Difference between revisions of "April 17, 2005"

From LPOD
Jump to: navigation, search
 
(5 intermediate revisions by the same user not shown)
Line 1: Line 1:
 
__NOTOC__
 
__NOTOC__
 
=Collapsing Mountain?=
 
=Collapsing Mountain?=
 +
<!-- Start of content -->
 
<table width="85%"  border="0" align="center" cellpadding="6" cellspacing="2">
 
<table width="85%"  border="0" align="center" cellpadding="6" cellspacing="2">
 
<tr>
 
<tr>
Line 12: Line 13:
 
</table>
 
</table>
 
<table width="80%"  border="0" align="center" cellpadding="8">
 
<table width="80%"  border="0" align="center" cellpadding="8">
<tr><td><div align="center" class="main_sm">Image Credit: [mailto:mwirths@superaje.com Mike Wirths]</p>
+
<tr><td><div align="center" class="main_sm"><p>Image Credit: [mailto:mwirths@superaje.com Mike Wirths]</p>
 
</div></td>
 
</div></td>
 
</tr>   
 
</tr>   
Line 26: Line 27:
 
March 20, 2005. 18" Starmaster + 5X's powermate + a Baader 685nm IR passband filter.</p>
 
March 20, 2005. 18" Starmaster + 5X's powermate + a Baader 685nm IR passband filter.</p>
 
<p><b>Related Links:</b><br>
 
<p><b>Related Links:</b><br>
[[iv_132_h1.jpg|Lunar Orbiter IV View ]]
+
[http://www.lpi.usra.edu/resources/lunar_orbiter/images/img/iv_132_h1.jpg Lunar Orbiter IV View ]
 
<br>Rukl Plate 53
 
<br>Rukl Plate 53
 
</p>
 
</p>
<p align="left"><b>Tomorrow's LPOD: </b> Unknown right now!</p>
+
<p><b>Yesterday's LPOD:</b> [[April 16, 2005|Ridgeback Crater]] </p>
 +
<p><b>Tomorrow's LPOD:</b> [[April 18, 2005|The Lunar Crater Wood]] </p>
 
</tr>
 
</tr>
 
</table>
 
</table>
Line 40: Line 42:
 
<p align="center" class="main_titles"><b>Author &amp; Editor:</b><br>  
 
<p align="center" class="main_titles"><b>Author &amp; Editor:</b><br>  
 
[mailto:tychocrater@yahoo.com Charles A. Wood]</p>
 
[mailto:tychocrater@yahoo.com Charles A. Wood]</p>
<p align="center" class="main_titles"><b>Technical Consultant:</b><br>
+
<!-- Cleanup of credits -->
[mailto:anthony@perseus.gr Anthony Ayiomamitis]</p>
+
<!-- Cleanup of credits -->
<p align="center" class="main_titles"><b>Contact Translator:</b><br>
+
<!-- Cleanup of credits -->
[mailto:pablolonnie@yahoo.com.mx Pablo Lonnie Pacheco Railey]  (Es)<br>
+
<!-- Cleanup of credits -->
[mailto:chlegrand@free.fr Christian Legrand] (Fr)</p>
+
<!-- Cleanup of credits -->
<p align="center" class="main_titles"><b>[mailto:webuser@observingthesky.org Contact Webmaster]</b></p>
+
<!-- Cleanup of credits -->
<p align="center" class="main_titles"><b>A service of:</b><br>
+
<!-- Cleanup of credits -->
[http://www.observingthesky.org/ ObservingTheSky.Org]</p>
+
<!-- Cleanup of credits -->
<p align="center" class="main_titles"><b>Visit these other PODs:</b> <br>
+
<!-- Cleanup of credits -->
[http://antwrp.gsfc.nasa.gov/apod/astropix.html Astronomy] | [http://www.msss.com/ Mars] | [http://epod.usra.edu/ Earth]</p>
+
<!-- Cleanup of credits -->
 
</td></tr>
 
</td></tr>
 
</table>  
 
</table>  
 
<p>&nbsp;</p>
 
<p>&nbsp;</p>
----
+
<!-- End of content -->
===COMMENTS?===
+
{{wiki/ArticleFooter}}
Register, and click on the <b>Discussion</b> tab at the top of the page.
 

Latest revision as of 14:14, 15 March 2015

Collapsing Mountain?

LPOD-2005-04-17.jpeg

Image Credit: Mike Wirths


Collapsing Mountain?

Stephen Keene’s image of the Hippalus Arcs is one of my all-time favorite lunar photos. The focus of attention of both Stephen’s previous LPOD image and today’s excellent one by Mike Wirths is the set of curved graben that mark where the lunar surface fractured when the weight of the Humorum lavas caused that basin center to subside. But on Mike’s image I immediately noticed something that I hadn’t seen before. The isolated peak left of center has a lobe of material to the left. It appears that the graben cuts this lobe because a faint trace of the graben edge is visible through the deposit. A more interesting interpretation is that the lobe flowed down from the mountain as a giant landslide. Landslides are rare on the Moon, but common elsewhere, especially on Mars and Jupiter’s moon Io. Landslides occur most readily where there is a weak layer that breaks apart and collapses gravitationally under stress. Probably most lunar scientists would say that the lobe is simply a residual piece of old lunar terrain surrounded by mare. It probably is, but may not be. This is a good target for hyper-resolution imaging!

Chuck Wood

Technical Details:
March 20, 2005. 18" Starmaster + 5X's powermate + a Baader 685nm IR passband filter.

Related Links:
Lunar Orbiter IV View
Rukl Plate 53

Yesterday's LPOD: Ridgeback Crater

Tomorrow's LPOD: The Lunar Crater Wood



Author & Editor:
Charles A. Wood

 


COMMENTS?

Register, Log in, and join in the comments.