Difference between revisions of "May 5, 2010"

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<em>image by [mailto:jocelyn.serot@wanadoo.fr" rel="nofollow Jocelyn Sérot], France</em><br />
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<em>image by [mailto:jocelyn.serot@wanadoo.fr Jocelyn Sérot], France</em><br />
 
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Is this a corner of the Moon you overlook? Have you specifically observed any of these craters? I thought not. The north eastern limb is an area lacking in remarkable craters, has only the smallest patch of mare lava, and generally looks tired. There are no detected basins right here to provide interesting rilles and wrinkle ridges. Its not as highly cratered as the farside so at some point the really old craters were erased. About the only way to erase things is a large impact, so perhaps Spei does mark the location of an ancient [http://lpod.wikispaces.com/April+5%2C+2010 |basin], gone except for crustal weaknesses that later allowed a little magma to reach the surface. This area was apparently much more interesting 3-4 billion years ago. We came too late for the best view.<br />
 
Is this a corner of the Moon you overlook? Have you specifically observed any of these craters? I thought not. The north eastern limb is an area lacking in remarkable craters, has only the smallest patch of mare lava, and generally looks tired. There are no detected basins right here to provide interesting rilles and wrinkle ridges. Its not as highly cratered as the farside so at some point the really old craters were erased. About the only way to erase things is a large impact, so perhaps Spei does mark the location of an ancient [http://lpod.wikispaces.com/April+5%2C+2010 |basin], gone except for crustal weaknesses that later allowed a little magma to reach the surface. This area was apparently much more interesting 3-4 billion years ago. We came too late for the best view.<br />
 
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<em>[mailto:tychocrater@yahoo.com" rel="nofollow Chuck Wood]</em><br />
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<em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br />
 
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<strong>Technical Details</strong><br />
 
<strong>Technical Details</strong><br />
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<strong>Related Links</strong><br />
 
<strong>Related Links</strong><br />
 
Rükl plate [http://the-moon.wikispaces.com/R%C3%BCkl+16 16]<br />
 
Rükl plate [http://the-moon.wikispaces.com/R%C3%BCkl+16 16]<br />
Jocelyn's updated lunar [http://pagesperso-orange.fr/legalet/AstroLG/Lune.html" rel="nofollow website]<br />
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Jocelyn's updated lunar [http://pagesperso-orange.fr/legalet/AstroLG/Lune.html website]<br />
 
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You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591" rel="nofollow LPOD!] || ||
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You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591 LPOD!] || ||
 
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===COMMENTS?===  
 
===COMMENTS?===  
Click on this icon [[image:PostIcon.jpg]] at the upper right to post a comment.
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Register, and click on the <b>Discussion</b> tab at the top of the page.

Revision as of 17:19, 11 January 2015

Hidden Ancient History

LPOD-May5-10.jpg
image by Jocelyn Sérot, France

Is this a corner of the Moon you overlook? Have you specifically observed any of these craters? I thought not. The north eastern limb is an area lacking in remarkable craters, has only the smallest patch of mare lava, and generally looks tired. There are no detected basins right here to provide interesting rilles and wrinkle ridges. Its not as highly cratered as the farside so at some point the really old craters were erased. About the only way to erase things is a large impact, so perhaps Spei does mark the location of an ancient |basin, gone except for crustal weaknesses that later allowed a little magma to reach the surface. This area was apparently much more interesting 3-4 billion years ago. We came too late for the best view.

Chuck Wood

Technical Details
Apr 29, 2010 around 0:15 UT. Mewlon 210 at prime focus, Astronomik red filter, DMK 31AF03, 9 images assembled, 250/1000 images stacked for each. Processing Avistack + Registax.

Related Links
Rükl plate 16
Jocelyn's updated lunar website


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


COMMENTS?

Register, and click on the Discussion tab at the top of the page.