Difference between revisions of "July 22, 2004"

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      <td><h2 align="left">Huge Fractures</h2></td>
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      <td><h2 align="right">July 22, 2004</h2></td>
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    [javascript:;" onMouseOver="MM_swapImage('Image1','','images/LPOD-2004-07-22b.jpeg',1)" onMouseOut="MM_swapImgRestore() <img src="images/LPOD-2004-07-22.jpeg" name="Image1" width="427" height="425" border="0" id="Image1">]</a>
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      <td><div align="center" span class="main_sm">Image Credit: [mailto:bobbotts@cogeco.ca Bob Botts] </div></td>
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These images are remarkable in showing the tectonic structure southeast of Mare Nectaris. And because Bob Botts took images on successive nights of the waning Moon we can see the same area illuminated and then deeply shadowed. The area SE of Nectaris is well known for its strong and conspicuous radial basin structures. Both the Snellius and Rheita Valleys (black lines on mouseover) are large secondary crater chains caused by mountainous blocks ejected during the formation of the Nectaris impact basin. But Bott's image shows other larger dislocations of the crust also radial to Nectaris. The Oct. 13 view shows a big slab of ground (labeled B for block) that casts a shadow to the north and is bounded on the south by a long, bright line that passes through Brenner. Block B appears to be fault-bounded and higher than the surfaces to its north and south. The previous night's view (remember these are sunset images so the terminator hides land to the east every night) reveals that the low land to the north of block B is partially flat and covered with smooth material. This makes sense, for mare lavas - or other flows - would be expected in lowlands. If block B did move differentially compared to its surroundings then it is one of the largest such blocks on the Moon - except for the truly gigantic circular faults like the Apennines and Altai that define impact basins.
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    <p align="right" class="story">&#8212; [mailto:chuck@observingthesky.org Chuck Wood]</blockquote>
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  <p class"story"><b>Technical Details:</b><br>
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    October 12 and 13, 2003. 12&quot; SCT f10 with Toucam webcam, processed&nbsp;using Registax</p>
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  <p class"story"><b>Related Links:</b> <br>
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    [http://www.lpi.usra.edu/research/lunar_orbiter/images/aimg/iv_064_h3.jpg Lunar Orbiter IV View] (notice fault)</p>
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  <p class"story"><b>Tomorrow's LPOD:</b> Sun, Moon and Stars </p>
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      <td><p align="center" class="main_titles"><b>Author & Editor:</b><br>
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          [mailto:chuck@observingthesky.org Charles A. Wood]</p>
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        <p align="center" class="main_titles"><b>Technical Consultant:</b><br>
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            [mailto:anthony@perseus.gr Anthony Ayiomamitis]</p>
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        <p align="center" class="main_titles"><b>[mailto:webmaster@entropysponge.com Contact Webmaster]</b></p>
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        <p align="center" class="main_titles"><b>A service of:</b><br>
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            <a class="one" href="http://www.observingthesky.org/">ObservingTheSky.Org</a></p>
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        <p align="center" class="main_titles"><b>Visit these other PODs:</b> <br>
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          <a class="one" href="http://antwrp.gsfc.nasa.gov/apod/astropix.html">Astronomy</a> | <a class="one" href="http://www.msss.com/">Mars</a> | <a class="one" href="http://epod.usra.edu/">Earth</a></p></td>
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<p>&nbsp;</p>
  
  

Revision as of 15:41, 4 January 2015

Huge Fractures

Huge Fractures

July 22, 2004

[javascript:;" onMouseOver="MM_swapImage('Image1',,'images/LPOD-2004-07-22b.jpeg',1)" onMouseOut="MM_swapImgRestore() <img src="images/LPOD-2004-07-22.jpeg" name="Image1" width="427" height="425" border="0" id="Image1">]</a>

Image Credit: Bob Botts

Huge Fractures

These images are remarkable in showing the tectonic structure southeast of Mare Nectaris. And because Bob Botts took images on successive nights of the waning Moon we can see the same area illuminated and then deeply shadowed. The area SE of Nectaris is well known for its strong and conspicuous radial basin structures. Both the Snellius and Rheita Valleys (black lines on mouseover) are large secondary crater chains caused by mountainous blocks ejected during the formation of the Nectaris impact basin. But Bott's image shows other larger dislocations of the crust also radial to Nectaris. The Oct. 13 view shows a big slab of ground (labeled B for block) that casts a shadow to the north and is bounded on the south by a long, bright line that passes through Brenner. Block B appears to be fault-bounded and higher than the surfaces to its north and south. The previous night's view (remember these are sunset images so the terminator hides land to the east every night) reveals that the low land to the north of block B is partially flat and covered with smooth material. This makes sense, for mare lavas - or other flows - would be expected in lowlands. If block B did move differentially compared to its surroundings then it is one of the largest such blocks on the Moon - except for the truly gigantic circular faults like the Apennines and Altai that define impact basins.

Chuck Wood

Technical Details:
October 12 and 13, 2003. 12" SCT f10 with Toucam webcam, processed using Registax

Related Links:
Lunar Orbiter IV View (notice fault)

Tomorrow's LPOD: Sun, Moon and Stars

<img src="MainPage/spacer.gif" width="640" height="1">


Author & Editor:
Charles A. Wood

Technical Consultant:
Anthony Ayiomamitis

Contact Webmaster

A service of:
<a class="one" href="http://www.observingthesky.org/">ObservingTheSky.Org</a>

Visit these other PODs:
<a class="one" href="http://antwrp.gsfc.nasa.gov/apod/astropix.html">Astronomy</a> | <a class="one" href="http://www.msss.com/">Mars</a> | <a class="one" href="http://epod.usra.edu/">Earth</a>

 



COMMENTS?

Click on this icon File:PostIcon.jpg at the upper right to post a comment.