Difference between revisions of "October 20, 2010"

From LPOD
Jump to: navigation, search
Line 1: Line 1:
 
__NOTOC__
 
__NOTOC__
 
=Fake Lava=
 
=Fake Lava=
 
 
<!-- ws:start:WikiTextHeadingRule:1:&lt;h1&gt; -->
 
<!-- ws:start:WikiTextHeadingRule:1:&lt;h1&gt; -->
 
<!-- ws:start:WikiTextLocalImageRule:16:&lt;img src=&quot;/file/view/LPOD-Oct-20-10.jpg/171946189/LPOD-Oct-20-10.jpg&quot; alt=&quot;&quot; title=&quot;&quot; /&gt; -->[[File:LPOD-Oct-20-10.jpg|LPOD-Oct-20-10.jpg]]<!-- ws:end:WikiTextLocalImageRule:16 --><br />
 
<!-- ws:start:WikiTextLocalImageRule:16:&lt;img src=&quot;/file/view/LPOD-Oct-20-10.jpg/171946189/LPOD-Oct-20-10.jpg&quot; alt=&quot;&quot; title=&quot;&quot; /&gt; -->[[File:LPOD-Oct-20-10.jpg|LPOD-Oct-20-10.jpg]]<!-- ws:end:WikiTextLocalImageRule:16 --><br />
<em>image by [mailto:jl.dauvergne@cieletespace.fr Jean-Luc Dauvergne], Elie Rousset &amp; Philippe Tosi, S2P / IMCCE / Obs. Midi, Pic du Midi, France</em><br />
+
<em>image by [mailto:jl.dauvergne@cieletespace.fr" rel="nofollow Jean-Luc Dauvergne], Elie Rousset &amp; Philippe Tosi, S2P / IMCCE / Obs. Midi, Pic du Midi, France</em><br />
 
<br />
 
<br />
To detect the rille on the floor of Moretus you can look at Lunar Orbiter [http://www.lpod.org/coppermine/displayimage.php?pid=2240&amp;fullsize=1 images], but there is better lighting on the telescopic image of JLuc and friends. The short rille cuts the relatively smooth surface that probably isn't a lava flow because no recognized volcanics are anywhere near this area of the Moon. The smooth material is most likely impact melt which does in some places show fractures, but this looks more like a volcanic type rille than a melt fracture. There is no other evidence for volcanism so this implies that impact melts may more closely mimic lavas than I previously thought.<br />
+
To detect the rille on the floor of Moretus you can look at Lunar Orbiter [http://www.lpod.org/coppermine/displayimage.php?pid=2240&amp;fullsize=1" rel="nofollow images], but there is better lighting on the telescopic image of JLuc and friends. The short rille cuts the relatively smooth surface that probably isn't a lava flow because no recognized volcanics are anywhere near this area of the Moon. The smooth material is most likely impact melt which does in some places show fractures, but this looks more like a volcanic type rille than a melt fracture. There is no other evidence for volcanism so this implies that impact melts may more closely mimic lavas than I previously thought.<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 16: Line 15:
 
<strong>Related Links</strong><br />
 
<strong>Related Links</strong><br />
 
Rükl plate [http://the-moon.wikispaces.com/R%C3%BCkl+73 73]<br />
 
Rükl plate [http://the-moon.wikispaces.com/R%C3%BCkl+73 73]<br />
JL Dauvergne [http://astrophotography.fr/ website]<br />
+
JL Dauvergne [http://astrophotography.fr/" rel="nofollow website]<br />
IMCCE [http://www.imcce.fr/langues/fr/ website]<br />
+
IMCCE [http://www.imcce.fr/langues/fr/" rel="nofollow website]<br />
Obs. Midi Pyrénées [http://ezomp.omp.obs-mip.fr/ website]<br />
+
Obs. Midi Pyrénées [http://ezomp.omp.obs-mip.fr/" rel="nofollow website]<br />
 
<br />
 
<br />
 
<hr />
 
<hr />
<div>You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591 LPOD!]<br />
+
<div>You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591" rel="nofollow LPOD!]<br />
 
</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 22:08, 4 January 2015

Fake Lava

LPOD-Oct-20-10.jpg
image by " rel="nofollow Jean-Luc Dauvergne, Elie Rousset & Philippe Tosi, S2P / IMCCE / Obs. Midi, Pic du Midi, France

To detect the rille on the floor of Moretus you can look at Lunar Orbiter " rel="nofollow images, but there is better lighting on the telescopic image of JLuc and friends. The short rille cuts the relatively smooth surface that probably isn't a lava flow because no recognized volcanics are anywhere near this area of the Moon. The smooth material is most likely impact melt which does in some places show fractures, but this looks more like a volcanic type rille than a melt fracture. There is no other evidence for volcanism so this implies that impact melts may more closely mimic lavas than I previously thought.

" rel="nofollow Chuck Wood

Technical Details
2010 september 29, ~4h59TU. 1 m telescope + Skynyx 2-1 + near IR filter
(>680nm); mosaïc of 4 images.

Related Links
Rükl plate 73
JL Dauvergne " rel="nofollow website
IMCCE " rel="nofollow website
Obs. Midi Pyrénées " rel="nofollow website


You can support LPOD when you buy any book from Amazon thru " rel="nofollow LPOD!

COMMENTS?

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