Difference between revisions of "October 21, 2013"
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| − | <em>image by [mailto:gari@adbooth.net Gari Arrillaga]</em><br /> | + | <em>image by [mailto:gari@adbooth.net" rel="nofollow Gari Arrillaga]</em><br /> |
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Do you notice anything unusual about the distribution of one type of landform here? The mare ridges snake around everywhere on the right side of the scene. But inside the ridge that defines Ancient Thebit there are essentially no ridges. I wonder why. Some of the quasi-circular ridges apparenly are ghost craters, marking the rims of lava-covered craters on the Nubium Basin floor. But many aren't. They also don't define a compelling inner circle as at Imbrium and other basins. If mare ridges result from the settling of a thick pond of frozen lava into a smaller volume as the basin floor subsides the lack of a pattern at Nubium makes the subsidence process hard to understand. The lack of ridges inside Ancient Thebit - around the Straight Wall - could be because the faulting released stresses in this portion of the mare. <br /> | Do you notice anything unusual about the distribution of one type of landform here? The mare ridges snake around everywhere on the right side of the scene. But inside the ridge that defines Ancient Thebit there are essentially no ridges. I wonder why. Some of the quasi-circular ridges apparenly are ghost craters, marking the rims of lava-covered craters on the Nubium Basin floor. But many aren't. They also don't define a compelling inner circle as at Imbrium and other basins. If mare ridges result from the settling of a thick pond of frozen lava into a smaller volume as the basin floor subsides the lack of a pattern at Nubium makes the subsidence process hard to understand. The lack of ridges inside Ancient Thebit - around the Straight Wall - could be because the faulting released stresses in this portion of the mare. <br /> | ||
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| − | <em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> | + | <em>[mailto:tychocrater@yahoo.com" rel="nofollow Chuck Wood]</em><br /> |
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<strong>Related Links</strong><br /> | <strong>Related Links</strong><br /> | ||
Revision as of 22:51, 4 January 2015
Familiar Terrain Seen a Little Differently
image by " rel="nofollow Gari Arrillaga
Do you notice anything unusual about the distribution of one type of landform here? The mare ridges snake around everywhere on the right side of the scene. But inside the ridge that defines Ancient Thebit there are essentially no ridges. I wonder why. Some of the quasi-circular ridges apparenly are ghost craters, marking the rims of lava-covered craters on the Nubium Basin floor. But many aren't. They also don't define a compelling inner circle as at Imbrium and other basins. If mare ridges result from the settling of a thick pond of frozen lava into a smaller volume as the basin floor subsides the lack of a pattern at Nubium makes the subsidence process hard to understand. The lack of ridges inside Ancient Thebit - around the Straight Wall - could be because the faulting released stresses in this portion of the mare.
" rel="nofollow Chuck Wood
Related Links
21st Century Atlas chart 16.
