http://the-moon.us/index.php?title=Compton&feed=atom&action=history
Compton - Revision history
2024-03-28T16:03:18Z
Revision history for this page on the wiki
MediaWiki 1.31.1
http://the-moon.us/index.php?title=Compton&diff=17441&oldid=prev
Api at 04:08, 17 April 2018
2018-04-17T04:08:23Z
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 04:08, 17 April 2018</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l40" >Line 40:</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Additional Information==</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Additional Information==</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>* From the shadows in [http://www.lpi.usra.edu/resources/lunarorbiter/frame/?5181 LO-V-181M], the central peaks of '''Compton''' rise about 2700 m above the floor. The crater appears to be somewhat deeper, but the shadows are not suitable for a measurement of its depth. <span class="membersnap">- <del class="diffchange diffchange-inline">Jim Mosher</del></span></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* From the shadows in [http://www.lpi.usra.edu/resources/lunarorbiter/frame/?5181 LO-V-181M], the central peaks of '''Compton''' rise about 2700 m above the floor. The crater appears to be somewhat deeper, but the shadows are not suitable for a measurement of its depth. <span class="membersnap">- <ins class="diffchange diffchange-inline">JimMosher</ins></span></div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>* Frame '''2700r''' from the [http://pds-imaging.jpl.nasa.gov/Missions/Galileo_mission.html Galileo] fly-by of the Moon shows the western part of '''Compton''' with a low [http://the-moon.us/wiki/sun%20angle sun angle] from the west. The shadows falling on the floor indicate a considerable variation in the height of the western rim, ranging from about 1300 m in north to 4100 m in south, with a typical value of about 3200 m near the middle. <span class="membersnap">- <del class="diffchange diffchange-inline">Jim Mosher</del></span></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* Frame '''2700r''' from the [http://pds-imaging.jpl.nasa.gov/Missions/Galileo_mission.html Galileo] fly-by of the Moon shows the western part of '''Compton''' with a low [http://the-moon.us/wiki/sun%20angle sun angle] from the west. The shadows falling on the floor indicate a considerable variation in the height of the western rim, ranging from about 1300 m in north to 4100 m in south, with a typical value of about 3200 m near the middle. <span class="membersnap">- <ins class="diffchange diffchange-inline">JimMosher</ins></span></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Three small pyroclastic deposits (area = 24, 45 & 5 km^2). Gaddis, L. (1999) [http://astrogeology.usgs.gov/Projects/LunarPyroclasticVolcanism/lunpyroWebDb.html Lunar Pyroclastic Volcanism Project].</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Three small pyroclastic deposits (area = 24, 45 & 5 km^2). Gaddis, L. (1999) [http://astrogeology.usgs.gov/Projects/LunarPyroclasticVolcanism/lunpyroWebDb.html Lunar Pyroclastic Volcanism Project].</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Four dark halo/pyroclastic deposits located on floor fractures; three are 2-6 km in diameter, the others is ~15 km wide. [http://www.lpi.usra.edu/meetings/LPSC98/pdf/1710.pdf Rosanova et al, 1998]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Four dark halo/pyroclastic deposits located on floor fractures; three are 2-6 km in diameter, the others is ~15 km wide. [http://www.lpi.usra.edu/meetings/LPSC98/pdf/1710.pdf Rosanova et al, 1998]</div></td></tr>
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Api
http://the-moon.us/index.php?title=Compton&diff=15600&oldid=prev
Api at 09:45, 16 April 2018
2018-04-16T09:45:11Z
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 09:45, 16 April 2018</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l6" >Line 6:</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Lat: 55.3°N, Long: 103.8°E, Main ring diam: 175 km, Depth: 3.2 km, Rükl: ''(farside)'', [http://the-moon.us/wiki/Stratigraphy Lower Imbrian]<br /></div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Lat: 55.3°N, Long: 103.8°E, Main ring diam: 175 km, Depth: 3.2 km, Rükl: ''(farside)'', [http://the-moon.us/wiki/Stratigraphy Lower Imbrian]<br /></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[http://www.lpod.org/coppermine/albums/userpics/Compton_LO-V-181M_LTVT.JPG [[Image:<del class="diffchange diffchange-inline">normal_Compton_LO</del>-V-181M_LTVT.JPG|external image normal_Compton_LO-V-181M_LTVT.JPG]]][http://www.lpod.org/coppermine/albums/userpics/Compton_Basin_LIDAR_LTVT.JPG [[Image:<del class="diffchange diffchange-inline">normal_Compton_Basin_LIDAR_LTVT</del>.JPG|external image normal_Compton_Basin_LIDAR_LTVT.JPG]]]<br /> '''Left:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-4137 LO-V-181M]''<br /> '''Right:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-2318 Clementine]'', Clementine LIDAR Altimeter texture from [http://pdsmaps.wr.usgs.gov/PDS/public/explorer/html/lidrlvls.htm PDS Map-a-Planet] remapped to north-up aerial view by [http://www.henriksucla.dk/ LTVT]. The dot is the center position and the white circle the main ring position from Chuck Wood's [http://www.lpod.org/cwm/DataStuff/Lunar%20Basins.htm Impact Basin Database]. Grid spacing = 10 degrees.<br /> <div id="toc"></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[http://www.lpod.org/coppermine/albums/userpics/Compton_LO-V-181M_LTVT.JPG [[Image:<ins class="diffchange diffchange-inline">Normal_Compton_LO</ins>-V-181M_LTVT.JPG|external image normal_Compton_LO-V-181M_LTVT.JPG]]][http://www.lpod.org/coppermine/albums/userpics/Compton_Basin_LIDAR_LTVT.JPG [[Image:<ins class="diffchange diffchange-inline">Normal_Compton_Basin_LIDAR_LTVT</ins>.JPG|external image normal_Compton_Basin_LIDAR_LTVT.JPG]]]<br /> '''Left:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-4137 LO-V-181M]''<br /> '''Right:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-2318 Clementine]'', Clementine LIDAR Altimeter texture from [http://pdsmaps.wr.usgs.gov/PDS/public/explorer/html/lidrlvls.htm PDS Map-a-Planet] remapped to north-up aerial view by [http://www.henriksucla.dk/ LTVT]. The dot is the center position and the white circle the main ring position from Chuck Wood's [http://www.lpod.org/cwm/DataStuff/Lunar%20Basins.htm Impact Basin Database]. Grid spacing = 10 degrees.<br /> <div id="toc"></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Images==</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Images==</div></td></tr>
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Api
http://the-moon.us/index.php?title=Compton&diff=10826&oldid=prev
Api at 00:18, 16 April 2018
2018-04-16T00:18:35Z
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 00:18, 16 April 2018</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l7" >Line 7:</td>
<td colspan="2" class="diff-lineno">Line 7:</td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[http://www.lpod.org/coppermine/albums/userpics/Compton_LO-V-181M_LTVT.JPG [[Image:normal_Compton_LO-V-181M_LTVT.JPG|external image normal_Compton_LO-V-181M_LTVT.JPG]]][http://www.lpod.org/coppermine/albums/userpics/Compton_Basin_LIDAR_LTVT.JPG [[Image:normal_Compton_Basin_LIDAR_LTVT.JPG|external image normal_Compton_Basin_LIDAR_LTVT.JPG]]]<br /> '''Left:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-4137 LO-V-181M]''<br /> '''Right:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-2318 Clementine]'', Clementine LIDAR Altimeter texture from [http://pdsmaps.wr.usgs.gov/PDS/public/explorer/html/lidrlvls.htm PDS Map-a-Planet] remapped to north-up aerial view by [http://www.henriksucla.dk/ LTVT]. The dot is the center position and the white circle the main ring position from Chuck Wood's [http://www.lpod.org/cwm/DataStuff/Lunar%20Basins.htm Impact Basin Database]. Grid spacing = 10 degrees.<br /> <div id="toc"></div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[http://www.lpod.org/coppermine/albums/userpics/Compton_LO-V-181M_LTVT.JPG [[Image:normal_Compton_LO-V-181M_LTVT.JPG|external image normal_Compton_LO-V-181M_LTVT.JPG]]][http://www.lpod.org/coppermine/albums/userpics/Compton_Basin_LIDAR_LTVT.JPG [[Image:normal_Compton_Basin_LIDAR_LTVT.JPG|external image normal_Compton_Basin_LIDAR_LTVT.JPG]]]<br /> '''Left:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-4137 LO-V-181M]''<br /> '''Right:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-2318 Clementine]'', Clementine LIDAR Altimeter texture from [http://pdsmaps.wr.usgs.gov/PDS/public/explorer/html/lidrlvls.htm PDS Map-a-Planet] remapped to north-up aerial view by [http://www.henriksucla.dk/ LTVT]. The dot is the center position and the white circle the main ring position from Chuck Wood's [http://www.lpod.org/cwm/DataStuff/Lunar%20Basins.htm Impact Basin Database]. Grid spacing = 10 degrees.<br /> <div id="toc"></div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del class="diffchange diffchange-inline">=Table of Contents=</del></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div> </div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del class="diffchange diffchange-inline"><div style="margin-left: 1em">[#Compton Basin Compton Basin]</div><div style="margin-left: 2em">[#Compton Basin-Images Images]</div><div style="margin-left: 2em">[#Compton Basin-Maps Maps]</div><div style="margin-left: 2em">[#Compton Basin-Basin Classification Basin Classification]</div><div style="margin-left: 2em">[#Compton Basin-Description Description]</div><div style="margin-left: 3em">[#Compton Basin-Description-Wikipedia Wikipedia]</div><div style="margin-left: 2em">[#Compton Basin-Additional Information Additional Information]</div><div style="margin-left: 2em">[#Compton Basin-Weird stratification at Compton's floor Weird stratification at Compton's floor]</div><div style="margin-left: 2em">[#Compton Basin-Nomenclature Nomenclature]</div><div style="margin-left: 2em">[#Compton Basin-LPOD Articles LPOD Articles]</div><div style="margin-left: 2em">[#Compton Basin-Bibliography Bibliography]</div></div></del></div></td><td colspan="2"> </td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Images==</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Images==</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[http://www.lpod.org/coppermine/thumbnails.php?album=search&type=full&search=Compton LPOD Photo Gallery] [http://www.lpi.usra.edu/resources/lunar_orbiter/bin/srch_nam.shtml?Compton%7C0 Lunar Orbiter Images]<br />  </div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[http://www.lpod.org/coppermine/thumbnails.php?album=search&type=full&search=Compton LPOD Photo Gallery] [http://www.lpi.usra.edu/resources/lunar_orbiter/bin/srch_nam.shtml?Compton%7C0 Lunar Orbiter Images]<br />  </div></td></tr>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Additional Information==</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Additional Information==</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>* From the shadows in [http://www.lpi.usra.edu/resources/lunarorbiter/frame/?5181 LO-V-181M], the central peaks of '''Compton''' rise about 2700 m above the floor. The crater appears to be somewhat deeper, but the shadows are not suitable for a measurement of its depth. <span class="membersnap">- <del class="diffchange diffchange-inline">[http://www.wikispaces.com/user/view/JimMosher [[Image:JimMosher-lg.jpg|16px|JimMosher]]] [http://www.wikispaces.com/user/view/JimMosher JimMosher]</del></span></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* From the shadows in [http://www.lpi.usra.edu/resources/lunarorbiter/frame/?5181 LO-V-181M], the central peaks of '''Compton''' rise about 2700 m above the floor. The crater appears to be somewhat deeper, but the shadows are not suitable for a measurement of its depth. <span class="membersnap">- <ins class="diffchange diffchange-inline">Jim Mosher</ins></span></div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>* Frame '''2700r''' from the [http://pds-imaging.jpl.nasa.gov/Missions/Galileo_mission.html Galileo] fly-by of the Moon shows the western part of '''Compton''' with a low [http://the-moon.us/wiki/sun%20angle sun angle] from the west. The shadows falling on the floor indicate a considerable variation in the height of the western rim, ranging from about 1300 m in north to 4100 m in south, with a typical value of about 3200 m near the middle. <span class="membersnap">- <del class="diffchange diffchange-inline">[http://www.wikispaces.com/user/view/JimMosher [[Image:JimMosher-lg.jpg|16px|JimMosher]]] [http://www.wikispaces.com/user/view/JimMosher JimMosher]</del></span></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* Frame '''2700r''' from the [http://pds-imaging.jpl.nasa.gov/Missions/Galileo_mission.html Galileo] fly-by of the Moon shows the western part of '''Compton''' with a low [http://the-moon.us/wiki/sun%20angle sun angle] from the west. The shadows falling on the floor indicate a considerable variation in the height of the western rim, ranging from about 1300 m in north to 4100 m in south, with a typical value of about 3200 m near the middle. <span class="membersnap">- <ins class="diffchange diffchange-inline">Jim Mosher</ins></span></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Three small pyroclastic deposits (area = 24, 45 & 5 km^2). Gaddis, L. (1999) [http://astrogeology.usgs.gov/Projects/LunarPyroclasticVolcanism/lunpyroWebDb.html Lunar Pyroclastic Volcanism Project].</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Three small pyroclastic deposits (area = 24, 45 & 5 km^2). Gaddis, L. (1999) [http://astrogeology.usgs.gov/Projects/LunarPyroclasticVolcanism/lunpyroWebDb.html Lunar Pyroclastic Volcanism Project].</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Four dark halo/pyroclastic deposits located on floor fractures; three are 2-6 km in diameter, the others is ~15 km wide. [http://www.lpi.usra.edu/meetings/LPSC98/pdf/1710.pdf Rosanova et al, 1998]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Four dark halo/pyroclastic deposits located on floor fractures; three are 2-6 km in diameter, the others is ~15 km wide. [http://www.lpi.usra.edu/meetings/LPSC98/pdf/1710.pdf Rosanova et al, 1998]</div></td></tr>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>----</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>----</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>  <del class="diffchange diffchange-inline">This page has been edited 1 times. The last modification was made by <span class="membersnap">- [http://www.wikispaces.com/user/view/tychocrater [[Image:tychocrater-lg.jpg|16px|tychocrater]]] [http://www.wikispaces.com/user/view/tychocrater tychocrater]</span> on Jun 13, 2009 3:24 pm - ''afx3u3''</del></div></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>  </div></div></td></tr>
</table>
Api
http://the-moon.us/index.php?title=Compton&diff=6174&oldid=prev
Api at 03:12, 12 April 2018
2018-04-12T03:12:01Z
<p></p>
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 03:12, 12 April 2018</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l4" >Line 4:</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wiki_table"</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wiki_table"</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Lat: 55.3°N, Long: 103.8°E, Main ring diam: 175 km, Depth: 3.2 km, Rükl: ''(farside)'', [http://the-moon.<del class="diffchange diffchange-inline">wikispaces.com</del>/Stratigraphy Lower Imbrian]<br /></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Lat: 55.3°N, Long: 103.8°E, Main ring diam: 175 km, Depth: 3.2 km, Rükl: ''(farside)'', [http://the-moon.<ins class="diffchange diffchange-inline">us/wiki</ins>/Stratigraphy Lower Imbrian]<br /></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|}</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[http://www.lpod.org/coppermine/albums/userpics/Compton_LO-V-181M_LTVT.JPG [[Image:normal_Compton_LO-V-181M_LTVT.JPG|external image normal_Compton_LO-V-181M_LTVT.JPG]]][http://www.lpod.org/coppermine/albums/userpics/Compton_Basin_LIDAR_LTVT.JPG [[Image:normal_Compton_Basin_LIDAR_LTVT.JPG|external image normal_Compton_Basin_LIDAR_LTVT.JPG]]]<br /> '''Left:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-4137 LO-V-181M]''<br /> '''Right:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-2318 Clementine]'', Clementine LIDAR Altimeter texture from [http://pdsmaps.wr.usgs.gov/PDS/public/explorer/html/lidrlvls.htm PDS Map-a-Planet] remapped to north-up aerial view by [http://www.henriksucla.dk/ LTVT]. The dot is the center position and the white circle the main ring position from Chuck Wood's [http://www.lpod.org/cwm/DataStuff/Lunar%20Basins.htm Impact Basin Database]. Grid spacing = 10 degrees.<br /> <div id="toc"></div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[http://www.lpod.org/coppermine/albums/userpics/Compton_LO-V-181M_LTVT.JPG [[Image:normal_Compton_LO-V-181M_LTVT.JPG|external image normal_Compton_LO-V-181M_LTVT.JPG]]][http://www.lpod.org/coppermine/albums/userpics/Compton_Basin_LIDAR_LTVT.JPG [[Image:normal_Compton_Basin_LIDAR_LTVT.JPG|external image normal_Compton_Basin_LIDAR_LTVT.JPG]]]<br /> '''Left:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-4137 LO-V-181M]''<br /> '''Right:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-2318 Clementine]'', Clementine LIDAR Altimeter texture from [http://pdsmaps.wr.usgs.gov/PDS/public/explorer/html/lidrlvls.htm PDS Map-a-Planet] remapped to north-up aerial view by [http://www.henriksucla.dk/ LTVT]. The dot is the center position and the white circle the main ring position from Chuck Wood's [http://www.lpod.org/cwm/DataStuff/Lunar%20Basins.htm Impact Basin Database]. Grid spacing = 10 degrees.<br /> <div id="toc"></div></td></tr>
<tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l16" >Line 16:</td>
<td colspan="2" class="diff-lineno">Line 16:</td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><br />  </div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><br />  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Maps==</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Maps==</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>''([http://the-moon.<del class="diffchange diffchange-inline">wikispaces.com</del>/LAC%20zone LAC zone] 16D1)'' [http://planetarynames.wr.usgs.gov/images/Lunar/lac_16.pdf USGS Digital Atlas PDF]<br /> <br />  </div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>''([http://the-moon.<ins class="diffchange diffchange-inline">us/wiki</ins>/LAC%20zone LAC zone] 16D1)'' [http://planetarynames.wr.usgs.gov/images/Lunar/lac_16.pdf USGS Digital Atlas PDF]<br /> <br />  </div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>==[http://the-moon.<del class="diffchange diffchange-inline">wikispaces.com</del>/Lunar%20Basins Basin Classification]==</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>==[http://the-moon.<ins class="diffchange diffchange-inline">us/wiki</ins>/Lunar%20Basins Basin Classification]==</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>  (description of terms and most numeric basin data from Wood, C.A. (2004) [http://www.lpod.org/cwm/DataStuff/Lunar%20Basins.htm Impact Basin Database])<br />  </div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>  (description of terms and most numeric basin data from Wood, C.A. (2004) [http://www.lpod.org/cwm/DataStuff/Lunar%20Basins.htm Impact Basin Database])<br />  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wiki_table"</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| class="wiki_table"</div></td></tr>
<tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l42" >Line 42:</td>
<td colspan="2" class="diff-lineno">Line 42:</td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* From the shadows in [http://www.lpi.usra.edu/resources/lunarorbiter/frame/?5181 LO-V-181M], the central peaks of '''Compton''' rise about 2700 m above the floor. The crater appears to be somewhat deeper, but the shadows are not suitable for a measurement of its depth. <span class="membersnap">- [http://www.wikispaces.com/user/view/JimMosher [[Image:JimMosher-lg.jpg|16px|JimMosher]]] [http://www.wikispaces.com/user/view/JimMosher JimMosher]</span></div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* From the shadows in [http://www.lpi.usra.edu/resources/lunarorbiter/frame/?5181 LO-V-181M], the central peaks of '''Compton''' rise about 2700 m above the floor. The crater appears to be somewhat deeper, but the shadows are not suitable for a measurement of its depth. <span class="membersnap">- [http://www.wikispaces.com/user/view/JimMosher [[Image:JimMosher-lg.jpg|16px|JimMosher]]] [http://www.wikispaces.com/user/view/JimMosher JimMosher]</span></div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>* Frame '''2700r''' from the [http://pds-imaging.jpl.nasa.gov/Missions/Galileo_mission.html Galileo] fly-by of the Moon shows the western part of '''Compton''' with a low [http://the-moon.<del class="diffchange diffchange-inline">wikispaces.com</del>/sun%20angle sun angle] from the west. The shadows falling on the floor indicate a considerable variation in the height of the western rim, ranging from about 1300 m in north to 4100 m in south, with a typical value of about 3200 m near the middle. <span class="membersnap">- [http://www.wikispaces.com/user/view/JimMosher [[Image:JimMosher-lg.jpg|16px|JimMosher]]] [http://www.wikispaces.com/user/view/JimMosher JimMosher]</span></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* Frame '''2700r''' from the [http://pds-imaging.jpl.nasa.gov/Missions/Galileo_mission.html Galileo] fly-by of the Moon shows the western part of '''Compton''' with a low [http://the-moon.<ins class="diffchange diffchange-inline">us/wiki</ins>/sun%20angle sun angle] from the west. The shadows falling on the floor indicate a considerable variation in the height of the western rim, ranging from about 1300 m in north to 4100 m in south, with a typical value of about 3200 m near the middle. <span class="membersnap">- [http://www.wikispaces.com/user/view/JimMosher [[Image:JimMosher-lg.jpg|16px|JimMosher]]] [http://www.wikispaces.com/user/view/JimMosher JimMosher]</span></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Three small pyroclastic deposits (area = 24, 45 & 5 km^2). Gaddis, L. (1999) [http://astrogeology.usgs.gov/Projects/LunarPyroclasticVolcanism/lunpyroWebDb.html Lunar Pyroclastic Volcanism Project].</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Three small pyroclastic deposits (area = 24, 45 & 5 km^2). Gaddis, L. (1999) [http://astrogeology.usgs.gov/Projects/LunarPyroclasticVolcanism/lunpyroWebDb.html Lunar Pyroclastic Volcanism Project].</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Four dark halo/pyroclastic deposits located on floor fractures; three are 2-6 km in diameter, the others is ~15 km wide. [http://www.lpi.usra.edu/meetings/LPSC98/pdf/1710.pdf Rosanova et al, 1998]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Four dark halo/pyroclastic deposits located on floor fractures; three are 2-6 km in diameter, the others is ~15 km wide. [http://www.lpi.usra.edu/meetings/LPSC98/pdf/1710.pdf Rosanova et al, 1998]</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>* Inner mare patches [http://the-moon.<del class="diffchange diffchange-inline">wikispaces.com</del>/Stratigraphy Imbrian] age and 4-4.5 wt% FeO content. Younger maria around outer edges ([http://the-moon.<del class="diffchange diffchange-inline">wikispaces.com</del>/Gillis%20and%20Spudis%2C%201996 Gillis and Spudis, 1996]).</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* Inner mare patches [http://the-moon.<ins class="diffchange diffchange-inline">us/wiki</ins>/Stratigraphy Imbrian] age and 4-4.5 wt% FeO content. Younger maria around outer edges ([http://the-moon.<ins class="diffchange diffchange-inline">us/wiki</ins>/Gillis%20and%20Spudis%2C%201996 Gillis and Spudis, 1996]).</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* First described as a basin by Hartmann & Wood (1971).</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* First described as a basin by Hartmann & Wood (1971).</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>* At favorable [http://the-moon.<del class="diffchange diffchange-inline">wikispaces.com</del>/librations librations], '''Compton''' can be seen straddling the limb, but it does not seem to have been recognized in Earth-based observations.</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* At favorable [http://the-moon.<ins class="diffchange diffchange-inline">us/wiki</ins>/librations librations], '''Compton''' can be seen straddling the limb, but it does not seem to have been recognized in Earth-based observations.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Telescopic observers of the moon might look for the central peaks of '''Compton''', which are visible during favourable libration! See LPOD [http://lpod.wikispaces.com/June%2011%2C%202009 Peaking over the Limb] and discussions.</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* Telescopic observers of the moon might look for the central peaks of '''Compton''', which are visible during favourable libration! See LPOD [http://lpod.wikispaces.com/June%2011%2C%202009 Peaking over the Limb] and discussions.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><br />  </div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><br />  </div></td></tr>
<tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l60" >Line 60:</td>
<td colspan="2" class="diff-lineno">Line 60:</td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>** [http://en.wikipedia.org/wiki/Karl_Taylor_Compton Karl Taylor Compton] (September 14, 1887 – June 22, 1954) was a prominent American physicist and president of the Massachusetts Institute of Technology (MIT) from 1930 to 1948.</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>** [http://en.wikipedia.org/wiki/Karl_Taylor_Compton Karl Taylor Compton] (September 14, 1887 – June 22, 1954) was a prominent American physicist and president of the Massachusetts Institute of Technology (MIT) from 1930 to 1948.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* The impact basin was named after the crater.</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* The impact basin was named after the crater.</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>* '''Compton''' was among the long list of farside names added to the [http://the-moon.<del class="diffchange diffchange-inline">wikispaces.com</del>/IAU%20nomenclature IAU nomenclature] in [http://the-moon.<del class="diffchange diffchange-inline">wikispaces.com</del>/Menzel%2C%201971 Menzel, 1971].</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* '''Compton''' was among the long list of farside names added to the [http://the-moon.<ins class="diffchange diffchange-inline">us/wiki</ins>/IAU%20nomenclature IAU nomenclature] in [http://the-moon.<ins class="diffchange diffchange-inline">us/wiki</ins>/Menzel%2C%201971 Menzel, 1971].</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* '''''Rimae Compton''''' (an unofficial name from D.Caes for the system of rilles on the floor of '''Compton''').</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* '''''Rimae Compton''''' (an unofficial name from D.Caes for the system of rilles on the floor of '''Compton''').</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><br />  </div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><br />  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==LPOD Articles==</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==LPOD Articles==</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>* [http://<del class="diffchange diffchange-inline">www</del>.lpod.org/<del class="diffchange diffchange-inline">?m=20070225 </del>Peak Rings]</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* [http://<ins class="diffchange diffchange-inline">www2</ins>.lpod.org/<ins class="diffchange diffchange-inline">wiki/February_25,_2007 </ins>Peak Rings]</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [http://lpod.wikispaces.com/June%2011%2C%202009 Peaking over the Limb] (terrestrial photograph of '''Compton''''s central peak).</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [http://lpod.wikispaces.com/June%2011%2C%202009 Peaking over the Limb] (terrestrial photograph of '''Compton''''s central peak).</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><br />  </div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><br />  </div></td></tr>
</table>
Api
http://the-moon.us/index.php?title=Compton&diff=496&oldid=prev
Api: Created page with "<div id="content_view" class="wiki" style="display: block"> =Compton Basin= ''(unofficial name; IAU crater name: '''Compton'''; 162 km diam)''<br /> {| class="wiki_table"..."
2018-04-11T03:44:13Z
<p>Created page with "<div id="content_view" class="wiki" style="display: block"> =Compton Basin= ''(unofficial name; IAU crater name: '''Compton'''; 162 km diam)''<br /> {| class="wiki_table"..."</p>
<p><b>New page</b></p><div><div id="content_view" class="wiki" style="display: block"><br />
=Compton Basin=<br />
''(unofficial name; IAU crater name: '''Compton'''; 162 km diam)''<br /> <br />
{| class="wiki_table"<br />
|<br />
Lat: 55.3°N, Long: 103.8°E, Main ring diam: 175 km, Depth: 3.2 km, Rükl: ''(farside)'', [http://the-moon.wikispaces.com/Stratigraphy Lower Imbrian]<br /><br />
|}<br />
[http://www.lpod.org/coppermine/albums/userpics/Compton_LO-V-181M_LTVT.JPG [[Image:normal_Compton_LO-V-181M_LTVT.JPG|external image normal_Compton_LO-V-181M_LTVT.JPG]]][http://www.lpod.org/coppermine/albums/userpics/Compton_Basin_LIDAR_LTVT.JPG [[Image:normal_Compton_Basin_LIDAR_LTVT.JPG|external image normal_Compton_Basin_LIDAR_LTVT.JPG]]]<br /> '''Left:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-4137 LO-V-181M]''<br /> '''Right:''' ''[http://lpod.org/coppermine/displayimage.php?pos=-2318 Clementine]'', Clementine LIDAR Altimeter texture from [http://pdsmaps.wr.usgs.gov/PDS/public/explorer/html/lidrlvls.htm PDS Map-a-Planet] remapped to north-up aerial view by [http://www.henriksucla.dk/ LTVT]. The dot is the center position and the white circle the main ring position from Chuck Wood's [http://www.lpod.org/cwm/DataStuff/Lunar%20Basins.htm Impact Basin Database]. Grid spacing = 10 degrees.<br /> <div id="toc"><br />
=Table of Contents=<br />
<div style="margin-left: 1em">[#Compton Basin Compton Basin]</div><div style="margin-left: 2em">[#Compton Basin-Images Images]</div><div style="margin-left: 2em">[#Compton Basin-Maps Maps]</div><div style="margin-left: 2em">[#Compton Basin-Basin Classification Basin Classification]</div><div style="margin-left: 2em">[#Compton Basin-Description Description]</div><div style="margin-left: 3em">[#Compton Basin-Description-Wikipedia Wikipedia]</div><div style="margin-left: 2em">[#Compton Basin-Additional Information Additional Information]</div><div style="margin-left: 2em">[#Compton Basin-Weird stratification at Compton's floor Weird stratification at Compton's floor]</div><div style="margin-left: 2em">[#Compton Basin-Nomenclature Nomenclature]</div><div style="margin-left: 2em">[#Compton Basin-LPOD Articles LPOD Articles]</div><div style="margin-left: 2em">[#Compton Basin-Bibliography Bibliography]</div></div><br />
==Images==<br />
[http://www.lpod.org/coppermine/thumbnails.php?album=search&type=full&search=Compton LPOD Photo Gallery] [http://www.lpi.usra.edu/resources/lunar_orbiter/bin/srch_nam.shtml?Compton%7C0 Lunar Orbiter Images]<br /> <br />
* '''Compton''' was photographed during the mission of Apollo 16, on color-''Hasselblad'' film, such as frame [http://www.lpi.usra.edu/resources/apollo/frame/?AS16-121-19445 AS16-121-19445]. In this frame, '''Compton''''s location is a little bit to the right of centre.<br />
* [http://www.lpi.usra.edu/resources/apollo/frame/?AS16-M-3019 AS16-M-3019] is one of Apollo 16's ''Fairchild''-camera photographs which show '''Compton''' near the limb at lower right. This photograph was made during Trans Earth Coast (TEC).<br />
* Research Apollo 16 photography: Danny Caes<br />
<br /> <br />
==Maps==<br />
''([http://the-moon.wikispaces.com/LAC%20zone LAC zone] 16D1)'' [http://planetarynames.wr.usgs.gov/images/Lunar/lac_16.pdf USGS Digital Atlas PDF]<br /> <br /> <br />
==[http://the-moon.wikispaces.com/Lunar%20Basins Basin Classification]==<br />
(description of terms and most numeric basin data from Wood, C.A. (2004) [http://www.lpod.org/cwm/DataStuff/Lunar%20Basins.htm Impact Basin Database])<br /> <br />
{| class="wiki_table"<br />
| '''Certainty of Existence'''<br /><br />
| '''USGS Age'''<br /><br />
| '''Wilhelms Age Group'''<br /><br />
| '''Ring Diameters'''<br /><br />
| '''Mare Thickness'''<br /><br />
| '''Mascon'''<br /><br />
|-<br />
| Certain<br /><br />
| Lower Imbrian<br /><br />
| <br /><br />
| 80, '''175''' km<br /><br />
| <br /><br />
| No<br /><br />
|}<br />
<br /> <br />
==Description==<br />
Peak ring basin<br /> <br /> <br />
===Wikipedia===<br />
[http://en.wikipedia.org/wiki/Compton_(crater) Compton]<br /> <br /> <br />
==Additional Information==<br />
<br />
* From the shadows in [http://www.lpi.usra.edu/resources/lunarorbiter/frame/?5181 LO-V-181M], the central peaks of '''Compton''' rise about 2700 m above the floor. The crater appears to be somewhat deeper, but the shadows are not suitable for a measurement of its depth. <span class="membersnap">- [http://www.wikispaces.com/user/view/JimMosher [[Image:JimMosher-lg.jpg|16px|JimMosher]]] [http://www.wikispaces.com/user/view/JimMosher JimMosher]</span><br />
* Frame '''2700r''' from the [http://pds-imaging.jpl.nasa.gov/Missions/Galileo_mission.html Galileo] fly-by of the Moon shows the western part of '''Compton''' with a low [http://the-moon.wikispaces.com/sun%20angle sun angle] from the west. The shadows falling on the floor indicate a considerable variation in the height of the western rim, ranging from about 1300 m in north to 4100 m in south, with a typical value of about 3200 m near the middle. <span class="membersnap">- [http://www.wikispaces.com/user/view/JimMosher [[Image:JimMosher-lg.jpg|16px|JimMosher]]] [http://www.wikispaces.com/user/view/JimMosher JimMosher]</span><br />
* Three small pyroclastic deposits (area = 24, 45 & 5 km^2). Gaddis, L. (1999) [http://astrogeology.usgs.gov/Projects/LunarPyroclasticVolcanism/lunpyroWebDb.html Lunar Pyroclastic Volcanism Project].<br />
* Four dark halo/pyroclastic deposits located on floor fractures; three are 2-6 km in diameter, the others is ~15 km wide. [http://www.lpi.usra.edu/meetings/LPSC98/pdf/1710.pdf Rosanova et al, 1998]<br />
* Inner mare patches [http://the-moon.wikispaces.com/Stratigraphy Imbrian] age and 4-4.5 wt% FeO content. Younger maria around outer edges ([http://the-moon.wikispaces.com/Gillis%20and%20Spudis%2C%201996 Gillis and Spudis, 1996]).<br />
* First described as a basin by Hartmann & Wood (1971).<br />
* At favorable [http://the-moon.wikispaces.com/librations librations], '''Compton''' can be seen straddling the limb, but it does not seem to have been recognized in Earth-based observations.<br />
* Telescopic observers of the moon might look for the central peaks of '''Compton''', which are visible during favourable libration! See LPOD [http://lpod.wikispaces.com/June%2011%2C%202009 Peaking over the Limb] and discussions.<br />
<br /> <br />
==Weird stratification at Compton's floor==<br />
<br />
* The eastern region of the floor of '''Compton''' shows some sort of weird stratification''':''' http://bit.ly/2DeCf2X<br />
<br /> <br />
==Nomenclature==<br />
<br />
* The IAU crater name honors two men:<br />
** [http://en.wikipedia.org/wiki/Arthur_Holly_Compton Arthur Holly Compton] (September 10, 1892 – March 15, 1962) was an American physicist who won the Nobel Prize in Physics (1927) for discovery of the Compton effect. In 1922, Compton found that X-rays wavelength increases due to scattering of the radiant energy by "free electrons". Scattered quanta have less energy than the quanta of the original ray. This discovery, known as the "Compton effect," demonstrates the "particle" concept of electromagnetic radiation.<br />
** [http://en.wikipedia.org/wiki/Karl_Taylor_Compton Karl Taylor Compton] (September 14, 1887 – June 22, 1954) was a prominent American physicist and president of the Massachusetts Institute of Technology (MIT) from 1930 to 1948.<br />
* The impact basin was named after the crater.<br />
* '''Compton''' was among the long list of farside names added to the [http://the-moon.wikispaces.com/IAU%20nomenclature IAU nomenclature] in [http://the-moon.wikispaces.com/Menzel%2C%201971 Menzel, 1971].<br />
* '''''Rimae Compton''''' (an unofficial name from D.Caes for the system of rilles on the floor of '''Compton''').<br />
<br /> <br />
==LPOD Articles==<br />
<br />
* [http://www.lpod.org/?m=20070225 Peak Rings]<br />
* [http://lpod.wikispaces.com/June%2011%2C%202009 Peaking over the Limb] (terrestrial photograph of '''Compton''''s central peak).<br />
<br /> <br />
==Bibliography==<br />
<br />
* Joliff, B. L. ''et al'' (2011). [http://www.lpi.usra.edu/meetings/lpsc2011/pdf/2224.pdf Compton-Belkovich: Nonmare, Silicic Volcanism on the Moon’s Far Side] – 42nd [http://www.lpi.usra.edu/meetings/lpsc2011/ LPSC] Conference (Mar), 2011.<br />
* Tran, T. ''et al'' (2011). [http://www.lpi.usra.edu/meetings/lpsc2011/pdf/2228.pdf Morphology of Lunar Volcanic Domes from LROC] – 42nd [http://www.lpi.usra.edu/meetings/lpsc2011/ LPSC] Conference (Mar), 2011.<br />
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