Difference between revisions of "October 13, 2010"

From LPOD
Jump to: navigation, search
 
(4 intermediate revisions by the same user not shown)
Line 1: Line 1:
 
__NOTOC__
 
__NOTOC__
 
=Little Marked Mare=
 
=Little Marked Mare=
 +
<!-- Start of content -->
 
<!-- ws:start:WikiTextHeadingRule:1:&lt;h1&gt; -->
 
<!-- ws:start:WikiTextHeadingRule:1:&lt;h1&gt; -->
 
<!-- ws:start:WikiTextLocalImageRule:16:&lt;img src=&quot;/file/view/LPOD-Oct13-10.jpg/169997063/LPOD-Oct13-10.jpg&quot; alt=&quot;&quot; title=&quot;&quot; /&gt; -->[[File:LPOD-Oct13-10.jpg|LPOD-Oct13-10.jpg]]<!-- ws:end:WikiTextLocalImageRule:16 --><br />
 
<!-- ws:start:WikiTextLocalImageRule:16:&lt;img src=&quot;/file/view/LPOD-Oct13-10.jpg/169997063/LPOD-Oct13-10.jpg&quot; alt=&quot;&quot; title=&quot;&quot; /&gt; -->[[File:LPOD-Oct13-10.jpg|LPOD-Oct13-10.jpg]]<!-- ws:end:WikiTextLocalImageRule:16 --><br />
<em>image by [[mailto:|Daniel Chang]], Hong Kong</em><br />
+
<em>image by Daniel Chang, Hong Kong</em><br />
 
<br />
 
<br />
Photoshop out Messier and its A and this region would be nearly unidentifiable. The mare of Fecunditatis has massive but little known ridges, and little else. The ridges show no obvious evidence of being inner rings of an impact basin - if there is an ancient basin filled by Mare Fecunditatis little structural evidence for it remains. The impact crater [http://the-moon.wikispaces.com/Ibn+Battuta Ibn Battuta] is the sole oddity because it was surrounded by lavas that rose to its rim crest but stopped before flooding into the crater. <br />
+
Photoshop out Messier and its A and this region would be nearly unidentifiable. The mare of Fecunditatis has massive but little known ridges, and little else. The ridges show no obvious evidence of being inner rings of an impact basin - if there is an ancient basin filled by Mare Fecunditatis little structural evidence for it remains. The impact crater [https://the-moon.us/wiki/Ibn_Battuta Ibn Battuta] is the sole oddity because it was surrounded by lavas that rose to its rim crest but stopped before flooding into the crater. <br />
 
<br />
 
<br />
 
<em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br />
 
<em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br />
Line 15: Line 16:
 
<br />
 
<br />
 
<strong>Related Links</strong><br />
 
<strong>Related Links</strong><br />
Rükl plate [http://the-moon.wikispaces.com/R%C3%BCkl+48 48]<br />
+
Rükl plate [https://the-moon.us/wiki/R%C3%BCkl_48 48]<br />
 
Daniel's image [http://picasaweb.google.com.hk/daniel.changck collection]<br />
 
Daniel's image [http://picasaweb.google.com.hk/daniel.changck collection]<br />
 
<br />
 
<br />
<hr />
 
 
<p><b>Yesterday's LPOD:</b> [[October 12, 2010|Northern Exposure]] </p>
 
<p><b>Yesterday's LPOD:</b> [[October 12, 2010|Northern Exposure]] </p>
 
<p><b>Tomorrow's LPOD:</b> [[October 14, 2010|Goodacre's Imbrium]] </p>
 
<p><b>Tomorrow's LPOD:</b> [[October 14, 2010|Goodacre's Imbrium]] </p>
 +
<hr />
 +
<table class="wiki_table">
 +
<tr>
 +
<td> <!-- RemoveRevolverMaps -->
 +
<!-- RemoveRevolverMaps -->
 +
</td>
 +
<!-- End of content -->
 
{{wiki/ArticleFooter}}
 
{{wiki/ArticleFooter}}

Latest revision as of 17:55, 13 October 2018

Little Marked Mare

LPOD-Oct13-10.jpg
image by Daniel Chang, Hong Kong

Photoshop out Messier and its A and this region would be nearly unidentifiable. The mare of Fecunditatis has massive but little known ridges, and little else. The ridges show no obvious evidence of being inner rings of an impact basin - if there is an ancient basin filled by Mare Fecunditatis little structural evidence for it remains. The impact crater Ibn Battuta is the sole oddity because it was surrounded by lavas that rose to its rim crest but stopped before flooding into the crater.

Chuck Wood
This image was found on the LPOD Photo Gallery.
Waiting for the first Chilean miner to appear above ground...


Technical Details
2010/06/29 18:42UT. Mewlon 180 f/30 DBK21.AF.04

Related Links
Rükl plate 48
Daniel's image collection

Yesterday's LPOD: Northern Exposure

Tomorrow's LPOD: Goodacre's Imbrium



COMMENTS?

Register, Log in, and join in the comments.