Difference between revisions of "March 26, 2006"

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=The Brightest Taurid=
 
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<p>[[File:LPOD-Mar26Romer.jpg|Romer-Higgins]]<br />
 
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<p>[[File:LPOD-Mar26Romer.jpg|Romer-Higgins]]<br />
 
 
<em>image by [mailto:starman2@charter.ne  Wes Higgins]</em></p>
 
<em>image by [mailto:starman2@charter.ne  Wes Higgins]</em></p>
 
<p>The Taurus Mountains are a ill-defined piece of lunar real estate with only one fresh crater, the floor-challenged Römer. The unnecessarily named Sinus Amoris - what is there to love about it? - and a piece of the Römer Rille complete the inventory of named features here. But Wes&#8217; image - the only close-up I&#8217;ve ever seen of this crater - shows that 40 km wide Römer is an unusual crater. The terraces of most lunar craters are 5-10 km wide at their tops and appear to be substantial chunks of rock that have coherently slide downslope. Römer&#8217;s terraces are thin slivers of material - the rock in this area must be less coherent than other places. The small crater that impacted on the inner slope of Römer smoothed the nearby wall, erasing the terraces, and is itself distorted by downslope movement. This is a nice example of how subsequent impacts justle the terraces of crater walls, gradually smoothing out topography. And where is the floor of Römer? It has been covered by terrace debris, but there may be more to the story. In Römer, as in the same sized and floorless Alpetragius, the central peak is broader than is typical. Perhaps the conditions that give rise to the thin terraces also produce the broad peak.</p>
 
<p>The Taurus Mountains are a ill-defined piece of lunar real estate with only one fresh crater, the floor-challenged Römer. The unnecessarily named Sinus Amoris - what is there to love about it? - and a piece of the Römer Rille complete the inventory of named features here. But Wes&#8217; image - the only close-up I&#8217;ve ever seen of this crater - shows that 40 km wide Römer is an unusual crater. The terraces of most lunar craters are 5-10 km wide at their tops and appear to be substantial chunks of rock that have coherently slide downslope. Römer&#8217;s terraces are thin slivers of material - the rock in this area must be less coherent than other places. The small crater that impacted on the inner slope of Römer smoothed the nearby wall, erasing the terraces, and is itself distorted by downslope movement. This is a nice example of how subsequent impacts justle the terraces of crater walls, gradually smoothing out topography. And where is the floor of Römer? It has been covered by terrace debris, but there may be more to the story. In Römer, as in the same sized and floorless Alpetragius, the central peak is broader than is typical. Perhaps the conditions that give rise to the thin terraces also produce the broad peak.</p>
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Rükl plate 25<br />
 
Rükl plate 25<br />
 
[http://higginsandsons.com/astro/ Wes’ lunar photos]</p>
 
[http://higginsandsons.com/astro/ Wes’ lunar photos]</p>
<p align="center"><b>SUPPORT LPOD - VISIT A SPONSOR (CLICK AN AD BELOW)! </b><br />
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<p><b>Yesterday's LPOD:</b> [[March 25, 2006|Nomenclature Zoo]] </p>
<i>Now you can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=102  LPOD!]</i></p>
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<p><b>Tomorrow's LPOD:</b> [[March 27, 2006|Amazing Grace]] </p>
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<p> </p>
===COMMENTS?===
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Latest revision as of 22:51, 8 February 2015

The Brightest Taurid

Romer-Higgins
image by Wes Higgins

The Taurus Mountains are a ill-defined piece of lunar real estate with only one fresh crater, the floor-challenged Römer. The unnecessarily named Sinus Amoris - what is there to love about it? - and a piece of the Römer Rille complete the inventory of named features here. But Wes’ image - the only close-up I’ve ever seen of this crater - shows that 40 km wide Römer is an unusual crater. The terraces of most lunar craters are 5-10 km wide at their tops and appear to be substantial chunks of rock that have coherently slide downslope. Römer’s terraces are thin slivers of material - the rock in this area must be less coherent than other places. The small crater that impacted on the inner slope of Römer smoothed the nearby wall, erasing the terraces, and is itself distorted by downslope movement. This is a nice example of how subsequent impacts justle the terraces of crater walls, gradually smoothing out topography. And where is the floor of Römer? It has been covered by terrace debris, but there may be more to the story. In Römer, as in the same sized and floorless Alpetragius, the central peak is broader than is typical. Perhaps the conditions that give rise to the thin terraces also produce the broad peak.

Chuck Wood

Technical Details:
04/14/05, 18″ Starmaster Reflector, DMK-21FO4 camera, MAP processing, 30fps, stack of 505 frames.

Related Links:
Rükl plate 25
Wes’ lunar photos

Yesterday's LPOD: Nomenclature Zoo

Tomorrow's LPOD: Amazing Grace


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