Difference between revisions of "February 1, 2004"

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<table width="640"  border="0" align="center" cellpadding="6" cellspacing="2">
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      <td width="50%"><h2 align="left">Theophilus</h2></td>
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  <td width="50%"><h2 align="right">February 1, 2004</h2></td>
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<table width="640"  border="0" align="center" cellpadding="6" cellspacing="2">
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      <td colspan="2"><div align="center">
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<IMG SRC="images/LPOD-2004-02-01.jpeg" NAME="main_image" width="427" height="400" border="0"></div>
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<table width="100%"  border="0" cellpadding="8">
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      <td><div align="center" span class="main_sm">Image Credit:  <A class="one" HREF="http://www.hq.nasa.gov/office/pao/History/SP-362/ch5.5.htm">Apollo 16 (AS16-0692)</A></div></td>
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<table class="story" border="0" bgcolor="#FFFFFF" width="90%" cellpadding="10" align="center"><tr><td>
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  <p class="story" align="center"><b>Theophilus </b></p>
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  <p class="story" align="left">If Copernicus is the king of lunar craters, Theophilus is at least a duke, if not a prince. Theophilus is a 100 km wide,
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4.4 km deep complex impact crater. This oblique Apollo 16 view clearly shows the trademark features of a complex crater:
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terraced walls, flat floor, and massive central peaks. Because its secondary craters and rays are less well preserved
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than those at Copernicus, Theophilus must be older. Don Wilhelms, a retired US Geologic Survey lunar expert, has
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classified Theophilus as Erastothenian in relative age - that is, somewhere between 1.1 and 3.2 billion years old. Its
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faint rays - can you see them at full Moon? - suggest that Theophilus is at the young end of that range. Finally, note
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the two dark halo craters to the middle left. These appear to be normal small impact pits that have excavated buried mare
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material from under the bright ejecta of Theophilus.  </p>
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  <p class"story"><b>Related Links:</b><br>
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  [http://www.hq.nasa.gov/office/pao/History/SP-362/contents.htm Apollo Over the Moon: The View from Orbit (NASA SP-362)]<br> 
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  [http://www.lpi.usra.edu/research/lunar_orbiter/images/img/iv_077_h2.jpg Lunar Orbiter view]</p>
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  <p class"story"> <b>Tomorrow's LPOD:</b> Brightness at Noon</p>
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  <p><img src="../../../MainPage/spacer.gif" width="640" height="1"></p>
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  </td></tr>
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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>
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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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      </tr>
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</table>
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<p>&nbsp;</p>
  
  

Revision as of 15:34, 4 January 2015

Theophilus

Theophilus

February 1, 2004

<IMG SRC="images/LPOD-2004-02-01.jpeg" NAME="main_image" width="427" height="400" border="0">
Image Credit: <A class="one" HREF="http://www.hq.nasa.gov/office/pao/History/SP-362/ch5.5.htm">Apollo 16 (AS16-0692)</A>

Theophilus

If Copernicus is the king of lunar craters, Theophilus is at least a duke, if not a prince. Theophilus is a 100 km wide, 4.4 km deep complex impact crater. This oblique Apollo 16 view clearly shows the trademark features of a complex crater: terraced walls, flat floor, and massive central peaks. Because its secondary craters and rays are less well preserved than those at Copernicus, Theophilus must be older. Don Wilhelms, a retired US Geologic Survey lunar expert, has classified Theophilus as Erastothenian in relative age - that is, somewhere between 1.1 and 3.2 billion years old. Its faint rays - can you see them at full Moon? - suggest that Theophilus is at the young end of that range. Finally, note the two dark halo craters to the middle left. These appear to be normal small impact pits that have excavated buried mare material from under the bright ejecta of Theophilus.

Related Links:
Apollo Over the Moon: The View from Orbit (NASA SP-362)
Lunar Orbiter view

Tomorrow's LPOD: Brightness at Noon

<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.