Difference between revisions of "November 15, 2012"
| (8 intermediate revisions by the same user not shown) | |||
| Line 1: | Line 1: | ||
__NOTOC__ | __NOTOC__ | ||
=Naughty Rays= | =Naughty Rays= | ||
| − | + | <!-- Start of content --> | |
<!-- ws:start:WikiTextHeadingRule:0:<h1> --> | <!-- ws:start:WikiTextHeadingRule:0:<h1> --> | ||
<!-- ws:start:WikiTextLocalImageRule:6:<img src="http://lpod.wikispaces.com/file/view/LPOD-Nov15-12.jpg/382578574/LPOD-Nov15-12.jpg" alt="" title="" /> -->[[File:LPOD-Nov15-12.jpg|LPOD-Nov15-12.jpg]]<!-- ws:end:WikiTextLocalImageRule:6 --><br /> | <!-- ws:start:WikiTextLocalImageRule:6:<img src="http://lpod.wikispaces.com/file/view/LPOD-Nov15-12.jpg/382578574/LPOD-Nov15-12.jpg" alt="" title="" /> -->[[File:LPOD-Nov15-12.jpg|LPOD-Nov15-12.jpg]]<!-- ws:end:WikiTextLocalImageRule:6 --><br /> | ||
<em>image by [mailto:howardeskildsen@msn.com Howard Eskildsen], Ocala, Florida</em><br /> | <em>image by [mailto:howardeskildsen@msn.com Howard Eskildsen], Ocala, Florida</em><br /> | ||
<br /> | <br /> | ||
| − | If ever a lettered crater deserved a name it was Olbers A, the magnificent 43 km wide rayed crater known since 1993 as Glushko. | + | If ever a lettered crater deserved a name it was Olbers A, the magnificent 43 km wide rayed crater known since 1993 as Glushko. |
| − | Rays from Glushko extend toward the farside and across Oceanus Procellarum. Especially famous is the ray that curves between | + | Rays from Glushko extend toward the farside and across Oceanus Procellarum. Especially famous is the ray that curves between |
| − | Cardanus and Seleucus. Rather than bemoan our failure to understand the exact ejection mechanics that produced the odd ray | + | Cardanus and Seleucus. Rather than bemoan our failure to understand the exact ejection mechanics that produced the odd ray |
| − | we should just accept it, just as we do tangential rays, and marvel at the amazing complexity of impact cratering. A high Sun, | + | we should just accept it, just as we do tangential rays, and marvel at the amazing complexity of impact cratering. A high Sun, |
| − | overhead view - courtesy of [http://www.mapaplanet.org/explorer-bin/explorer.cgi?map=Moon&layers=moon_clementine_base_v2&west=271.18&south=2.52&east=293.68&north=13.80&center_lat=0&center=282.43&defaultcenter=on&grid=none&stretch=auto&projection=SIMP&r=1&g=1&b=1&advoption=NO&info=NO&resolution=32&scale=1.89520&imageTopX=-681327.7906775475&imageTopY=590357.7379584312 Clementine,] reveals that Glushko was formed by a low angle oblique impact for there are few rays to | + | overhead view - courtesy of [http://www.mapaplanet.org/explorer-bin/explorer.cgi?map=Moon&layers=moon_clementine_base_v2&west=271.18&south=2.52&east=293.68&north=13.80&center_lat=0&center=282.43&defaultcenter=on&grid=none&stretch=auto&projection=SIMP&r=1&g=1&b=1&advoption=NO&info=NO&resolution=32&scale=1.89520&imageTopX=-681327.7906775475&imageTopY=590357.7379584312 Clementine,] reveals that Glushko was formed by a low angle oblique impact for there are few rays to |
| − | the NNW or SSE. Just looking at the ray distribution it is hard to determine which direction the projectile came from, but [http://lpod. | + | the NNW or SSE. Just looking at the ray distribution it is hard to determine which direction the projectile came from, but [http://www2.lpod.org/wiki/August_16,_2011 radar] |
| − | reveals splashes of impact melt to the NNW, suggesting that the projectile came from the opposite direction and transferred its | + | reveals splashes of impact melt to the NNW, suggesting that the projectile came from the opposite direction and transferred its |
| − | momentum to the melt.<br /> | + | momentum to the melt. |
| + | <br /> | ||
<br /> | <br /> | ||
<em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> | <em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> | ||
<br /> | <br /> | ||
<strong>Related Links</strong><br /> | <strong>Related Links</strong><br /> | ||
| − | Rükl plate [ | + | Rükl plate [https://the-moon.us/wiki/R%C3%BCkl_28 28]<br /> |
<br /> | <br /> | ||
| + | <p><b>Yesterday's LPOD:</b> [[November 14, 2012|A Long Cool One]] </p> | ||
| + | <p><b>Tomorrow's LPOD:</b> [[November 16, 2012|Crescent Sun]] </p> | ||
<hr /> | <hr /> | ||
| + | {{wiki/ArticleFooter}} | ||
Latest revision as of 08:34, 28 October 2018
Naughty Rays
image by Howard Eskildsen, Ocala, Florida
If ever a lettered crater deserved a name it was Olbers A, the magnificent 43 km wide rayed crater known since 1993 as Glushko.
Rays from Glushko extend toward the farside and across Oceanus Procellarum. Especially famous is the ray that curves between
Cardanus and Seleucus. Rather than bemoan our failure to understand the exact ejection mechanics that produced the odd ray
we should just accept it, just as we do tangential rays, and marvel at the amazing complexity of impact cratering. A high Sun,
overhead view - courtesy of Clementine, reveals that Glushko was formed by a low angle oblique impact for there are few rays to
the NNW or SSE. Just looking at the ray distribution it is hard to determine which direction the projectile came from, but radar
reveals splashes of impact melt to the NNW, suggesting that the projectile came from the opposite direction and transferred its
momentum to the melt.
Chuck Wood
Related Links
Rükl plate 28
Yesterday's LPOD: A Long Cool One
Tomorrow's LPOD: Crescent Sun
COMMENTS?
Register, Log in, and join in the comments.
