February 3, 2020

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The Glorious Serpentine Ridge

Originally published August 22, 2010 LPOD-Aug22-10.jpg
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

Yesterday's LPOD: Continuing Deformation

Tomorrow's LPOD: Moon Ball


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