Difference between revisions of "August 15, 2013"
| Line 3: | Line 3: | ||
<!-- ws:start:WikiTextHeadingRule:0:<h1> --> | <!-- ws:start:WikiTextHeadingRule:0:<h1> --> | ||
<!-- ws:start:WikiTextLocalImageRule:6:<img src="/file/view/LPOD-Aug15-13.jpg/444885794/LPOD-Aug15-13.jpg" alt="" title="" /> -->[[File:LPOD-Aug15-13.jpg|LPOD-Aug15-13.jpg]]<!-- ws:end:WikiTextLocalImageRule:6 --><br /> | <!-- ws:start:WikiTextLocalImageRule:6:<img src="/file/view/LPOD-Aug15-13.jpg/444885794/LPOD-Aug15-13.jpg" alt="" title="" /> -->[[File:LPOD-Aug15-13.jpg|LPOD-Aug15-13.jpg]]<!-- ws:end:WikiTextLocalImageRule:6 --><br /> | ||
| − | <em>north to the upper right image by [mailto:aerts.leo@skynet.be | + | <em>north to the upper right image by [mailto:aerts.leo@skynet.be Leo Aerts], Belgium</em><br /> |
<br /> | <br /> | ||
Sabine and Ritter are a pair, like Atlas and Hercules, and Aristoteles and Eudoxus. These are all separate craters but because for each set <br /> | Sabine and Ritter are a pair, like Atlas and Hercules, and Aristoteles and Eudoxus. These are all separate craters but because for each set <br /> | ||
| Line 11: | Line 11: | ||
lunar scientists in the 1960s and 70s. But then in 1976 Peter Schultz recognized such inner-ringed craters as a class of modified impact crater<br /> | lunar scientists in the 1960s and 70s. But then in 1976 Peter Schultz recognized such inner-ringed craters as a class of modified impact crater<br /> | ||
called [http://the-moon.wikispaces.com/Floor+Fractured+Craters floor-fractured craters] (FFC), and the volcanic camp disappeared. Sabine has relatively little on its floor except a broad ring, reminiscent<br /> | called [http://the-moon.wikispaces.com/Floor+Fractured+Craters floor-fractured craters] (FFC), and the volcanic camp disappeared. Sabine has relatively little on its floor except a broad ring, reminiscent<br /> | ||
| − | of [http://lroc.sese.asu.edu/news/index.php?/archives/794-Oblique-Image-of-Concentric-Crater.html | + | of [http://lroc.sese.asu.edu/news/index.php?/archives/794-Oblique-Image-of-Concentric-Crater.html concentric craters]. Ritter's interior is more complex with a broad wreath of hilly terrain, obviously buttressed by debris that slid down its <br /> |
crater walls, and three or possibly four rilles wiggle through the wreath. Ritter could almost not be a FFC but simply a crater with heavy wall <br /> | crater walls, and three or possibly four rilles wiggle through the wreath. Ritter could almost not be a FFC but simply a crater with heavy wall <br /> | ||
slumps that circle its floor. Sabine seems harder to explain that way. Notice also the relation of these craters to the mare. The craters cover <br /> | slumps that circle its floor. Sabine seems harder to explain that way. Notice also the relation of these craters to the mare. The craters cover <br /> | ||
| Line 17: | Line 17: | ||
Sabine and Ritter are covered by the mare lavas, indicating that the craters are younger than the lavas. What do you think?<br /> | Sabine and Ritter are covered by the mare lavas, indicating that the craters are younger than the lavas. What do you think?<br /> | ||
<br /> | <br /> | ||
| − | <em>[mailto:tychocrater@yahoo.com | + | <em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> |
<br /> | <br /> | ||
<strong>Technical Details</strong><br /> | <strong>Technical Details</strong><br /> | ||
Revision as of 18:08, 11 January 2015
Younger? Older?
north to the upper right image by Leo Aerts, Belgium
Sabine and Ritter are a pair, like Atlas and Hercules, and Aristoteles and Eudoxus. These are all separate craters but because for each set
the two are near each other and look somewhat similar they always get considered together. Sabine - at center right- and Ritter - just above
Sabine - do look similar in diameter, general degree of erosion, and concentric inner structure. With nearby Delambre (half-shadowed) as a
reminder of what a complex impact crater should look like, Sabine and Ritter don't fit. They were considered likely volcanic craters by some
lunar scientists in the 1960s and 70s. But then in 1976 Peter Schultz recognized such inner-ringed craters as a class of modified impact crater
called floor-fractured craters (FFC), and the volcanic camp disappeared. Sabine has relatively little on its floor except a broad ring, reminiscent
of concentric craters. Ritter's interior is more complex with a broad wreath of hilly terrain, obviously buttressed by debris that slid down its
crater walls, and three or possibly four rilles wiggle through the wreath. Ritter could almost not be a FFC but simply a crater with heavy wall
slumps that circle its floor. Sabine seems harder to explain that way. Notice also the relation of these craters to the mare. The craters cover
some of the broad-floor rilles that run both below and above them showing that the craters are younger than the rille. But the ejecta from
Sabine and Ritter are covered by the mare lavas, indicating that the craters are younger than the lavas. What do you think?
Chuck Wood
Technical Details
March 18th 2013, 18h25 UT. C14, 1.8x barlow projection and redfilter. I used a DMK31AU03 webcam.
Related Links
21st Century Atlas chart 7.
