Difference between revisions of "April 24, 2007"

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=Magnificent Side View=
 
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<p>[[File:2007_04_21_19_34_54_Red_Humboldt_flat.jpg|2007_04_21_19_34_54_Red_Humboldt_flat.jpg]]<br />
 
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<p>[[File:2007_04_21_19_34_54_Red_Humboldt_flat.jpg|2007_04_21_19_34_54_Red_Humboldt_flat.jpg]]<br />
 
 
<em>image by [mailto:pete.lawrence@digitalsky.org.uk  Pete Lawrence], Selsey, England.</em></p>
 
<em>image by [mailto:pete.lawrence@digitalsky.org.uk  Pete Lawrence], Selsey, England.</em></p>
 
<p>This wonderful image emphasizes the steep walls that surround the 207 km wide Humboldt crater. The walls look absolutely shear with no irregularities until the jumbled pile of slumped material is reached at their bottoms.  The scarped rim is missing on the farside of the crater in the region behind the three craters on the floor of Humboldt and behind the nearby dark pyroclastic deposit. This area is not well imaged from space, but the poor Orbiter IV [http://www.lpod.org/coppermine/displayimage.php?album=9&#038;pos=31 image] shows that at least part of this missing zone occurs where Humboldt&#8217;s rim intersects a pre-existing crater. A more clear, non-overhead view, from [http://www.lpod.org/?m=20060206 Apollo 15] confirms that formation of Humboldt&#8217;s rim was severely modified by this pre-existing low spot. The very strong rim scarp occurs where Humboldt is nearly tangent to the older crater [http://www.lpod.org/coppermine/displayimage.php?album=9&#038;pos=32 Barnard] to the right. In this case, the adjacent crater seems to have been a buttress that supported a larger than normal scarp. Finally, the middle of the three craters on the farside of Humboldt&#8217;s floor is a famous concentric crater. Pete&#8217;s image is the only Earth-based view that I am aware of that hints at the existence of the inner donut.</p>
 
<p>This wonderful image emphasizes the steep walls that surround the 207 km wide Humboldt crater. The walls look absolutely shear with no irregularities until the jumbled pile of slumped material is reached at their bottoms.  The scarped rim is missing on the farside of the crater in the region behind the three craters on the floor of Humboldt and behind the nearby dark pyroclastic deposit. This area is not well imaged from space, but the poor Orbiter IV [http://www.lpod.org/coppermine/displayimage.php?album=9&#038;pos=31 image] shows that at least part of this missing zone occurs where Humboldt&#8217;s rim intersects a pre-existing crater. A more clear, non-overhead view, from [http://www.lpod.org/?m=20060206 Apollo 15] confirms that formation of Humboldt&#8217;s rim was severely modified by this pre-existing low spot. The very strong rim scarp occurs where Humboldt is nearly tangent to the older crater [http://www.lpod.org/coppermine/displayimage.php?album=9&#038;pos=32 Barnard] to the right. In this case, the adjacent crater seems to have been a buttress that supported a larger than normal scarp. Finally, the middle of the three craters on the farside of Humboldt&#8217;s floor is a famous concentric crater. Pete&#8217;s image is the only Earth-based view that I am aware of that hints at the existence of the inner donut.</p>
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[http://www.digitalsky.org.uk/ Pete&#8217;s spectacular web site]<br />
 
[http://www.digitalsky.org.uk/ Pete&#8217;s spectacular web site]<br />
 
A new [http://www.thenation.com/doc/20070430/anderson novel] about the naturalist Humboldt and his compatriot Gauss.</p>
 
A new [http://www.thenation.com/doc/20070430/anderson novel] about the naturalist Humboldt and his compatriot Gauss.</p>
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===COMMENTS?===  
 
===COMMENTS?===  
 
Click on this icon [[image:PostIcon.jpg]] at the upper right to post a comment.
 
Click on this icon [[image:PostIcon.jpg]] at the upper right to post a comment.

Revision as of 17:52, 4 January 2015

Magnificent Side View

2007_04_21_19_34_54_Red_Humboldt_flat.jpg
image by Pete Lawrence, Selsey, England.

This wonderful image emphasizes the steep walls that surround the 207 km wide Humboldt crater. The walls look absolutely shear with no irregularities until the jumbled pile of slumped material is reached at their bottoms. The scarped rim is missing on the farside of the crater in the region behind the three craters on the floor of Humboldt and behind the nearby dark pyroclastic deposit. This area is not well imaged from space, but the poor Orbiter IV image shows that at least part of this missing zone occurs where Humboldt’s rim intersects a pre-existing crater. A more clear, non-overhead view, from Apollo 15 confirms that formation of Humboldt’s rim was severely modified by this pre-existing low spot. The very strong rim scarp occurs where Humboldt is nearly tangent to the older crater Barnard to the right. In this case, the adjacent crater seems to have been a buttress that supported a larger than normal scarp. Finally, the middle of the three craters on the farside of Humboldt’s floor is a famous concentric crater. Pete’s image is the only Earth-based view that I am aware of that hints at the existence of the inner donut.

Chuck Wood

Technical Details:
April 21, 2007, 19:35 UT. Celestron C-14 + Lumenera SKYnyx 2-0M + Astronomik red filter.

Related links:
Rükl plate 60
Pete’s spectacular web site
A new novel about the naturalist Humboldt and his compatriot Gauss.


COMMENTS?

Click on this icon File:PostIcon.jpg at the upper right to post a comment.