[meteorite-list] Venus Catastrophic Resurfacing HypothesisChallenged
From: Sterling K. Webb <sterling_k_webb_at_meteoritecentral.com>
Date: Mon, 26 Apr 2010 01:50:32 -0500 Message-ID: <2957203A17934CDE9C81198FC03298AF_at_ATARIENGINE2> Listoids and Venus Fans, The Global Catastrophe "Hypothesis" became a problem as soon as the Magellan dataset was mostly complete. The data was turned over to the "crater-counters" who are able to date a planetary surface by the statistical distribution of crater size, and date it quite precisely, too. When they announced the age of the Venusian surface as 520 million years, plus or minus a 40-50 million year error (or 480 to 560 my), they were immediately surrounded by hysterical geologists screaming that they had to be wrong. The crater counters were replaced by other crater counters who gave the same results. This is a narrow specialization -- crater counting -- there are only so many crater counters, and it's a very precise technique that has dated every solid planetary surface we can image with results that are both consistent and to every appearance accurate everywhere. A decade or so was wasted on "geological" mechanisms that could re-surface without outside interference. They were largely hooey that convinced no one, posing improbable mechanisms to accomplish world-wide simultaneous subduction. The problem is not a "hypothesis" problem; it is a "fact" problem looking for a hypothesis. If we take a step backward and look at events in the ENTIRE solar system, we see that: a) ~600 million years ago, the largest asteroid breakup in the last 4 billion years occurred (the Flora Family), b) starting at 600 million years ago, the impact rate in the solar system jumped up to high levels not seen for 3.2 billion years (dated by lunar impact spherules collected by the Apollo missions), c) between 600 million years ago and 500 million years ago, the Earth had three catastrophically nasty ice ages, including the Snowball Earth episode in which the entire planet froze to the equator, the worst ice age ever, d) 484 million years ago, the Earth suffered a prolonged period in which the rate of meteoritic infall was up to 150 times greater than it is today, http://www.psrd.hawaii.edu/Mar04/fossilMeteorites.html and e) the surface of Venus was wholly or partially melted and resurfaced with fresh rock (just like the old days, huh?). I see these events as connected, as I've been sometimes posting here for the last 6 or 7 years. Or, they could be one freakin' big coincidence... So, I read the RTT paper with great interest. They advance solid arguments for the conclusion that the RTT had to be formed in one discrete episode or interval. In a word, that it's datable. They then assert that it had to have formed very early in the planet's history because "thermal modeling indicates that ribbon fabric formation requires an extremely high thermal gradient..." That is, a high internal heat flowing up to the crust as it does at the end of planetary formation and cooling. In other words, you can't form RTT unless the crust is very hot. That is the extent of their "dating" attempt. The ancient origin would be true in the case of the absence of a viable geological "catastrophic" or global turnover model ONLY IF you exclude impacts (giant or multiple) large enough to melt the crust down to the mantle. Best way to prove your case is to ignore anything that would disprove your case, I always say. The RTT are scattered in disconnected patches over the planet. They could be a relict of ancient terrains or they could be the places where the 100-300-kilometer asteroids DIDN'T fall. The fall of planetoid sized bodies, of course, heats the crust planet wide by degrading the impact energy into thermal energy. The heat doesn't have to be internal when you melt a planet's surface. Hansen and Lopez have another paper on the RTT, characterizing them as lava "scrum ponds," also from this same year (2009): http://www.lpi.usra.edu/meetings/venus2009/pdf/2012.pdf (I think you ought to hold it down to one theory a year.) This is a strange idea since the RTT is 1-3 km. HIGHER than the low flat plains -- why didn't the lava run off? But, then, I'm no geologist and I don't really know how to make lava run uphill... How you do dat? In fairness, a few RTT parches are on the lowest level... but only a few small ones. Another view on the RTT by another member of the original Magellan team (this one from 1996): http://www.agu.org/pubs/crossref/1996/96JE01245.shtml Author of many papers on Venus; Google "Ivanov Venus." There's another theory of the RTT, the "pulsating continent" theory. Bouncy continents... That sounds like fun: http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6V61-4TRR8Y0-1&_user=10&_coverDate=11%2F30%2F2008&_rdoc=1&_fmt=high&_orig=search&_sort=d&_docanchor=&view=c&_searchStrId=1310409062&_rerunOrigin=google&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=1a74f8614c1c46478bfbfe77b807a05a There seems to be this continuing effort in explaining Venus' geology by "mechanisms without outside interference." I'm tempted to see it as the old "we're-geologists---take-your- asteroids-and-never-darken-my door-again." The dinosaurs died off from bad head colds... Didn't you know? The "Mega-Catastrophe" paper from 2 years ago (which IS an impact paper) is by Huw Davies, not Davis. Hmm... Cardiff -- home of the "red-rain-is-alien-life" theory. OK, what's the theory? Well, that Venus formed "by a near head-on collision of two large planetary embryos, as might be expected from favoured oligarchic planetary accretion." A "head-on" collision means that ONE of the two equal near-planets would have to have been moving in a retrograde orbit about the Sun. How can I explain how difficult it is to explain retrograde motion? All the planets revolve prograde. All the planets rotate prograde except Venus, Uranus, and Pluto. All the good-sized moons orbit prograde except Triton. There are some retrograde small or asteroidal moons of the giant planets. Triton we explain as a retrograde capture from the Kuiper Belt or from Pluto. All but 20 of the tens of thousands of asteroids orbit prograde. All but a handful of exoplanets orbiting other stars are prograde. Comets are a mix because they "choose" an orbit by just falling in. A retrograde giant planetesimal as close to Sun as the Venus orbit is a billion-to-one shot... at least. I'd believe the Red Rain first. And last, since this paper, ESA has released results from Venus Express that show that water is still being lost from the top of atmosphere, an astounding result if you believe Venus has lost all its water and is bone dry. Venus is still leaking water, still outgassing. You can forget the totally dry Venus proposed by this paper. You can also forget the notion that whatever happened to Venus happened billions of years ago. If it's still outgassing, the disaster was (geologically) recent, say, a half billion years ago? If you wonder what else besides asteroids that could have hit Venus, well, it could also be the fall of a retrograde moon. A prograde moon (like ours) is gradually pushed away by the momentum transfer of tidal friction, but a retrograde moon is pulled down to the Roche Limit, where it breaks up and falls to the planet below. Talk about A Really Bad Day -- the Moon is falling. Or, a large asteroid could have been captured in a close orbit; retrograde capture is much easier than prograde. Then, the following breakup and fall would melt the crust (if the moon was big enough). For more, Google "Malcuit Venus." Dr. Malcuit is a geologist at Denison U. in Ohio and has been doing computer simulations of this problem for 20 years. Venus, Problem Child of the Solar System... If the Earth had been whacked with a 300-km object a half billion years ago, the crust would have melted, the oceans would have boiled off, the carbonates on the surface would devolved in the superheated steam into CO2, forcing the temperature and pressure to rise catastrophically and finish the job. The Earth has enough carbonates on its surface to form a CO2 atmosphere of 90 bar pressure. (Interestingly, the Earth-sized Venus has 90 bar of CO2). The Earth would be 400 degrees. The Earth would have high plateau continents (like Venus), vast abysmal plains where the sea beds once were (like Venus), and rippled and folded "undersea" mountains and sea-mounts at middle elevations (like the RTT on Venus) There, but for grace of asteroid, go I. Oh, well, probably all a coincidence. Sterling K. Webb ---------------------------------------------------------------------------- ----- Original Message ----- From: "Paul H." <oxytropidoceras at cox.net> To: <meteorite-list at meteoritecentral.com> Sent: Sunday, April 25, 2010 9:06 PM Subject: [meteorite-list] Venus Catastrophic Resurfacing HypothesisChallenged > Dear Friends, > > Ribbon tessera terrain on Venus challenges catastrophic > resurfacing hypothesis. > > Venus Records a Rich Early History > ScienceDaily, March 25, 2010) > > http://www.sciencedaily.com/releases/2010/03/100326125438.htm > > the paper is: > > Hansen, V. L., and I. Lopez, 2010, Venus records > a rich early history. Geology. vol. 38, no. 4, > pp. 311-314, doi:10.1130/G30587.1 > > http://geology.gsapubs.org/content/38/4/311.abstract > > Hansen, V. L., and I. Lopez, 2009, Implications of > Venus Evolution Based on Ribbon Tessera Terrain > Relations Within Five Large Regional Areas. 40th > Lunar and Planetary Science Conference, (Lunar > and Planetary Science XL), held March 23-27, 2009 > in The Woodlands, Texas, id.2306 > > http://www.lpi.usra.edu/meetings/lpsc2009/pdf/2306.pdf > > http://adsabs.harvard.edu/abs/2009LPI....40.2306H > > A related article: > > Did A Mega-Collision Alter Venus? > ScienceDaily (Feb. 27, 2008) > > http://www.sciencedaily.com/releases/2008/02/080226160017.htm > > The paper is: > > Davis, H. J., 2009, Did a mega-collision dry Venus' > interior? Earth and Planetary Science Letters. > vol. 268, no. 3-4, pp. 376-383. > > http://dx.doi.org/10.1016/j.epsl.2008.01.031 > > Yours, > > Paul H. > ______________________________________________ > Visit the Archives at > http://www.meteoritecentral.com/mailing-list-archives.html > Meteorite-list mailing list > Meteorite-list at meteoritecentral.com > http://six.pairlist.net/mailman/listinfo/meteorite-list Received on Mon 26 Apr 2010 02:50:32 AM PDT |
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