Difference between revisions of "March 20, 2012"
| Line 1: | Line 1: | ||
__NOTOC__ | __NOTOC__ | ||
=A Moonlike View= | =A Moonlike View= | ||
| − | |||
<!-- ws:start:WikiTextHeadingRule:0:<h1> --> | <!-- ws:start:WikiTextHeadingRule:0:<h1> --> | ||
<!-- ws:start:WikiTextLocalImageRule:6:<img src="/file/view/LPOD-Mar20-12.jpg/312645612/LPOD-Mar20-12.jpg" alt="" title="" style="width: 900px;" /> -->[[File:LPOD-Mar20-12.jpg|LPOD-Mar20-12.jpg]]<!-- ws:end:WikiTextLocalImageRule:6 --><br /> | <!-- ws:start:WikiTextLocalImageRule:6:<img src="/file/view/LPOD-Mar20-12.jpg/312645612/LPOD-Mar20-12.jpg" alt="" title="" style="width: 900px;" /> -->[[File:LPOD-Mar20-12.jpg|LPOD-Mar20-12.jpg]]<!-- ws:end:WikiTextLocalImageRule:6 --><br /> | ||
| − | <em>image by [mailto:sheehan41@charter.net Bill Sheehan]</em><br /> | + | <em>image by [mailto:sheehan41@charter.net" rel="nofollow Bill Sheehan]</em><br /> |
<br /> | <br /> | ||
East and West Clearwater Lakes are nearly touching, simultaneously-formed impact craters cutting into the ancient rocks of the Canadian Shield of Quebec, Canada. East Clearwater Lake crater - in front - is 26 km wide, and the far, western one is 36 km in diameter. This difference in diameter apparently spans the transition from complex craters to peak ring basins, known first from the Moon. On the Moon the transition occurs at much larger diameter than on Earth, or Mars and Mercury - the transition diameter is inversely related to gravity, so for big Earth basin morphology begins at about 30 km diameter. The larger crater has an inner basin ring of islands that are covered with impact melt. You might notice that the smaller crater doesn't look like a complex crater, but if you could drain the lake you would find a central mountain, not quite tall enough to break the waves. These craters were formed, perhaps from an asteroid or comet that got gravitationally pulled apart before impacting, 290 million years ago, after Aristarchus but before Tycho. Perhaps some of the ejecta from the Lakes craters escaped Earth's gravity and awaits recovery on the Moon. And somewhere on Earth there is undoubtedly ejecta from the formation of Tycho and Aristarchus. <br /> | East and West Clearwater Lakes are nearly touching, simultaneously-formed impact craters cutting into the ancient rocks of the Canadian Shield of Quebec, Canada. East Clearwater Lake crater - in front - is 26 km wide, and the far, western one is 36 km in diameter. This difference in diameter apparently spans the transition from complex craters to peak ring basins, known first from the Moon. On the Moon the transition occurs at much larger diameter than on Earth, or Mars and Mercury - the transition diameter is inversely related to gravity, so for big Earth basin morphology begins at about 30 km diameter. The larger crater has an inner basin ring of islands that are covered with impact melt. You might notice that the smaller crater doesn't look like a complex crater, but if you could drain the lake you would find a central mountain, not quite tall enough to break the waves. These craters were formed, perhaps from an asteroid or comet that got gravitationally pulled apart before impacting, 290 million years ago, after Aristarchus but before Tycho. Perhaps some of the ejecta from the Lakes craters escaped Earth's gravity and awaits recovery on the Moon. And somewhere on Earth there is undoubtedly ejecta from the formation of Tycho and Aristarchus. <br /> | ||
<br /> | <br /> | ||
| − | <em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> | + | <em>[mailto:tychocrater@yahoo.com" rel="nofollow Chuck Wood]</em><br /> |
<br /> | <br /> | ||
<strong>Technical Details</strong><br /> | <strong>Technical Details</strong><br /> | ||
| Line 14: | Line 13: | ||
<br /> | <br /> | ||
<strong>Related Links</strong><br /> | <strong>Related Links</strong><br /> | ||
| − | A [http://www.artofmosaic.com/Img1795_Clearwater_Lakes.asp mosaic] view of the lakes (unexpected!)<br /> | + | A [http://www.artofmosaic.com/Img1795_Clearwater_Lakes.asp" rel="nofollow mosaic] view of the lakes (unexpected!)<br /> |
| − | Jim Head's [http://www.planetary.brown.edu/pdfs/3925.pdf model] for crater to two-ring basin transition.<br /> | + | Jim Head's [http://www.planetary.brown.edu/pdfs/3925.pdf" rel="nofollow model] for crater to two-ring basin transition.<br /> |
<br /> | <br /> | ||
<hr /> | <hr /> | ||
Revision as of 21:28, 4 January 2015
A Moonlike View
image by " rel="nofollow Bill Sheehan
East and West Clearwater Lakes are nearly touching, simultaneously-formed impact craters cutting into the ancient rocks of the Canadian Shield of Quebec, Canada. East Clearwater Lake crater - in front - is 26 km wide, and the far, western one is 36 km in diameter. This difference in diameter apparently spans the transition from complex craters to peak ring basins, known first from the Moon. On the Moon the transition occurs at much larger diameter than on Earth, or Mars and Mercury - the transition diameter is inversely related to gravity, so for big Earth basin morphology begins at about 30 km diameter. The larger crater has an inner basin ring of islands that are covered with impact melt. You might notice that the smaller crater doesn't look like a complex crater, but if you could drain the lake you would find a central mountain, not quite tall enough to break the waves. These craters were formed, perhaps from an asteroid or comet that got gravitationally pulled apart before impacting, 290 million years ago, after Aristarchus but before Tycho. Perhaps some of the ejecta from the Lakes craters escaped Earth's gravity and awaits recovery on the Moon. And somewhere on Earth there is undoubtedly ejecta from the formation of Tycho and Aristarchus.
" rel="nofollow Chuck Wood
Technical Details
On a flight back from Europe near Hudson's Bay.
Related Links
A " rel="nofollow mosaic view of the lakes (unexpected!)
Jim Head's " rel="nofollow model for crater to two-ring basin transition.
