[meteorite-list] New Theory: Water On Mars Came After Asteroid Impacts
From: Ron Baalke <baalke_at_meteoritecentral.com>
Date: Thu Apr 22 09:53:33 2004 Message-ID: <200212051748.JAA04580_at_zagami.jpl.nasa.gov> http://www.saljournal.com/stories/120502/tec_mars.html New theory: Water on Mars came after asteroid impacts By PAUL RECER Associated Press December 5, 2002 WASHINGTON (AP) -- Mars never had oceans as some researchers have claimed, but instead is a cold, dry planet that was pounded by water-bearing asteroids and showered with scalding rain that carved vast gullies and valleys. This suggests the Red Planet was a less than favorable place for life as we know it, a new study claims. The study, appearing this week in the journal Science, sheds new light on a continuing debate by Mars researchers about how much water there was on Mars, where did it go and how did it form the planet's intricate pattern of canyons, river beds and deltas. Using Mars photos and computer simulations, researchers at the University of Colorado at Boulder concluded that immense asteroids pounded Mars some 3.6 billion years ago, bringing vast quantities of water to the young planet and releasing powerful shock waves of heat that melted existing underground deposits of ice. Owen B. Toon, senior author of the study, said at least 25 craters on Mars were gouged out by asteroids 60 to 150 miles in diameter. The impact of such large space rocks would have propelled into the atmosphere millions of tons of superheated rock vapor and melted ice. It also would have unleashed a blast wave heated to more than 4,000 degrees and blanketed the entire planet with heated rock several hundred feet thick. "The atmosphere would be hotter than a self-cleaning oven," said Toon. "When the water was released from the atmosphere, it would fall as scalding rain." The blanket of hot rocks "would be a global thing, causing rivers to form anywhere. The ice would be melting all over the planet," he said. Based on the erosion features on Mars, the researchers estimated that after a major impact, more than 150 feet of water would flow in some areas, carving the riverine features. By some calculations, they said, there could be many decades with rainfall of 6 feet per year. Between impacts, Toon said, Mars would eventually cool, turning again into a dry, chilled planet with water present only as subsurface ice. "We believe these events caused short periods of a warm and wet climate, but overall, we think Mars has been cold and dry for the majority of its history," said co-author Teresa Segura. Toon said that since the moist and warm periods were short, the conditions were not favorable for life to evolve on the planet's surface. Peter H. Smith, a University of Arizona planetary scientist, said that if warmth and liquid water were available on Mars only episodically, "then you have a pretty gloomy picture for life." But he said there were other forces on the planet, particularly volcanic action, that may have created subsurface pools of water where microscopic life could have lived. "In my opinion, they haven't closed the book on the prospects for the evolution of life on Mars," said Smith. He applauded the study, saying, "Assuming their calculations are correct, this must have happened on Mars." Ronald Greeley, a planetary researcher at Arizona State University, said the study by Toon, Segura and others "has the potential to tie together several loose ends regarding Mars surface history." Water ejected into the atmosphere by asteroid impacts, he said, "could account for many of the apparently water-eroded features." However, Greeley said the study "doesn't put a nail in the coffin" for evolution of life on Mars. Like Smith, he said hydrothermal systems powered by volcanic action and subsurface brine pools could still exist and would be favorable for the evolution of life. Received on Thu 05 Dec 2002 12:48:36 PM PST |
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