Difference between revisions of "November 29, 2007"

From LPOD
Jump to: navigation, search
Line 1: Line 1:
 
__NOTOC__
 
__NOTOC__
 
=Not From Orbit=
 
=Not From Orbit=
 +
<div class="post" id="post-1551">
  
+
<div class="storycontent">
<div class="post" id="post-1551">
+
<p>[[File:Posidonius-08-03-07.jpg|Posidonius-08-03-07.jpg]]<br />
 
<div class="storycontent">
 
<p>[[File:Posidonius-08-03-07.jpg|Posidonius-08-03-07.jpg]]<br />
 
 
<em>image by [mailto:starman2@allegiance.tv Wes Higgins]</em></p>
 
<em>image by [mailto:starman2@allegiance.tv Wes Higgins]</em></p>
 
<p>There is no doubt that spacecraft orbiting the Moon can take higher resolution images than amateurs on Earth using backyard telescopes; but spacecraft can&#8217;t outdo Wes for stunning beauty. Posidonius is a favorite crater because of the tilted floor, criss-crossed with rilles, and the lighting of this image gives a hyper-realistic feel for the plasticity of the surface. At the southern part of the plateau, where two rilles cross like an X, there seems to be a subtle doming. In fact, the crossed rille pattern is exactly what modelers get when they uplift a solid surface - cracks made by fracturing, not volcanism. Of course, a rising blob of magma is probably what tilted and uplifted the floor of Posidonius, as well as creating the smaller localized swelling. Wes pointed out another intriguing feature - the worm on the northern part of the lava-covered floor. I don&#8217;t remember ever seeing this feature and am baffled by it. It is too even in width to be a mare ridge, and its abrupt northern end is strange. Perhaps some day we&#8217;ll have a higher resolution orbital view to help interpretation, but I doubt if it will be more dramatic. </p>
 
<p>There is no doubt that spacecraft orbiting the Moon can take higher resolution images than amateurs on Earth using backyard telescopes; but spacecraft can&#8217;t outdo Wes for stunning beauty. Posidonius is a favorite crater because of the tilted floor, criss-crossed with rilles, and the lighting of this image gives a hyper-realistic feel for the plasticity of the surface. At the southern part of the plateau, where two rilles cross like an X, there seems to be a subtle doming. In fact, the crossed rille pattern is exactly what modelers get when they uplift a solid surface - cracks made by fracturing, not volcanism. Of course, a rising blob of magma is probably what tilted and uplifted the floor of Posidonius, as well as creating the smaller localized swelling. Wes pointed out another intriguing feature - the worm on the northern part of the lava-covered floor. I don&#8217;t remember ever seeing this feature and am baffled by it. It is too even in width to be a mare ridge, and its abrupt northern end is strange. Perhaps some day we&#8217;ll have a higher resolution orbital view to help interpretation, but I doubt if it will be more dramatic. </p>
Line 16: Line 14:
 
Another great [http://www.lpod.org/?m=20070428 view]</p>
 
Another great [http://www.lpod.org/?m=20070428 view]</p>
 
<p align="center"><em>Now you can support LPOD when you buy ANY book from Amazon thru [[LPOD]]</em></p>
 
<p align="center"><em>Now you can support LPOD when you buy ANY book from Amazon thru [[LPOD]]</em></p>
</div>
+
</div>
 
 
 
 
----
 
----
 
===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 19:00, 4 January 2015

Not From Orbit

Posidonius-08-03-07.jpg
image by Wes Higgins

There is no doubt that spacecraft orbiting the Moon can take higher resolution images than amateurs on Earth using backyard telescopes; but spacecraft can’t outdo Wes for stunning beauty. Posidonius is a favorite crater because of the tilted floor, criss-crossed with rilles, and the lighting of this image gives a hyper-realistic feel for the plasticity of the surface. At the southern part of the plateau, where two rilles cross like an X, there seems to be a subtle doming. In fact, the crossed rille pattern is exactly what modelers get when they uplift a solid surface - cracks made by fracturing, not volcanism. Of course, a rising blob of magma is probably what tilted and uplifted the floor of Posidonius, as well as creating the smaller localized swelling. Wes pointed out another intriguing feature - the worm on the northern part of the lava-covered floor. I don’t remember ever seeing this feature and am baffled by it. It is too even in width to be a mare ridge, and its abrupt northern end is strange. Perhaps some day we’ll have a higher resolution orbital view to help interpretation, but I doubt if it will be more dramatic.

Chuck Wood

Technical Details:
08-03-07. 18" Reflector, Infinity 2-1m camera, MAP /99, Registered AVI processing, stack of 540 frames.

Related Links:
Rükl plate 14
Another great view

Now you can support LPOD when you buy ANY book from Amazon thru LPOD


COMMENTS?

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