Difference between revisions of "March 17, 2004"

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=Awesome Pitatus=
 
=Awesome Pitatus=
 
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      <td width="50%"><h2 align="left">Awesome Pitatus</h2></td>
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  <td width="50%"><h2 align="right">March 17, 2004</h2></td>
 
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<IMG SRC="images/LPOD-2004-03-17.gif" NAME="main_image" width="435" height="315" border="0"></div>
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[[File:LPOD-2004-03-17.gif|LPOD-2004-03-17.gif]]</div>
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      <td><div align="center" span class="main_sm">Image Credit:  [mailto:Bruno.DAVERSIN@lahague.com Bruno Daversin]</div></td>
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<td><div align="center"><p>Image Credit:  [mailto:Bruno.DAVERSIN@lahague.com Bruno Daversin]</p></div></td>
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<p class="story" align="center"><b>Awesome Pitatus </b></p>
  <p class="story" align="center"><b>Awesome Pitatus </b></p>
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<p class="story" align="left">
 
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Pitatus is one of the under-appreciated gems of the Moon. With a diameter of 97 km it is about the same width as  
  <p class="story" align="left">
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[[January_24,_2004|Plato]] (101 km), but has a much more interesting interior. Presumably Pitatus  
          Pitatus is one of the under-appreciated gems of the Moon. With a diameter of 97 km it is about the same width as  
+
was a Copernicus style crater when formed, with magnificent concentric wall terraces and a large central peak.  
        [../01/LPOD-2004-01-24.htm Plato] (101 km), but has a much more interesting interior. Presumably Pitatus  
+
Today the crater's rim is heavily battered by later impacts, the terraces are mush, the central peak is still  
        was a Copernicus style crater when formed, with magnificent concentric wall terraces and a large central peak.  
+
there, and the floor is filled with mare lavas. What this extraordinary image shows is that Pitatus has an  
        Today the crater's rim is heavily battered by later impacts, the terraces are mush, the central peak is still  
+
amazing system of rilles that hug the edges of the floor, with some fainter ones crossing it. In two places - the  
        there, and the floor is filled with mare lavas. What this extraordinary image shows is that Pitatus has an  
+
upper left (west) and the middle right (east) - the rille looks like the mare material it formed on was domed up,  
        amazing system of rilles that hug the edges of the floor, with some fainter ones crossing it. In two places - the  
+
like a crack on the crust of home baked bread. Pitatus is another example of a floor-fractured crater - like  
        upper left (west) and the middle right (east) - the rille looks like the mare material it formed on was domed up,  
+
[[January_15,_2004|Gassendi]] and [[January_9,_2004|Posidonius]] but its rilles  
        like a crack on the crust of home baked bread. Pitatus is another example of a floor-fractured crater - like  
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are more concentrated around the floor edges. FFCs are thought to result from a magma intrusion that lifted the  
        [../01/LPOD-2004-01-15.htm Gassendi] and [../01/LPOD-2004-01-09.htm Posidonius] but its rilles  
+
entire floor (hence the high - 480 m - central peak) and perhaps domed it, producing the tension craters around  
        are more concentrated around the floor edges. FFCs are thought to result from a magma intrusion that lifted the  
+
the edges.
        entire floor (hence the high - 480 m - central peak) and perhaps domed it, producing the tension craters around  
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</p>
        the edges.
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<p><b>Technical Details:</b><br>
</p>
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Image obtained with Ludiver Observatory (Normandy, France) 600 mm (24") F/D=16 cassegrain telescope + infrared filter + TouCam Pro in B&W mode.<br>
 
 
  <p><b>Technical Details:</b><br>
 
 
 
  Image obtained with Ludiver Observatory (Normandy, France) 600 mm (24") F/D=16 cassegrain telescope + infrared filter + TouCam Pro in B&W mode.<br>
 
 
[http://www.lpi.usra.edu/research/cla/info/fiv/ Pitatus area at full Moon] </p>
 
[http://www.lpi.usra.edu/research/cla/info/fiv/ Pitatus area at full Moon] </p>
 
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<p class="story"><b>Related Links:</b><br>
  <p class"story"><b>Related Links:</b><br>
 
 
 
 
[http://www.ludiver.com/conquerir_espace_scientifique_lune.php Ludiver Planetarium & Observatory]<br>
 
[http://www.ludiver.com/conquerir_espace_scientifique_lune.php Ludiver Planetarium & Observatory]<br>
 
[http://www.lpi.usra.edu/research/cla/info/fiv/ Pitatus area at full Moon]</p>
 
[http://www.lpi.usra.edu/research/cla/info/fiv/ Pitatus area at full Moon]</p>
 
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<p><b>Yesterday's LPOD:</b> [[March 16, 2004|Lunar Ephemeris]] </p>
  <p class"story"> <b>Tomorrow's LPOD:</b> Bull's Eye!</p>
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<p><b>Tomorrow's LPOD:</b> [[March 18, 2004|Bull's Eye!]] </p>
 
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<p align="center" class="main_titles"><b>Author & Editor:</b><br>
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[mailto:tychocrater@yahoo.com Charles A. Wood]</p>
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  <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>
 
      <p align="center" class="main_titles"><b>[mailto:webmaster@entropysponge.com Contact Webmaster]</b></p>
 
      <p align="center" class="main_titles"><b>A service of:</b><br>
 
      <a class="one" href="http://www.observingthesky.org/">ObservingTheSky.Org</a></p>
 
      <p align="center" class="main_titles"><b>Visit these other PODs:</b> <br>
 
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Latest revision as of 18:13, 7 February 2015

Awesome Pitatus

LPOD-2004-03-17.gif

Image Credit: Bruno Daversin

Awesome Pitatus

Pitatus is one of the under-appreciated gems of the Moon. With a diameter of 97 km it is about the same width as Plato (101 km), but has a much more interesting interior. Presumably Pitatus was a Copernicus style crater when formed, with magnificent concentric wall terraces and a large central peak. Today the crater's rim is heavily battered by later impacts, the terraces are mush, the central peak is still there, and the floor is filled with mare lavas. What this extraordinary image shows is that Pitatus has an amazing system of rilles that hug the edges of the floor, with some fainter ones crossing it. In two places - the upper left (west) and the middle right (east) - the rille looks like the mare material it formed on was domed up, like a crack on the crust of home baked bread. Pitatus is another example of a floor-fractured crater - like Gassendi and Posidonius but its rilles are more concentrated around the floor edges. FFCs are thought to result from a magma intrusion that lifted the entire floor (hence the high - 480 m - central peak) and perhaps domed it, producing the tension craters around the edges.

Technical Details:
Image obtained with Ludiver Observatory (Normandy, France) 600 mm (24") F/D=16 cassegrain telescope + infrared filter + TouCam Pro in B&W mode.
Pitatus area at full Moon

Related Links:
Ludiver Planetarium & Observatory
Pitatus area at full Moon

Yesterday's LPOD: Lunar Ephemeris

Tomorrow's LPOD: Bull's Eye!


Author & Editor:
Charles A. Wood

 


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