to be found upon the surface of Venus it would
support the claim that it is a youthful planet in the early
stages of cooling. (45) A planet that had differentiated its
iron into its central core would not be expected to pour iron
onto the surface with volcanic materials. The reason that the
iron compounds have not completely corroded in Venus' corrosive
atmosphere, most probably, is that these outpourings of iron are
extremely recent surface coverings measured in perhaps a few
years. Iron on Venus' surface is clear evidence that supports
Velikovsky.
_Argon
_The superabundance of 36 Argon, and the tiny amount of 40 Ar,
are glaring puzzles for the conventional view of Venus' history
but perfectly consistent with Velikovsky's view that Venus is a
youthful planet. As Glass explains, the 40 Argon builds up over
time by the breakdown of 40 Potassium: The ratio of the mass of
radiogenic 40 Ar to the mass of Venus is smaller by amount of a
factor of 15 than the value for the Earth. Since 40 Ar within a
planet increases with time due to radio active decay of 40 K,
the amount of 40 Ar should be higher if the primary outgassing
took place late in the planet's history. (46) If Venus did not
outgas much 40 Ar over time why did it outgas so much 36 Argon?
If Venus lost nearly all its 40 Ar why did it retain 36 Argon?
If, on the other hand, the great outflowings of lava released
great amounts of 36 Argon why didn't these outpourings also
release large amounts of 40 Ar?
_Oxygen
_Ultraviolet radiation photodissociates CO 2, SO 2 and H 2 O;
over millions of years oxygen should have become plentiful in
Venus' atmosphere, but it remains a minute constituent. Venus'
water vapor cannot have escaped in less than 20 billion years.
Where then is Venus' water? To argue Venus had no water but
retains other volatiles is a basic contradiction. Moreover,
Venus' middle atmosphere should have been converted to CO 2 and
O 2 over a few thousand years, yet this is not the case. To
argue that the Sun's magnetic flow implants and removes gases is
based on assumptions that have never been proven and does not
address all the problems of the other gases which exist and are
unrelated to the solar wind. A similar problem surrounds the
prevalence of hydrofluoric and hydrochloric acids. Both of these
acids are neutralized by new surface rock; oxygen, on the other
hand, will unite with new surface rock. If nearly all of Venus'
oxygen was removed by uniting with new outflows of molten rock
why didn't these great outflowings neutralize all the
hydrochloric and hydrofluoric acid? The lack of abundant oxygen
on Venus and the existence of hydrochloric and hydrofluoric acid
are only congruent with one theory-- that of Immanuel
Velikovsky.
_The Greenhouse Effect
_For years the scientific community has maintained that the
great heat of Venus is derived from an atmospheric greenhouse
effect. Gary Hunt and Patrick Moore outline the ingredients
necessary to generate a large and powerful greenhouse on Venus:
CO 2 is responsible for about 55% of the trapped heat. A further
25% is due to the presence of water vapor, while SO 2 which
constitutes only 0.02% [2/100 of a per cent of the atmosphere,
traps 5% of remaining infrared radiation. The remaining 15% of
the greenhouse is due to the clouds and hazes which surround the
planet. (47) While carbon dioxide is certainly present on Venus,
it can account for only 55% of the greenhouse effect. As Barrie
Jones explains, other factors are also necessary to make the
greenhouse work: Efficient trapping [of heat cannot be produced
by CO 2 alone, in spite of the enormous mass of CO 2 in the
atmosphere. This is because CO 2 is fairly transparent over
certain wavelength ranges to planetary wavelengths. Radiation
could escape through these "windows" in sufficient quantities to
greatly reduce the greenhouse effect below that which exists. It
is by blocking of these windows by SO 2, by H 2 O and by the
clouds that greatly increases the greenhouse effect. (48) In
short, it is crucial to the runaway greenhouse effect that there
be sufficient water, sulfur dioxide, and haze to maintain the
heat holding capacity of the planet. Respecting water,
especially in the lower atmosphere, the scientists have been
looking for this vapor for a very long time. As late as
September 1991, water vapor has not been found in anything like
that amount needed to support the contention that the greenhouse
is a foregone conclusion. According to R. Cowan: A research team
has focused on the greenhouse puzzle...The absence of water
vapor above Venus' cloud banks mystifies scientists because
models of the planet's strong greenhouse effect suggest that
[water vapor plays a key role in maintaining the warming.
Researchers have now looked for water below the cloud bank and
down to the surface-- and their search has come up dry. Evidence
of a dry Venus may force researchers to consider whether other
chemicals could create and sustain the planet's greenhouse
effect, says David Crisp of the Jet Propulsion Laboratory, who
coauthored the new report. (49) Now when a vapor responsible for
25% of the efficiency of the greenhouse-effect has been sought
in vain for some 20 years it implies that a major problem exists
with the model in question. Furthermore, in our earlier
discussion of the SO 2 and haze in the Venusian atmosphere we
have shown that measurements indicate that these materials are
transient products and do not sustain themselves for long
periods of time. With this additional undermining of the
greenhouse effect the process becomes more and more difficult to
imagine. One of the major theoretical supports of the greenhouse
model is the belief that Venus is in thermal balance. Over and
over we are told that measurements of the cloud tops for
infrared emissions show conclusively that the amount of sunlight
incident on the planet is equal to the infrared radiation
emitted by Venus. However, this must also be supported by in
situ measurements throughout the atmosphere: Radiative balance
occurs [on a planet at every level when the amount of
downward-directed solar radiation that is absorbed is equal to
the amount of infrared radiation that is emitted upward. When
local temperatures satisfy this balance the atmospheric
temperature is maintained. (emphasis added) (50) Not only must
there be thermal balance at one level of the atmosphere, this
thermal balance must exist at all levels throughout the
atmosphere to confirm thermal balance. That this is not the case
upon Venus has been known for some time. As long ago as 1980
Richard Kerr reported in Science that: When [4 Pioneer Venus
probes looked at the temperature, each one found more energy
being radiated up from the lower atmosphere than enters it as
sunlight. To further complicate the situation, the size of the
apparent upward flow of energy varies from place to place by a
factor of 2 which was a disturbing discovery. (51) Kerr adds a
telling and fundamental observation in this regard: "The much
ballyhooed greenhouse effect of Venus can account for only part
of the heating." (52) [emphasis added This simply means that the
measured evidence from in situ probes precludes the possibility
that Venus is in thermal balance. Since this evidence was
confirmed by four probes it is highly unlikely that each probe
could have been in error. What is most significant is the
variation from place to place, the amount of heat rising varying
at some places by a factor of 2. Thus, if in one region of
Venus' atmosphere the temperature was x degrees, in another area
it was 2x degrees. This means that there was at least twice the
amount of heat coming up at 2x than could have been supplied by
the greenhouse effect. It is most unlikely that in one region of
Venus' atmosphere the greenhouse effect is twice as strong as in
the other regions.
_Conclusion
_A fair reading of history will show that conventional
astronomers have a very poor record when it comes to predicting
the surface conditions of Venus. Such is not the case with
regards to the thesis outlined by Immanuel Velikovsky in 1950.
As this essay has sought to show, the evidence from Venus is
fully consistent with the thesis of its anomalous origin and
tumultuous recent history as set forth in Worlds in Collision.
Indeed, it is this author's sincere hope that the day will come
when members of the scientific community will find the courage
and integrity to call for a full and proper investigation of
Velikovsky's hypothesis.
*** References
#Post#: 240--------------------------------------------------
Re: Mathis on Velikovsky +
By: Admin Date: December 24, 2018, 11:44 pm
---------------------------------------------------------
Evidence for the Extreme Youth of Venus [SIS C&C Review]
From: SIS Chronology& Catastrophism Review (1994) "Proceedings
of the 1993 Cambridge Conference"
_Evidence for the Extreme Youth of Venus, Wal Thornhill
_"The purpose of the Universe is the perpetual astonishment of
mankind."- Arthur C. Clarke "Person who say it cannot be done
should not interrupt person doing it."- spurious Chinese proverb
_Introduction
_The planet Venus is the brightest object in the sky- after the
Sun and the Moon. Astronomers repeatedly refer to it as Earth's
'twin' [1. They should not- for twins are always born close
together in time and there is no evidence to support their
assumption that the two planets are of the same age. I will show
instead that Venus has the hallmarks of a recent genesis. What
do I mean by 'recent'? By recent I mean too recent to be
measured in millions, let alone billions of years: more likely
the event occurred within human memory and its age can be
measured in thousands of years. What is meant by 'genesis'? At
least it means the final chapters of the interaction between an
errant, cometary Venus and other planets of the Solar System and
its final settlement into a highly regular, planetary orbit
about the Sun. At most it hints at the parturition of one of the
gas giant planets to form the new planet Venus. The implications
of such a late and spectacular event in the Solar System are
profound. It will be difficult to contemplate by those who have
built the current cosmogonic consensus. That consensus is built
upon ad hoc additions to centuries-old ideas. It relies on
gravity as the aggregating force acting over millions of years
upon widely dispersed material to form the Solar System.
Clearly, in the current steady state of the Solar System,
gravitational theory seems to predict planet orbits accurately.
Not only does the clockwork certainty make life easier for the
mathematicians but it also makes the world seem safe. However,
reality has a way of being much more complex than mathematical
models: there is evidence, in particular from the behaviour of
comets, that non-gravitational forces are also at work in the
Solar System. Establishing a very recent and drastic change in
the Solar System would cause reverberations in every field of
study. As a recent example, scientists have pointed to the
hellish surface conditions on Venus and have warned that the
Earth could suffer the same fate as a result of rapacious human
activity. Such an argument assumes that the genesis of Venus was
similar to that of Earth but that the two evolved very
differently. A quite different interpretation would result from
the youthful Venus theory: that the Earth's biosphere seems to
have a remarkable capacity to recover from catastrophe attendant
upon a recent rearrangement of the inner Solar System. In turn,
this would indicate that the biosphere, even now, may not be in
a steady state, which has been suggested on theoretical grounds
[2. Venus, Earth's twin? If Venus is a newcomer to its present
orbit in the inner Solar System, it is necessary to dismiss the
oft-quoted idea of it being a twin of Earth. This idea arose
from their relative proximity in the inner Solar System and
almost equal size and mass. Couple these facts with the nebular
theory of planet formation (from a disk of gas and dust
encircling the proto-sun) and we have Earth being formed at
nearly the same time and from almost the same materials as
Venus. The mean distances of the two planets from the centre of
the Sun differ by about 25%, which would lead to an expected
initial difference in composition of the same order. Then why
does Venus have almost no water and Earth an abundance? Why does
Venus have a much higher content of primordial inert gases? The
astronomer V. A. Firsoff wrote: "I once described Earth and
Venus as 'non-identical twins'. It used to be thought that their
differences were more apparent than real. But in the words of
Sherlock Holmes, 'Eliminate the impossible and what is left,
however improbable, is the truth'. And it would be hard to find
a more improbable planet than Venus." [3 Predictably, planetary
geologists take the 'Earth's twin' approach and are thereby
forced to make the faintly absurd pronouncement: 'The overall
impression is that Venus is a dynamic world that has been shaped
by processes fundamentally similar to those that have taken
place on the Earth, but often with dramatically different
results' [4. This can only be true if one accepts qualifiers
like 'somehow' and 'mysteriously' as scientific descriptions of
processes on Venus. More likely it indicates that our ideas of
the relationship between geological cause and effect on the
Earth may be wrong. Dr S. R. Taylor, a planetologist of the
Australian National University Research School of Earth
Sciences, summed up a lecture titled 'Venus:- a twin planet?' [5
by stating: "You are not looking at a twin planet to the Earth
at all; there are very many substantial differences....the
differences are so great it makes you wonder whether you could
ever produce a twin of the Earth in some other solar system when
you can't do it in your own." Venus, the improbable planet So,
what is now known about Venus? The following sections give a
brief summary of the space age findings and the accepted
interpretations:-
_1. Magnetosphere
_A planet's magnetosphere is the region in space surrounding the
planet where its magnetic field dominates. Under the influence
of the solar wind it is compressed on the sunward side of the
planet and stretches away behind the planet like a comet's tail.
The dynamo theory of planetary magnetic fields supposes that
they are generated by an internal dynamo created by fluid
motions in a metallic outer core. The early Mariner spacecraft
provided a surprise when they found an extensive 'cometary'
magnetotail stretching behind Venus [6 along the Sun-Venus line.
It is longer than that found for any other planet. The 'scale
length' of the tail is about 700, compared to Earth's less than
300. [The scale length is the {} of Earth, the tail wake
stretches for 3000 Earth radii (R E) and the magnetosphere
varies between 10 and 15 R E. Atmospheric ions are stripped away
from Venus in its tail. Venus appears to have no intrinsic
magnetic field. This finding was unexpected because the dynamo
theory would predict a small field for Venus, given its slow
rotation and molten core. (The dynamo theory also fails to
explain why slowly rotating Mercury has a magnetic field. That
planet is not believed to have a molten core). The magnetic flux
of the solar wind appears to interact directly with the
ionosphere of Venus. This was not anticipated either, and is
unlike all other planets in the solar family. Spikes in the
Pioneer Venus orbiter magnetometer readings were interpreted as
twisted magnetic field lines wrapped around each other like
ropes. Alternatively, the magnetic field spikes may be induced
in the ionosphere by electric current flows in the solar wind.
Another major surprise is the presence of an ionosphere on the
night side of Venus. Ionospheres are thought to be created by
dissociation of atoms in the upper atmosphere by the action of
solar ultraviolet (UV) radiation. It was thought that the long
Venusian night would be long enough for recombination to take
place and for the ionosphere there to disappear.
_2. Rotation
_Venus has a retrograde axial rotation period of 243 days. It is
assumed, because it so different to the Earth's rotation rate,
that it must have been similar at some time in the past and then
drastically modified as a result of a of a very large collision.
There is no generally accepted theory to explain planetary
rotation or axial tilt. Strangely, Venus always presents the
same hemisphere to the Earth at times of inferior conjunction.
_3. Isotopic anomalies
_Three isotopes of argon are considered important in
investigations of planetary atmospheres. 40 Ar is produced by
the decay of radioactive potassium( 40 K) in the planet's rocks
and is outgassed into the atmosphere over time. Venus has only
of the amount of 40 Ar found in the Earth's atmosphere. The
other isotopes, 36 Ar and 38 Ar are thought to be primordial
gases, present when the planet formed. 36 Ar appears in
proportions up to 100 times that found on Earth or Mars. Since
it cannot be created after a planet's formation, if Venus was
formed in the way the Earth and Mars were it should have an
equal or lower concentration. There is also about 45 times more
neon and 3 times more krypton in the atmosphere of Venus. Its
atmosphere shows a deuterium to hydrogen ratio of about 100
times that of the Earth which, it is argued, might be consistent
with the loss of oceans of water and the preferential outgassing
of the lighter hydrogen. But such a mechanism does not easily
remove the last vestiges of water to leave such a dry
atmosphere. The isotopic abundances do not follow the expected
pattern for planet formation from a nebula. For example, Venus,
being nearer the Sun than Earth and Mars, should have lost more
36 Ar to the early, strong solar wind than those planets.
_4. Atmosphere
_None of the the characteristics of the Venusian atmosphere were
predicted by prevailing cosmogonic theories. Venus has a
planet-wide cloud cover and massive atmosphere which is
remarkably uniform in temperature and pressure at all latitudes
and in both day and night hemispheres. With a gravity 90% of the
Earth's and being closer to the Sun, Venus would be expected to
have retained less volatiles and hence have a thinner (not
thicker) atmosphere than the Earth. The Venusian atmospheric
composition is shown below. Atmosphere Earth Venus 77% nitrogen
21% oxygen 1% water vapour 97% carbon dioxide 2% nitrogen 1%
oxygen Ammonia (0.1 percent) was detected by the Soviet probe,
Venus 8, at the height of the clouds. Hydrocarbons of many sorts
showed up in the initial evaluation of the mass spectrometer on
board the Pioneer atmospheric probes but were discounted as
lingering instrumental residues [7. Clouds occupy several
discrete layers, at heights typically 46, 47-49, 50-55, and
56-62 kilometres above the surface (clouds on Earth rarely top
15km altitude), with the uppermost, yellowish, cirrus-like haze
made from droplets of concentrated sulphuric acid. Since
sulphuric acid does not account for the yellowish colour of the
clouds, this deduction is suspect. It is this uppermost layer
that is responsible for the markings visible in UV images. It
has also been found that a major constituent of large cloud
particles is chlorine. The highly reflective upper haze
effectively hides lower levels rather like a veil in bright
sunlight hides a bride's face. The clouds below are not as
opaque as earthly clouds but are more akin to photochemical
smog. Investigators had expected that only 2% of the total
incident sunlight would reach the surface and that the
atmosphere would be super-refractive. Neither is the case: it is
surprisingly bright at the surface and pictures by Veneras 9 and
10 showed the horizon 200-300m distant. Cloud movements show a 4
day rotation period of the upper atmosphere at the equator which
declines to 2 days towards the poles. This is explained by a
constant wind velocity on a reducing perimeter as the upper
atmosphere spirals up to the poles. However, with a rotation
period of the planet of 243 days retrograde and sluggish surface
winds, the upper atmospheric movement is incomprehensible. The
negligible variation in surface temperature is explained
theoretically in astronomical textbooks by slow winds in the
dense lower atmosphere of 1 to 2 metres/sec from the poles to
the equator [8. There are three reasons why this explanation is
unsound: i). Since the planet is now the same temperature
overall there is no heat engine to drive the lower atmosphere.
ii). Moving patterns detected in two specific windows for
infrared radiation through the carbon dioxide atmosphere
indicate that the lower clouds are patchy and move at velocities
up to 250kph [9. iii). Winds at the surface are slow (about
6kph) and always in the direction of rotation, not from pole to
equator. In 1972, a 'breathing' phenomenon was discovered in the
Venusian atmosphere [10. It is as if the cloud cover is acting
like the lid on a kettle of boiling water; the infrared CO> 2
lines swing through a four day cycle akin to a relaxation
oscillation which builds up slowly during each cycle and then
collapses. This indicates that the cloud deck moves up and down
through 1 km over the entire planet. Such a phenomenon requires
considerable energy input- which is difficult to account for on
a very slowly rotating planet if solar energy is the only
source. The 'breathing' has been confirmed by the Magellan
orbiter which underwent variable atmospheric braking at the
lowest point of its orbit, with a 4 day cycle. Explanations of
the Venusian atmosphere have required large numbers of
assumptions and special conditions to be imposed on the
hypothetical early solar nebula and the activity of the
proto-sun. Many anomalies remain.
_5. Heat balance
_The rocks of the Earth contain radioactive uranium, thorium and
potassium-40 which in the process of decay provide energy to
heat up the planet's interior. The potassium/uranium ratio is
about the same on Venus as on the Earth. It is therefore
assumed, on the grounds that the two planets are twins, that the
internal heat production is the same. The very high surface
temperature of Venus of 750 K or 900 F is usually explained by
the 'greenhouse effect' of CO 2, or even the 'runaway greenhouse
effect', first suggested by Fred Hoyle in 1955 and worked out in
detail in the late 1960s by Ingersoll and Pollack of Caltech.
Such explanations also rely on the assumption that both Venus
and Earth have had largely parallel development (twins again)
and that therefore something went seriously wrong with the
atmospheric evolution on Venus. Firsoff noted: "Earth's seas
are not boiling hot, despite the total greenhouse effect of
water and average sunlight stronger than at the ground level of
Venus. Nor is it at all clear how such a condition could have
become established" [11 Venus receives 1.9 times more solar
radiation than Earth but its clouds reflect about 80% of that
sunlight, so that Venus actually absorbs less solar energy than
the Earth. Solar radiation measured at the surface is 10-20W/m 2
(compare this with 340W/m 2 at the Earth's surface in the
tropics). Even with the maximum greenhouse effect, the effective
surface temperature of Venus should be low enough to freeze
water [12. What is being asked of the 'runaway greenhouse
effect' is equivalent to expecting a well-insulated oven to
reach a temperature sufficient to melt lead by having only the
pilot light switched on! The humorous but sadly apt inversion,
'I'll see it when I believe it', seems to apply to the
interpretation of results relayed to Earth from all four Pioneer
lander probes as their radiometers began to give anomalous
results as they descended through the atmosphere. "Taken at face
value, the anomalies suggest that parts of the atmosphere are
transmitting about twice the energy upwards that is available
from solar radiation at the same level." [13 Despite the obvious
interpretation that the laws of thermodynamics are not being
violated and that, simply, Venus is intrinsically hot and still
cooling, the investigators are able to blandly state in the same
paragraph: "In spite of these difficulties in interpreting some
of the observations, the greenhouse effect, coupled with global
dynamics, is now well established as the basic explanation of
the high surface temperature." On the night side of Venus where
sunlight reflected from the uppermost haze cannot dazzle the
observer, it is possible to see surprisingly deeply into the
planet's atmosphere. The only illumination is the infrared
radiation from the planet's hot surface which is almost
sufficiently intense to be seen as a very dull red glow. Cloud
patterns picked out in infrared are intense enough to be seen
during inferior conjunction (in broad daylight) from Earth using
a suitably equipped 20cm telescope. The emissivity of the
surface at the Magellan radar wavelength, which corresponds to
surface electrical properties and surface temperature,
correlates strongly with altitude. There are some exceptions to
this pattern. High altitude temperatures are often much lower
than would be expected on the basis of the adiabatic lapse rate
of minus 9 K/km. The conventional view is that the higher
emissivity is largely due to the surface chemical composition
being different in the highlands. The greenhouse effect would
have the surface temperature conforming to the lapse rate.
Figure 1. A typical Venusian sinuous rille. The scale bar= 10km.
They tend to grow narrow and shallow towards their termini. They
are widely distributed in the equatorial regions.
_6. Lightning
_"The most striking [the pun seems unintended observations made
by the Galileo spacecraft during its flyby of Venus was evidence
of lightning." [14 The surprise is curious. Earlier reports of
lightning were discounted, it seems, because they did not fit
the pattern of earthly lightning. The Venera spacecraft found
'continuous lightning activity from 32km down to about 2km
altitude, with discharges as frequent as an amazing 25 per
second' [15. The highest recorded rate on Earth is 1.4/sec
during a severe blizzard [16. The Pioneer lander recorded 1000
radio impulses. Thirty-two minutes after landing, Venera 11
detected a very loud (82 decibel) noise which was believed to be
thunder. Garry Hunt suggested at the time that:'... the
Venusians may well be glowing from the nearly continuous
discharges of those frequent lightning strokes' [17. A
'mysterious glow' was detected coming from the surface at a
height of 16km by 2 Pioneer probes as they descended on the
night hemisphere. The glow increased on descent and may have
been caused by a form of St. Elmo's fire and/or chemical
reactions in the atmosphere, close to the surface. Lightning is
poorly understood. The mechanism of charging of storm clouds
remains a mystery. Because lightning is conventionally
associated with violent vertical cloud movement on Earth, it was
a surprise when investigators found strong evidence of lightning
in the quiescent atmosphere of Venus. 'On Venus the clouds tend
to resemble fogbanks,.... You don't see much lightning in fog.'
[18
_7. Volcanism
_Venus seems to have about 4 times more sulphuric acid in its
atmosphere than Earth. It also has minute concentrations of
hydrochloric and hydrofluoric acids. These findings suggest
lively, recent volcanic activity on the planet. There are
between 100,000 and 200,000 small basaltic domes (averaging a
few hundred metres high and 2km across), rather like underwater
sea mounts. Some appear to have explosively erupted, judging by
radar-bright deposits or 'plumes' of material broadening away
from them. Venus apparently has very fluid lavas. Venusian
sinuous rilles have been identified (Figure 1) in large numbers.
These rilles are thought to be due to erosional processes
involving very hot, fluid lavas. Smooth basaltic plains and lava
flows, relatively unmarked by craters, make up 80% of the
planet's surface- indicating its extreme youthfulness. There are
430 volcanoes of 19km or more diameter and tens of thousands of
small ones. There is an enigma in that there are relatively few
craters which have been encroached upon by lava. This would
suggest that the craters, most of which look very new, are of
more recent origin than the global lava flows. There is no
satisfactory explanation for a resurfacing event which involved
the entire planet. The word 'resurfacing' itself assumes there
once existed an older cratered terrain- but, again, there is no
evidence for that. There are many curious features on Venus
which are attributed to upwelling lava. For example, there are
large circular domes (750 metres high and averaging 25km
diameter), often arranged in a chain, with craters and a complex
pattern of 'fractures' on top. See Figure 2. These objects are
interpreted as a thick lava flow which welled up through
openings on level ground, although it is difficult to understand
why they should all be so near perfect circles. Such circularity
requires too many special conditions to be plausible. The lava
orifice would need to be circular, the surface dead level with
no obstructions, and the lava viscosity and cooling rate within
very narrow limits. Compare the domes with the lobate structure
of a true lava flow in Figure 3. The dome fractures are thought
to be caused by the cracking of solidified surface lava by
further outflows. It is strange that the fractures seem to be of
relatively uniform width on widely separated domes. Also some
'fractures' in the surrounding plain appear to climb the wall of
a dome and continue across the top (see Figure 2). Small craters
appear on top of the domes, generally in the centre and even
smaller craters seem to populate the fractures. The surrounding
plain is unmarked by craters, with the notable exception being
along the floors of fractures. Figure 2. Seven circular 'domes'
averaging 25km in diameter with maximum heights of 750m in Alpha
Regio. North is at the top. The linear features are termed
'fractures'. Note the small craters populating the floors of
some of them. The long channel in the southeast has a secondary
channel along its floor. Figure 3. Multiple eruptions appear in
this volcanic structure, located on the plains between Artemis
Chasma and Imdr Regio. The central dome structure is 100km wide
and about 450m thick on average. Note the usual uneven, lobate
form.
_8. Cratering
_Craters are randomly distributed on Venus with some areas of
higher or lower density. Surprisingly, most are in pristine
condition. As expected, most craters are described in the Jet
Propulsion Laboratory's images as 'meteorite impact craters' and
their features as 'typical..., including rough (bright) material
around the rim, terraced inner walls, and central peaks.' [19
The central peaks are termed 'rebound' peaks. The largest
craters may show concentric rings. Venus has a relatively low
crater count which is attributed to both a global volcanic
resurfacing event and the planet's thick atmosphere acting as a
shield against small meteors. However, small craters do exist
and are found populating the floors of the numerous linear
'fractures', which argues against their formation by impact. The
insistence on describing craters as impact-generated is more due
to the fact that it is geologists making such pronouncements and
that they have difficulty matching the craters with volcanoes
observed on Earth. Significantly, astronomers tend to ascribe
the craters to volcanic activity, which indicates that neither
group feel comfortable with an explanation based on processes
with which they are familiar. Two characteristics of so-called
impact craters which beg explanation are their near-perfect
circularity and the melted floors of large, recent craters,
clear of impact debris. Despite this, counting craters is the
main technique for determining the age of a planet's surface. It
also relies on assumptions about the past population of
orbit-crossing comets and meteors in the inner Solar System.
"The planetary geologists who are studying the radar images
streaming back from Magellan find they have an enigma on their
hands. When they read the geologic clock that tells them how old
the Venusian surface is they find a planet on the brink of
adolescence. But when they look at the surface itself, they see
a newborn babe... Magellan scientists have been struck by the
newly minted appearances of the craters formed...." [20 Crater
counting and the random distribution puts the entire surface age
at 500 million years. It is therefore generally concluded that
any old surface was wiped clean by a cataclysmic event at that
time and remained volcanically quiet since then. The high degree
of circularity of most craters suggests that whatever created
them acted largely perpendicular to the surface, which is highly
unlikely for impacts. Such crater circularity is also a feature
on our Moon, the moons of Mars (Figure 4), oddly shaped
asteroids, and the nucleus of comet Halley where the cratering
process may have been observed in action (Figure 5). Figure 4.
View of the 17km long asteroid 951 Gaspra (top), taken by the
Galileo spacecraft. The smallest details are 55 metres across.
Deimos (left) and Phobos (right), the moons of Mars, are shown
for comparison. Note the craterlets on the rim of the large
crater on Phobos. Figure 5. An artist's enhancement of the
images of the nucleus of comet Halley taken by the Giotto
spacecraft. Notice the bright circular spots and jets. Figure 6.
Three large craters with diameters from 37 to 50km are seen in
this image from the Lavinia region. Note the truncated ejecta
fields around the craters. Asymmetric ejecta patterns have been
cited as evidence for impact at an angle to the vertical. Some
craters (Figure 6) have a flower-like ejecta blanket which did
not travel very far, presumably due to the high atmospheric
density. Mars shows similar features which were attributed to
the action of water. Since Venus has no water that theory cannot
be relevant. There are a number of asymmetric craters which do
hint at impact. They show possible effects of the thick
atmosphere on the way that meteors reach the surface or the
manner in which the ejecta blankets are distributed. Many
craters seem to be flooded from below with lava which is
presumed to exist in hot layers just beneath the thin crust of
Venus.
_9. Plate tectonics
_The surface of Venus has been described as 'spotty'. There are
no apparent equivalents of our continental plates. There is only
flimsy evidence for some form of plate subduction around the
rims of pimple-like elevations called coronae but the origin of
the coronae is a mystery. They have been described as magma
extrusion features. There is no evidence of a mid-ocean type
ridge on Venus to generate new crust. The situation was summed
up recently in New Scientist: "The high-resolution radar images
Magellan has produced show no evidence of the long chains of
volcanoes, and no mid-ocean ridges or other features that would
indicate a global system of plates." [21 Venus has rocks similar
to those on Earth and possibly more internal heat which would be
expected to lead to more dynamic tectonic activity. One
suggestion is that the surface of Venus is too hot to sustain
rigid plates and that the surface puckers and wrinkles in
response to interior forces. Another flimsy idea is that the
lack of water on Venus means that it lacks the essential
lubricant for sliding crustal plates [22. The many differences
between the crusts of Earth and Venus suggest an unusual event
to have caused the observed continental rifting on Earth. The
assumed driving mechanism for continental drift is mantle
convection due to internal radiogenic heat. But it is a very
unsatisfactory explanation given the rigidity of the crust and
modest heat input which would lead to a low velocity of
convection [23. There is no good evidence that anything other
than settling movements between plates are now taking place on
Earth, long after some past catastrophic rifting 'event(s)'.
Rifting is most easily explained by external torques on the
Earth. Surface features on Venus, interpreted as fractures,
suggest crustal expansion with few signs of compression. The
size and spacing of wrinkles is believed to give an indication
of the crustal thickness. Venus has 'smaller, more closely
spaced features than any previously seen' [24, which argues for
a thin crust. But there is another possibility- that the
so-called fracture lines are not fractures at all but channels,
gouged out of the surface by a mechanism to be described later.
Gravity mapping is to be undertaken by Magellan after its orbit
is lowered by atmospheric braking, and then circularised. Such
mapping should provide more clues to the structure of Venus.
Already it is believed that the prominent Maxwell Montes region
should subside under self gravity in a relatively short time.
_10. Channels and valleys
_Venus appears to be laced with fractures, ranging from
elaborate networks of fine cracks that extend over large areas
of the planet to extensive canyons thousands of miles long. Up
to 200 channels of various types (some clusters being counted as
a unit) have been counted. They are concentrated in the
equatorial regions and particularly the highlands, rift and
fracture zones associated with large shield volcanoes, and the
uniquely Venusian coronae. Twelve valleys have been counted.
They have been classified as either labyrinthic, rectangular,
and irregular or pitted. Some valleys graduate into channels.
Simple, non-branching channels have been classified as sinuous
rilles, channels with flow margins, and canali [25. Figure 7a.
The meandering channel known as the river Styx. It is 6,800km
long but practically constant in width at about 2km. The scale
bar= 50km. Figure 7b. Detail of river Styx. Note the indications
of a smaller channel in the bed of the 'river'.Sinuous rilles
generally originate in depressions up to a few hundred meters
deep. The channel is cut into the terrain and grows narrower and
shallower distally, with no outflow deposit. They are the most
numerous channel type and seem to be concentrated near coronae
and arachnoid features. They are thought to be due, in some
degree, to "a process of lava drainage channel deepening and
widening through thermal-mechanical erosion by high temperature,
low viscosity lava during a sustained eruption at high effusion
rates" [26. There are severe problems with this proposal. For
example, outwash deposits are generally lacking and the channel
narrows rather than widens at the lower end. The channels are
often preferentially cratered compared with the surrounding
terrain. They are probably too deeply cut into the surface
(several hundred metres) to be explained by lava drainage. The
dimensions of the Venusian sinuous rilles are far greater than
any lava channels seen on Earth. Channels with flow margins
occur on volcanic flow deposits. They are shallow and do not cut
into the terrain like sinuous rilles. They are consistent with a
lava flow origin. Canali are the next most common channel type.
They are extraordinarily long, have remarkably constant width
and depth and a lack of complex branching. Canali are found on
the smooth plains and trend in random directions. The longest
canali are confined to specific plains. There is generally no
way of distinguishing which end of the channel is the source and
there is no evidence of ponding. Narrow levees can be discerned
on some of the radar images. Suggestions for their origin
struggle with enormous flows of long duration of exotic, highly
fluid lavas on a scale not seen on any other body in the Solar
System. Since there is no evidence of any outflow of the canali
it is suggested that successive outflows of lava or weathering
has obliterated the sources and sinks of the canali! One of the
most bizarre canali is the remarkably long and narrow Hildr
Fossa, which Magellan scientists have nicknamed the River Styx
(Figure 7). The feature has no analogue on Earth. With a
constant width of less than 2km, Hildr is 6,800km long! Slightly
longer than the Nile, it is the longest channel known in the
Solar System. What is even more weird for a channel which is
assumed to have been formed by the flow of some unspecified
extremely hot, thin liquid is that it runs up hill and down dale
by as much as a kilometre in a roller-coaster fashion. It has
been suggested that the terrain must have undergone uplift since
the channel was formed. But practically all of the many 'rifts'
and channels on Venus exhibit the same disregard for gravity
without signs of channel disturbance which would be expected
from extensive ground movement. In the searing heat and
crushing pressure at the planet's surface, it is impossible to
imagine any substance that could remain liquid long enough to
carve out such a lengthy, uniform channel, to somehow disappear
along the way and defy gravity in the process! Unremarked by
investigators is a secondary, even more sinuous, channel
meandering along the floor of Hildr (and most other channels and
fractures where image resolution allows) with what appears to be
small craterlets dotted along its length. This looks like a
more extensive form of the sinuous rilles. The bright radar echo
from both sides of these channels and the shadow behind the top
of the radar illuminated bank suggests that the banks are
narrow, raised levees [27. The channels and valleys on Venus are
assumed to be erosional features caused by a flowing liquid. The
only liquid expected at the surface temperature of Venus is
lava. Few of the features observed can be explained by lava
flows.
_11. Surface age
_It is to be expected that the surface has not suffered from
much erosion. With a year-round temperature at the surface of
470 degrees C, surface water, if there ever was any, has long
ago boiled away leaving a totally dry and arid landscape. Winds
in the lower atmosphere are also very sluggish due to the even
temperature and high atmospheric density near the surface. So
impact craters and scars from geologic events should remain
visible for millions or billions of years. Using accepted
assumptions about impact cratering rates in the inner Solar
System, it is assumed that the surface age can be determined by
crater counting. Scientists were surprised to find a distinct
shortage of craters, which indicates a young planet. An early
report of the Magellan findings stated: "The Venusian surface
appears to be 100 million to 1 billion years old, quite ancient
by terrestrial standards" [28 but very young when compared with
the Moon or Mercury which also suffer little erosion. The
craters on Venus all appear to be new. There is no evidence of
an old, heavily cratered terrain. It was simply suggested that
the planet's outer layers have been 'reworked and erased
relatively recently' [29 without any cause being given. The
erasure of the planet's features must have stopped abruptly for
there to be little sign of encroachment of lava upon the
craters. Clearly, the age will be too high if cratering rates
were greater in the recent past. The detailed nature of the
surface, revealed by panoramic photographs from Venera 9 after
landing, was a surprise. There were no signs of a dust cloud on
touch-down at 24 kph and the stones were sharp-edged and recent
looking. Even if the erosion rate on Venus were a fraction of a
percent of that on Earth, a soil measured in metres would be
expected to form in 100 million years. In addition, some of the
slopes on Venus, determined by the Magellan orbiter, are
remarkably steep. There are slopes of 1 in 4, which is near the
limit of stability. Such slopes obviously cannot have existed
for long. They are remarkably young. It is assumed that
resurfacing by basaltic lavas is responsible for the apparent
youthfulness of the surface. This requires some unknown
mechanism based on unproven convection in the mantle to cause
widespread resurfacing of the planet, followed by quiescence. It
seems to be asking too much for some indeterminate internal
process to create planet-wide lavas and then shut down for
hundreds of millions of years while cratering takes place. Of
course, all of this presupposes that Venus has a history prior
to the 'global resurfacing event'. 12. No satellite Venus has no
satellite. The Earth is unique among the inner planets in having
a moon which would not appear out of place among the satellites
of the giant outer planets. It suggests a quite different
history for Earth compared to Venus. How are planets formed?
Before any discussion can take place about the age of Venus, the
method of planet formation needs to be determined. The accepted
nebular theory of the birth of the Solar System does not allow
much leeway from a figure of 4.5 billion years. If Venus was
added to the solar family of planets very recently, then a new
cosmogony must be proposed which does not require that all
planets be created at the same time. This would be a radical
departure from astronomical thinking today and would result in a
completely new perspective in cosmology as well as cosmogony.
The better we understand our own back yard, the better are the
chances that we will eventually unravel the mystery of our
origins, and the solution will come sooner if our minds are
prepared to accept the truth when it is found, however fantastic
it may be. It we are guided by our reason and our scientific
method, if we let the Universe describe its wonder to us, rather
than telling it how it ought to be, then we will soon come to
the answers we seek, perhaps even within our own lifetimes.' [34
_References
#Post#: 332--------------------------------------------------
Re: Mathis on Velikovsky +
By: Admin Date: August 13, 2021, 11:07 pm
---------------------------------------------------------
I discussed at
HTML https://cuttingthroughthefog.com/2018/11/09/current-events-discussion-thread/comment-page-2/#comments
and
HTML https://cuttingthroughthefog.com/2018/11/09/current-events-discussion-thread/comment-page-3/#comments
etc
*****************************************************