Difference between revisions of "January 25, 2006"

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=Subtle Lineations=
 
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<p>[[File:Delambre_20051023_0239_zann.jpg|Delambre-Zaannelli]]<br />
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<p>[[File:Delambre_20051023_0239_zann.jpg|Delambre-Zaannelli]]<br />
 
 
<em>image by [mailto:c.zannelli@virgilio.it Carmelo Zannelli]</em></p>
 
<em>image by [mailto:c.zannelli@virgilio.it Carmelo Zannelli]</em></p>
 
<p>Delambre is a standard, mid-size (diameter 52 km) crater with slumped terraces and some sort of odd layer across the floor, perhaps covering a central peak. But in looking closely at Carmelo’s technically fine image the eye sees a persistent pattern of lineations that trend from north-northwest to south-southeast. This subtle grain parallels the edges of ruined craters and secondary crater chains on the left side of the image. These features are both delicate and coarse reminders of the surge of ejecta that scoured the surface from the formation of the Imbrium basin about 3.8 billion years ago. But now look even more closely at the top and bottom of Delambre – there is a faint but definite pattern of lineations nearly at right angles to the Imbrium direction. Narrow, bright-edged parallel ridges cross the northern (top) portion of Delembre’s rim and extend pass Delambre D (the small crater on its rim) to the east for 5-10 km. And southwest of Delambre’s southern rim are hints of a wider, longer and more obscure pattern of ridges paralleling those on the north of the crater. This southern strip continues through the crater’s inner wall and perhaps to the southeast of the crater. I have no idea what these ridges are – or even if they are real. Is it possible the subtle ridges perpendicular to the Imbrium direction are an artifact of processing? It seems unlikely because this pattern doesn’t occur anywhere except near Delambre. In looking at Lunar Orbiter images and Consolidated Lunar Atlas images I catch no glimpse of them. But Carmelo’s image combines high resolution and low sun in a way that is superior to either of those earlier images. I think the pattern is real, but what geologically explains it? On Earth, parallel ridges often reflect tilted layers of rocks – that seems unlikely here. I think, once again, that an amateur image shows something that we never knew existed. Great!</p>
 
<p>Delambre is a standard, mid-size (diameter 52 km) crater with slumped terraces and some sort of odd layer across the floor, perhaps covering a central peak. But in looking closely at Carmelo’s technically fine image the eye sees a persistent pattern of lineations that trend from north-northwest to south-southeast. This subtle grain parallels the edges of ruined craters and secondary crater chains on the left side of the image. These features are both delicate and coarse reminders of the surge of ejecta that scoured the surface from the formation of the Imbrium basin about 3.8 billion years ago. But now look even more closely at the top and bottom of Delambre – there is a faint but definite pattern of lineations nearly at right angles to the Imbrium direction. Narrow, bright-edged parallel ridges cross the northern (top) portion of Delembre’s rim and extend pass Delambre D (the small crater on its rim) to the east for 5-10 km. And southwest of Delambre’s southern rim are hints of a wider, longer and more obscure pattern of ridges paralleling those on the north of the crater. This southern strip continues through the crater’s inner wall and perhaps to the southeast of the crater. I have no idea what these ridges are – or even if they are real. Is it possible the subtle ridges perpendicular to the Imbrium direction are an artifact of processing? It seems unlikely because this pattern doesn’t occur anywhere except near Delambre. In looking at Lunar Orbiter images and Consolidated Lunar Atlas images I catch no glimpse of them. But Carmelo’s image combines high resolution and low sun in a way that is superior to either of those earlier images. I think the pattern is real, but what geologically explains it? On Earth, parallel ridges often reflect tilted layers of rocks – that seems unlikely here. I think, once again, that an amateur image shows something that we never knew existed. Great!</p>
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<strong>Related Links:</strong><br />
 
<strong>Related Links:</strong><br />
 
Rükl chart 46</p>
 
Rükl chart 46</p>
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<p><b>Yesterday's LPOD:</b> [[January 24, 2006|Fecund Questions]] </p>
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<p><b>Tomorrow's LPOD:</b> [[January 26, 2006|Humble Topo]] </p>
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===COMMENTS?===
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Click on this icon [[image:PostIcon.jpg]] at the upper right to post a comment.
 

Latest revision as of 19:23, 7 February 2015

Subtle Lineations

Delambre-Zaannelli
image by Carmelo Zannelli

Delambre is a standard, mid-size (diameter 52 km) crater with slumped terraces and some sort of odd layer across the floor, perhaps covering a central peak. But in looking closely at Carmelo’s technically fine image the eye sees a persistent pattern of lineations that trend from north-northwest to south-southeast. This subtle grain parallels the edges of ruined craters and secondary crater chains on the left side of the image. These features are both delicate and coarse reminders of the surge of ejecta that scoured the surface from the formation of the Imbrium basin about 3.8 billion years ago. But now look even more closely at the top and bottom of Delambre – there is a faint but definite pattern of lineations nearly at right angles to the Imbrium direction. Narrow, bright-edged parallel ridges cross the northern (top) portion of Delembre’s rim and extend pass Delambre D (the small crater on its rim) to the east for 5-10 km. And southwest of Delambre’s southern rim are hints of a wider, longer and more obscure pattern of ridges paralleling those on the north of the crater. This southern strip continues through the crater’s inner wall and perhaps to the southeast of the crater. I have no idea what these ridges are – or even if they are real. Is it possible the subtle ridges perpendicular to the Imbrium direction are an artifact of processing? It seems unlikely because this pattern doesn’t occur anywhere except near Delambre. In looking at Lunar Orbiter images and Consolidated Lunar Atlas images I catch no glimpse of them. But Carmelo’s image combines high resolution and low sun in a way that is superior to either of those earlier images. I think the pattern is real, but what geologically explains it? On Earth, parallel ridges often reflect tilted layers of rocks – that seems unlikely here. I think, once again, that an amateur image shows something that we never knew existed. Great!

Chuck Wood

Technical Details:
23 Oct 2005, 235mm SCT @ ~7500 mm + Lumenera Infinity 2-1 M camera + IR cut-off filter; 200 of 1305 stacked frames.
Related Links:
Rükl chart 46

Yesterday's LPOD: Fecund Questions

Tomorrow's LPOD: Humble Topo

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