Difference between revisions of "October 27, 2010"

From LPOD
Jump to: navigation, search
Line 17: Line 17:
 
<br />
 
<br />
 
<hr />
 
<hr />
<table class="wiki_table">
+
<div>You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591 LPOD!]<br />
<tr>
 
<td><!-- ws:start:WikiTextMediaRule:0:&lt;img src=&quot;http://www.wikispaces.com/site/embedthumbnail/custom/4814793?h=0&amp;w=0&quot; class=&quot;WikiMedia WikiMediaCustom&quot; id=&quot;wikitext@@media@@type=&amp;quot;custom&amp;quot; key=&amp;quot;4814793&amp;quot;&quot; title=&quot;Custom Media&quot;/&gt; --><!-- ws:end:WikiTextMediaRule:0 --><br />
 
</td>
 
<td><!-- ws:start:WikiTextHeadingRule:3:&lt;h3&gt; --><h3 id="toc1"><!-- ws:end:WikiTextHeadingRule:3 -->COMMENTS?</h3>
 
Click the <strong>Discussion</strong> tab above.<br />
 
<hr />
 
The rotating globe shows locations of folks who visit LPOD. The most recent visits include location names - so you can see who else is on when you visit. For example, if you see &quot;Wheeling/ West Virginia&quot; I am probably editing an LPOD. After a few minutes just a small red dot appears.<br />
 
<br />
 
<hr />
 
You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591 LPOD!]<br />
 
</td>
 
</tr>
 
</table>
 
 
</div>
 
</div>
  

Revision as of 22:28, 2 January 2015

Icy or Ice-Free?

LPOD-Oct27-10.jpg
LRO DTM image from NASA/ASU

The south pole of the Moon is where the black lines cross on the rim of Shackleton crater. In this high resolution digital topography image the entire 19 km wide crater is shown as if by X-rays. The walls are smooth because of downslope movement of debris but the flat floor includes some mounds and 8-10 small impact craters. By counting craters on deposits beyond Shackleton's rim Paul Spudis and colleagues estimated that the young looking crater was actually 3.6 billion years old. The craters on the floor of Shackleton suggest that any ice there has been heated and churned repeatedly. This may explain why the Kaguya team found no evidence for ice at the surface of the floor. Obviously the unique history of cratering within each polar crater may determine if comet-deposited ice is preserved. This might help explain why the recent LCROSS results did not include ice in some permanently shadowed crater floors.

Chuck Wood

Technical Details
Admission: I can't find where I got this image on the LRO website - sorry!

Related Links
Rükl plate 73


You can support LPOD when you buy any book from Amazon thru LPOD!

COMMENTS?

Click on this icon File:PostIcon.jpg at the upper right to post a comment.