Difference between revisions of "January 8, 2007"

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=A Dome on the Limb=
 
=A Dome on the Limb=
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<p>[[File:Lyot_2006_11_05.jpg|lyot_2006_11_05.jpg]]</p>
 
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<p>[[File:Lyot_2006_11_05.jpg|lyot_2006_11_05.jpg]]</p>
 
 
<p><em>image by [mailto:dpeach_78@yahoo.co.uk Damian Peach]</em></p>
 
<p><em>image by [mailto:dpeach_78@yahoo.co.uk Damian Peach]</em></p>
<p>Far out on the Moon&#8217;s southeast limb is [http://www.lpod.org/archive/archive/2004/05/LPOD-2004-05-18.htm Mare Australe], a rimless collection of mare-filled craters and mare patches that are all that&#8217;s left of an ancient impact basin. The features in Australe are too squashed by foreshortening to be well studied from Earth, until now. Damian has captured a remarkable high resolution, low-Sun view of Lyot, the largest crater within Australe. A high-Sun Clementine [http://www.lpod.org/coppermine/displayimage.php?album=28&#038;pos=7 image] shows that the northwestern quadrant of Lyot is dark mare and the rest is older and perhaps dusted by highland ejecta. On Damian&#8217;s image this difference is indicated by the greater number of craters and greater roughness of the southern part of the floor. A few mare ridges and a ghost crater are visible on the floor, but most interestingly - and apparently unknown - is the large dome at the northern end of the floor. Its diameter is 13 km - scaled from the 38 km length of Lyot A, the bright crater at upper left. The existence of this dome is interesting because Australe, despite its abundance of mare has few small volcanic eruption landforms such as domes, sinuous rilles and volcanic dark halo craters. But while researching this dome I discovered one more and a swell on another part of Australe!
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<p>Far out on the Moon&#8217;s southeast limb is [[May_18,_2004|Mare Australe]], a rimless collection of mare-filled craters and mare patches that are all that&#8217;s left of an ancient impact basin. The features in Australe are too squashed by foreshortening to be well studied from Earth, until now. Damian has captured a remarkable high resolution, low-Sun view of Lyot, the largest crater within Australe. A high-Sun Clementine [http://www.lpod.org/coppermine/displayimage.php?album=28&#038;pos=7 image] shows that the northwestern quadrant of Lyot is dark mare and the rest is older and perhaps dusted by highland ejecta. On Damian&#8217;s image this difference is indicated by the greater number of craters and greater roughness of the southern part of the floor. A few mare ridges and a ghost crater are visible on the floor, but most interestingly - and apparently unknown - is the large dome at the northern end of the floor. Its diameter is 13 km - scaled from the 38 km length of Lyot A, the bright crater at upper left. The existence of this dome is interesting because Australe, despite its abundance of mare has few small volcanic eruption landforms such as domes, sinuous rilles and volcanic dark halo craters. But while researching this dome I discovered one more and a swell on another part of Australe!
 
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<p>[mailto:tychocrater@yahoo.com Chuck Wood]</p>
 
<p>[mailto:tychocrater@yahoo.com Chuck Wood]</p>
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Rükl chart 76<br />
 
Rükl chart 76<br />
 
[http://www.damianpeach.com/lunar.htm Damian&#8217;s website]</p>
 
[http://www.damianpeach.com/lunar.htm Damian&#8217;s website]</p>
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<p><b>Yesterday's LPOD:</b> [[January 7, 2007|Lacus Niger Major]] </p>
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<p><b>Tomorrow's LPOD:</b> [[January 9, 2007|Sunrise on an Unflat Plain]] </p>
 
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Latest revision as of 11:49, 22 March 2015

A Dome on the Limb

lyot_2006_11_05.jpg

image by Damian Peach

Far out on the Moon’s southeast limb is Mare Australe, a rimless collection of mare-filled craters and mare patches that are all that’s left of an ancient impact basin. The features in Australe are too squashed by foreshortening to be well studied from Earth, until now. Damian has captured a remarkable high resolution, low-Sun view of Lyot, the largest crater within Australe. A high-Sun Clementine image shows that the northwestern quadrant of Lyot is dark mare and the rest is older and perhaps dusted by highland ejecta. On Damian’s image this difference is indicated by the greater number of craters and greater roughness of the southern part of the floor. A few mare ridges and a ghost crater are visible on the floor, but most interestingly - and apparently unknown - is the large dome at the northern end of the floor. Its diameter is 13 km - scaled from the 38 km length of Lyot A, the bright crater at upper left. The existence of this dome is interesting because Australe, despite its abundance of mare has few small volcanic eruption landforms such as domes, sinuous rilles and volcanic dark halo craters. But while researching this dome I discovered one more and a swell on another part of Australe!

Chuck Wood

Technical Details:
6 November, 2006. C14 @ F25. Lumenera Skynyx 2.0M.

Related Links:
Rükl chart 76
Damian’s website

Yesterday's LPOD: Lacus Niger Major

Tomorrow's LPOD: Sunrise on an Unflat Plain


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