Difference between revisions of "August 22, 2010"
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| − | <em>image by [mailto:daversin.bruno@neuf.fr | + | <em>image by [mailto:daversin.bruno@neuf.fr Bruno Daversin], France</em><br /> |
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| − | One of the most wondrous lunar sights can be observed when the Moon is 6 days old. Paralleling the eastern shore of Mare Serenitatis is the snakelike Serpentine Ridge. This fine name has been around since Schroeter (1790s), but the IAU, in their woeful ignorance of history and selenology, gave different parts of this obvious single structure two unnecessary names: Dorsum Smirnov and Dorsum Lister. Bruno Daversin's exquisite image reveals both the broad and detailed structure of this wrinkle ridge system. Mare ridges generally have a a wide swelling with one edge being steeper-sided and higher. This can be well seen near the crater Very (large crater near the upper left). From [http://www.lpi.usra.edu/resources/mapcatalog/LTO/lto42b3_1/72dpi.jpg | + | One of the most wondrous lunar sights can be observed when the Moon is 6 days old. Paralleling the eastern shore of Mare Serenitatis is the snakelike Serpentine Ridge. This fine name has been around since Schroeter (1790s), but the IAU, in their woeful ignorance of history and selenology, gave different parts of this obvious single structure two unnecessary names: Dorsum Smirnov and Dorsum Lister. Bruno Daversin's exquisite image reveals both the broad and detailed structure of this wrinkle ridge system. Mare ridges generally have a a wide swelling with one edge being steeper-sided and higher. This can be well seen near the crater Very (large crater near the upper left). From [http://www.lpi.usra.edu/resources/mapcatalog/LTO/lto42b3_1/72dpi.jpg LTO 42B3] we can see that the broad part of the ridge rises as much as 200 m over a horizontal distance of 4-5 km, but the steep part of the ridge rises 200 m higher in a distance of a little less than a kilometer. At the southern end of the ridge there is a strongly curved arc that looks almost like a crater rim. And unlike the rest of the ridge, this arc has its tall side on the eastern edge of the broad structure. I don't know what that means, but it is different. Near the top right corner of this scene (near the crater Borel) is a lower ridge system that may actually be a ghost crater - i.e. ridges marking a lava-covered crater. Other images of the area show that the ridge continues as almost a full circle. In general, Serenitatis must be deep, for few partially flooded craters exist there, but it makes sense that this ridge may be a buried crater because it is on the shallow outer bench of the mare.<br /> |
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| − | <em>[mailto:tychocrater@yahoo.com | + | <em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> |
| − | <em>This is a classic LPOD from [http://www.lpod.org/archive/LPOD-2004-11-17.htm | + | <em>This is a classic LPOD from [http://www.lpod.org/archive/LPOD-2004-11-17.htm Nov 11, 2004]. I'll be happy when more current images are available!</em><br /> |
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<strong>Technical Details</strong><br /> | <strong>Technical Details</strong><br /> | ||
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| − | <div>You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591 | + | <div>You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591 LPOD!]<br /> |
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===COMMENTS?=== | ===COMMENTS?=== | ||
| − | + | Register, and click on the <b>Discussion</b> tab at the top of the page. | |
Revision as of 17:23, 11 January 2015
The Glorious Serpentine Ridge
image by Bruno Daversin, France
One of the most wondrous lunar sights can be observed when the Moon is 6 days old. Paralleling the eastern shore of Mare Serenitatis is the snakelike Serpentine Ridge. This fine name has been around since Schroeter (1790s), but the IAU, in their woeful ignorance of history and selenology, gave different parts of this obvious single structure two unnecessary names: Dorsum Smirnov and Dorsum Lister. Bruno Daversin's exquisite image reveals both the broad and detailed structure of this wrinkle ridge system. Mare ridges generally have a a wide swelling with one edge being steeper-sided and higher. This can be well seen near the crater Very (large crater near the upper left). From LTO 42B3 we can see that the broad part of the ridge rises as much as 200 m over a horizontal distance of 4-5 km, but the steep part of the ridge rises 200 m higher in a distance of a little less than a kilometer. At the southern end of the ridge there is a strongly curved arc that looks almost like a crater rim. And unlike the rest of the ridge, this arc has its tall side on the eastern edge of the broad structure. I don't know what that means, but it is different. Near the top right corner of this scene (near the crater Borel) is a lower ridge system that may actually be a ghost crater - i.e. ridges marking a lava-covered crater. Other images of the area show that the ridge continues as almost a full circle. In general, Serenitatis must be deep, for few partially flooded craters exist there, but it makes sense that this ridge may be a buried crater because it is on the shallow outer bench of the mare.
Chuck Wood
This is a classic LPOD from Nov 11, 2004. I'll be happy when more current images are available!
Technical Details
Sept 4, 2004. Ludiver Observatory 600 mm (24") Schmidt-Cassegrain & B&W webcam.
Related Links
Rükl plate 24
COMMENTS?
Register, and click on the Discussion tab at the top of the page.
