Difference between revisions of "July 28, 2012"

From LPOD
Jump to: navigation, search
Line 3: Line 3:
 
<!-- ws:start:WikiTextHeadingRule:0:&lt;h1&gt; -->
 
<!-- ws:start:WikiTextHeadingRule:0:&lt;h1&gt; -->
 
<!-- ws:start:WikiTextLocalImageRule:6:&lt;img src=&quot;/file/view/LPOD-Jul28-12.jpg/355131622/LPOD-Jul28-12.jpg&quot; alt=&quot;&quot; title=&quot;&quot; /&gt; -->[[File:LPOD-Jul28-12.jpg|LPOD-Jul28-12.jpg]]<!-- ws:end:WikiTextLocalImageRule:6 --><br />
 
<!-- ws:start:WikiTextLocalImageRule:6:&lt;img src=&quot;/file/view/LPOD-Jul28-12.jpg/355131622/LPOD-Jul28-12.jpg&quot; alt=&quot;&quot; title=&quot;&quot; /&gt; -->[[File:LPOD-Jul28-12.jpg|LPOD-Jul28-12.jpg]]<!-- ws:end:WikiTextLocalImageRule:6 --><br />
<em>image by [mailto:coutege@wanadoo.fr" rel="nofollow Gerard Coute], Chateaugay, France</em><br />
+
<em>image by [mailto:coutege@wanadoo.fr Gerard Coute], Chateaugay, France</em><br />
 
<br />
 
<br />
 
I observed last night in appalling turbulence conditions after a very hot day (38 ° C). But it allowed me to notice something I had never seen before, a fault in Vallis Alpes. This was confirmed by LRO ACTREACT QuickMap Path; the difference in elevation is about 230 m in 11 km. I also found that Vallis Alpes has an asymmetrical profile, it rises from east to west about 500m (- 3000m to - 2500 m) in 80 km, until the fault, then presents a flat profile at an altitude of - 2700 m to its junction with Imbrium. Another remark: the rough floor of W Bond while Barrow and Meton are smooth, ejecta / intrusive basalt?. Here's proof that a picture is never bad. You must just make it sing.<br />
 
I observed last night in appalling turbulence conditions after a very hot day (38 ° C). But it allowed me to notice something I had never seen before, a fault in Vallis Alpes. This was confirmed by LRO ACTREACT QuickMap Path; the difference in elevation is about 230 m in 11 km. I also found that Vallis Alpes has an asymmetrical profile, it rises from east to west about 500m (- 3000m to - 2500 m) in 80 km, until the fault, then presents a flat profile at an altitude of - 2700 m to its junction with Imbrium. Another remark: the rough floor of W Bond while Barrow and Meton are smooth, ejecta / intrusive basalt?. Here's proof that a picture is never bad. You must just make it sing.<br />
 
<br />
 
<br />
<em>[mailto:coutege@wanadoo.fr" rel="nofollow Gerard Coute]</em><br />
+
<em>[mailto:coutege@wanadoo.fr Gerard Coute]</em><br />
 
<br />
 
<br />
 
Technical details<br />
 
Technical details<br />

Revision as of 17:52, 11 January 2015

Just Make It Sing

LPOD-Jul28-12.jpg
image by Gerard Coute, Chateaugay, France

I observed last night in appalling turbulence conditions after a very hot day (38 ° C). But it allowed me to notice something I had never seen before, a fault in Vallis Alpes. This was confirmed by LRO ACTREACT QuickMap Path; the difference in elevation is about 230 m in 11 km. I also found that Vallis Alpes has an asymmetrical profile, it rises from east to west about 500m (- 3000m to - 2500 m) in 80 km, until the fault, then presents a flat profile at an altitude of - 2700 m to its junction with Imbrium. Another remark: the rough floor of W Bond while Barrow and Meton are smooth, ejecta / intrusive basalt?. Here's proof that a picture is never bad. You must just make it sing.

Gerard Coute

Technical details
2012 07 26, 20 h 05 UT - Mewlon 210 F/D 11.5 + DMK 31 , 4000 images with Registax 6

Related Links
Rükl plate 12