NASA Space Craft Detects Buried Glaciers on Mars

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thor06

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<p>Wow!&nbsp; </p><p>&nbsp; &nbsp; When do we go?&nbsp; This is the most amazing discovery yet IMO.&nbsp; Both in terms of possible life and for resource gathering on manned missions.&nbsp; Take the "drill baby drill" mentality to mars!</p><p>The site:</p><p>MRO discovers buried glaciers </p><p>&nbsp;</p><p>If this is already being discussed elsewhere let me know.... </p> <div class="Discussion_UserSignature"> <p> </p><p> <font color="#0000ff">                           www.watchnasatv.com</font></p><p>                          ONE PERCENT FOR NASA! </p> </div>
 
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BrianSlee

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Replying to:<BR/><DIV CLASS='Discussion_PostQuote'>Wow!&nbsp; &nbsp; &nbsp; When do we go?&nbsp; This is the most amazing discovery yet IMO.&nbsp; Both in terms of possible life and for resource gathering on manned missions.&nbsp; Take the "drill baby drill" mentality to mars!The site:MRO discovers buried glaciers &nbsp;If this is already being discussed elsewhere let me know.... <br />Posted by thor06</DIV><br /><br />Wow is right.&nbsp; This is monumental if true. <div class="Discussion_UserSignature"> <p> </p><p>"I am therefore I think" </p><p>"The only thing "I HAVE TO DO!!" is die, in everything else I have freewill" Brian P. Slee</p> </div>
 
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exoscientist

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<p><font size="2">Anyone know how thick is the dust over cover of the glaciers?<br /> There have been theories that might be relict glaciers left at near equatorial locations on Mars, but the consensus view is that they should have sublimated away even with a dust over cover.<br /> However with Mars Phoenix showing water ice precipitation occurs in the north polar region that raises the possibility it could very well occur at other locations on Mars thus providing the water precipitation to replenish the glaciers.<br /><br /> ==================================<br /> 01-October-2008, 04:59 PM<br /> RGClark<br /> Senior Member<br /> Join Date: Feb 2004<br /> Location: Philadelphia, PA<br /><br /> ...<br /> Obviously, the important thing here is that it was water ice snow that was shown to be falling at the Phoenix site. The previous observations showed that CO2 snow could fall at the south pole.<br /> This is important because it will suggest the possibility this can be wide spread on Mars, which will have important implications for the Mars water cycle.<br /> Two very key questions it can have application to are the observation of geologically recent glaciers on Mars and the high H2O content from GRS readings even at equatorial locations.<br /> For the first, glaciers normally require precipitation to be active, but these recent glaciers would have been active during the current geological epoch where the possibility of water precipitation has been largely disregarded.<br /> For the second, the question was always asked where could this water have come from for this water at the equator? Answer: because of the extensive and frequent systems of clouds near the equator they could have provided wide spread water deposition near the equator from cloud precipitation.<br /><br /><br /> Bob Clark<br /> ==============================<br />http://www.bautforum.com/space-exploration/78062-phoenix-mars-extended-mission-6.html#post1334859<br /><br />&nbsp;</font> </p><p><font size="2">&nbsp;Notice also that the Hellas basin where some of the still existing glaciers were found is frequently a site of low lying clouds/fogs:<br /><br /> Martian Clouds.<br /> ...<br /> "Fog<br /> Fog often appears in low-lying areas. It typically occurs in the southern hemisphere especially in the Argyre and Hellas basins. It forms frequently in craters. Occasionally, it occurs in higher regions such as Sinus Sabaeus and Solis Planum."<br />http://www.solarviews.com/eng/marscld.htm#views <br /><br /> Image of fogs over Hellas:<br />http://www.solarviews.com/raw/mars/fog.gif<br /><br /> Bob Clark</font> </p> <div class="Discussion_UserSignature"> </div>
 
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3488

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<p><font size="2"><strong>What about Deuteronilus Mensae? </strong></font></p><p><font size="2"><strong>Fascinating feature in the mid latitudes in the northern hemisphere. Sure looks like a glacier to me.<br /></strong></font></p><p><strong><font size="3">ESA DLR Mars Express article.&nbsp;</font></strong></p><p><font size="4">Merging lobate scarps in Deuteronilus Mensae MRO.&nbsp;</font></p><p><font size="4">Scarps in Deuteronilus Mensae MRO.&nbsp;</font></p><p><font size="4">Flow form MRO HiRISE.&nbsp;</font></p><p><font size="4">Lobate Debris Aprons MRO HiRISE.&nbsp;</font></p><p><font size="4">Mesas, Massifs & Debris Aprons MRO HiRISE.&nbsp;</font></p><p><font size="4">Mars Odyssey THEMIS evaluation of Deuteronilus Mensae.&nbsp;</font></p><p><font size="4">Mars Odyssey THEMIS showing flow forms in Deuteronilus Mensae.&nbsp;</font></p><p><font size="2"><strong>Andrew Brown.&nbsp;</strong></font></p> <div class="Discussion_UserSignature"> <p><font color="#000080">"I suddenly noticed an anomaly to the left of Io, just off the rim of that world. It was extremely large with respect to the overall size of Io and crescent shaped. It seemed unbelievable that something that big had not been visible before".</font> <em><strong><font color="#000000">Linda Morabito </font></strong><font color="#800000">on discovering that the Jupiter moon Io was volcanically active. Friday 9th March 1979.</font></em></p><p><font size="1" color="#000080">http://www.launchphotography.com/</font><br /><br /><font size="1" color="#000080">http://anthmartian.googlepages.com/thisislandearth</font></p><p><font size="1" color="#000080">http://web.me.com/meridianijournal</font></p> </div>
 
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