Difference between revisions of "March 17, 2004"

From LPOD
Jump to: navigation, search
(Created page with "__NOTOC__ =Awesome Pitatus= ---- ===COMMENTS?=== Click on this icon image:PostIcon.jpg at the upper right to post a comment.")
 
 
(10 intermediate revisions by the same user not shown)
Line 1: Line 1:
 
__NOTOC__
 
__NOTOC__
 
=Awesome Pitatus=
 
=Awesome Pitatus=
 
+
<!-- Start of content -->
 
+
<table width="640"  border="0" align="center" cellpadding="6" cellspacing="2">
 
+
<tr>
----
+
</tr>
===COMMENTS?===  
+
</table>
Click on this icon [[image:PostIcon.jpg]] at the upper right to post a comment.
+
<table width="85%"  border="0" align="center" cellpadding="6" cellspacing="2">
 +
<tr>
 +
<td colspan="2"><div align="center">
 +
[[File:LPOD-2004-03-17.gif|LPOD-2004-03-17.gif]]</div>
 +
</td>
 +
</tr>
 +
</table>
 +
<table width="100%"  border="0" cellpadding="8">
 +
<tr>
 +
<td><div align="center"><p>Image Credit:  [mailto:Bruno.DAVERSIN@lahague.com Bruno Daversin]</p></div></td>
 +
</tr>
 +
</table>
 +
<table class="story" border="0" bgcolor="#FFFFFF" width="90%" cellpadding="10" align="center"><tr><td>
 +
<p class="story" align="center"><b>Awesome Pitatus </b></p>
 +
<p class="story" align="left">
 +
Pitatus is one of the under-appreciated gems of the Moon. With a diameter of 97 km it is about the same width as
 +
[[January_24,_2004|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
 +
[[January_15,_2004|Gassendi]] and [[January_9,_2004|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.
 +
</p>
 +
<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>
 +
<p class="story"><b>Related Links:</b><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>
 +
<p><b>Yesterday's LPOD:</b> [[March 16, 2004|Lunar Ephemeris]] </p>
 +
<p><b>Tomorrow's LPOD:</b> [[March 18, 2004|Bull's Eye!]] </p>
 +
</td></tr>
 +
</table>
 +
<!-- start bottom -->
 +
<table width="100%"  border="0" cellspacing="2" cellpadding="4">
 +
<tr>
 +
<td><hr></td>
 +
</tr>
 +
<tr>
 +
<td>
 +
<p align="center" class="main_titles"><b>Author & Editor:</b><br>
 +
[mailto:tychocrater@yahoo.com Charles A. Wood]</p>
 +
<!-- Cleanup of credits -->
 +
<!-- Cleanup of credits -->
 +
<!-- Cleanup of credits -->
 +
<!-- Cleanup of credits -->
 +
<!-- Cleanup of credits -->
 +
<!-- Cleanup of credits -->
 +
<!-- Cleanup of credits -->
 +
</tr>
 +
</table>
 +
<p>&nbsp;</p>
 +
<!-- End of content -->
 +
{{wiki/ArticleFooter}}

Latest revision as of 19:13, 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

 


COMMENTS?

Register, Log in, and join in the comments.