[meteorite-list] Did A Giant Impact Create The Two Faces of Mars?
From: Ron Baalke <baalke_at_meteoritecentral.com>
Date: Fri, 16 Mar 2007 18:13:51 -0700 (PDT) Message-ID: <200703170113.l2H1DpP27737_at_zagami.jpl.nasa.gov> http://space.newscientist.com/article/dn11387-did-a-giant-impact-create-the-two-faces-of-mars.html Did a giant impact create the two faces of Mars? David Shiga New Scientist 15 March 2007 The impact of a giant asteroid could explain why Mars has two very different faces - but only if it struck the planet with a glancing blow, computer simulations suggest. A longstanding puzzle about Mars is why its northern and southern hemispheres are so different. The northern hemisphere is much flatter and lies lower than the southern hemisphere, with a difference in elevation between the two of about 5 kilometres. In the 1980s, scientists suggested a giant impact by an asteroid about 300 kilometres across in Mars's early history could have led to a permanent depression in the planet's northern hemisphere. Now, two teams of scientists have created the first computer simulations testing whether such an impact could have produced the observed differences. Shawn Hart of the University of California in Santa Cruz, US, led one of the simulation teams. His team found that such an impactor would produce huge amounts of lava - enough to cover the planet in an ocean of molten rock somewhere between 14 and 48 kilometres thick. That would have ended up erasing any record that an impact happened in the first place. "We therefore consider it unlikely that you'll create the Martian crustal dichotomy utilising a single giant impact," Hart says. But simulations carried out by the second team, led by Margarita Marinova of Caltech in Pasadena, US, suggest the giant impact hypothesis could still do the job if it struck only a glancing blow. Less lava In simulations of grazing collisions, the team found the impactor still makes a depression, but produces less heat, melting only a relatively small area around the impact site. Watch an animation <http://media.newscientist.com/data/images/ns/av/dn11387V1.gif> showing the result of a giant impact (805 kB). In this scenario, the total amount of lava produced is equivalent to a 5-kilometre-deep layer distributed over the whole planet. This would be small enough to avoid erasing the depression, the researchers say. "You can have a very large impact and not melt the whole planet and preserve some signature of this impact," Marinova told New Scientist. William McKinnon of Washington University in St Louis, Missouri, US, says a giant impact may explain the crustal dichotomy. But he cautions that it is too early to draw hard and fast conclusions from the simulations. "I think it's exciting work, but we don't have the whole picture yet," he told New Scientist. An unresolved question is exactly how the lava would arrange itself after such an impact, says Walter Keifer of the Lunar and Planetary Institute in Houston, Texas, US. "Where does the melt go and how much of the basin does it fill is a key issue," he told New Scientist. The results were presented on Wednesday at the Lunar and Planetary Science Conference in Houston, Texas, US. Received on Fri 16 Mar 2007 09:13:51 PM PDT |
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