Difference between revisions of "July 28, 2012"
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| − | <em>image by [mailto:coutege@wanadoo.fr Gerard Coute], Chateaugay, France</em><br /> | + | <em>image by [mailto:coutege@wanadoo.fr" rel="nofollow Gerard Coute], Chateaugay, France</em><br /> |
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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 /> | ||
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| − | <em>[mailto:coutege@wanadoo.fr Gerard Coute]</em><br /> | + | <em>[mailto:coutege@wanadoo.fr" rel="nofollow Gerard Coute]</em><br /> |
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Technical details<br /> | Technical details<br /> | ||
Revision as of 21:34, 4 January 2015
Just Make It Sing
image by " rel="nofollow 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.
" rel="nofollow 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
