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| =Mersenius West= | | =Mersenius West= |
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| + | <p>[[File:MerseniusArea-Pettenpaul.jpg|MerseniusArea-Pettenpaul.jpg]]<br /> |
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− | <p><img id="image1672" src="http://www.lpod.org/wp-content/uploads/2008/01/MerseniusArea-Pettenpaul.jpg" alt="MerseniusArea-Pettenpaul.jpg"/><br />
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| <em>image by [mailto:oliver@galaxyso.de Oliver Pettenpaul]</em></p> | | <em>image by [mailto:oliver@galaxyso.de Oliver Pettenpaul]</em></p> |
− | <p>Mare Humorum and Orientale are such compelling targets that the region between is often overlooked. Oliver has resisted that urge and captured a wonderful image of this complex area. The jumbled texture between the craters is ejecta from the formation of various basins, with that from the Humorum Basin being buried by debris from Imbrium and then Orientale. Some of the isolated mountain masses are probably segments of the basin’s rings. At bottom right is a pond of lava captured between the Humorum mare-edge ring (diameter 425 km according to Paul Spudis) and the next one out. This mare patch is cut by linear rilles whose directions seem unrelated to Humorum basin structure. One rille peters out in the basin debris between Mersenius (top-right) and Cavendish (bottom-center). The nearly twin craters once [http://the-moon.wikispaces.com/Henry+Frères named] for the 19th century Henry brothers are at far left. The main focus of attention though is Mersenius, whose floor is [http://www.lpod.org/archive/archive/2004/04/LPOD-2004-04-03.htm rarely imaged] so clearly. The rilles have an odd distribution, being mainly on the western half of the floor - I wonder why?</p> | + | <p>Mare Humorum and Orientale are such compelling targets that the region between is often overlooked. Oliver has resisted that urge and captured a wonderful image of this complex area. The jumbled texture between the craters is ejecta from the formation of various basins, with that from the Humorum Basin being buried by debris from Imbrium and then Orientale. Some of the isolated mountain masses are probably segments of the basin’s rings. At bottom right is a pond of lava captured between the Humorum mare-edge ring (diameter 425 km according to Paul Spudis) and the next one out. This mare patch is cut by linear rilles whose directions seem unrelated to Humorum basin structure. One rille peters out in the basin debris between Mersenius (top-right) and Cavendish (bottom-center). The nearly twin craters once [https://the-moon.us/wiki/Henry_Frères named] for the 19th century Henry brothers are at far left. The main focus of attention though is Mersenius, whose floor is [[April_3,_2004|rarely imaged]] so clearly. The rilles have an odd distribution, being mainly on the western half of the floor - I wonder why?</p> |
| <p>[mailto:tychocrater@yahoo.com Chuck Wood]</p> | | <p>[mailto:tychocrater@yahoo.com Chuck Wood]</p> |
| <p><strong>Technical Details</strong><br /> | | <p><strong>Technical Details</strong><br /> |
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| <p><strong>Related Links:</strong><br /> | | <p><strong>Related Links:</strong><br /> |
| Rükl plate 51<br /> | | Rükl plate 51<br /> |
− | [www.astro-imaging.de/astro Oliver’s website]</p> | + | [http://www.astro-imaging.de/astro Oliver’s website]</p> |
− | <p><em>LPOD earns a commision when you buy ANY book from Amazon thru [[LPOD]] Have you bought a book lately?</em></p> | + | <p><b>Yesterday's LPOD:</b> [[January 6, 2008|Inconspicuous Volcanics]] </p> |
− | </div>
| + | <p><b>Tomorrow's LPOD:</b> [[January 8, 2008|Crystal Skyring]] </p> |
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− | ===COMMENTS?===
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