Difference between revisions of "November 8, 2014"
Line 1: | Line 1: | ||
__NOTOC__ | __NOTOC__ | ||
=Most Famous Crater of Se Quadrant?= | =Most Famous Crater of Se Quadrant?= | ||
− | |||
<!-- ws:start:WikiTextHeadingRule:0:<h1> --> | <!-- ws:start:WikiTextHeadingRule:0:<h1> --> | ||
<!-- ws:start:WikiTextLocalImageRule:6:<img src="/file/view/LPOD-Nov8-14.jpg/530066516/LPOD-Nov8-14.jpg" alt="" title="" /> -->[[File:LPOD-Nov8-14.jpg|LPOD-Nov8-14.jpg]]<!-- ws:end:WikiTextLocalImageRule:6 --><br /> | <!-- ws:start:WikiTextLocalImageRule:6:<img src="/file/view/LPOD-Nov8-14.jpg/530066516/LPOD-Nov8-14.jpg" alt="" title="" /> -->[[File:LPOD-Nov8-14.jpg|LPOD-Nov8-14.jpg]]<!-- ws:end:WikiTextLocalImageRule:6 --><br /> | ||
− | <em>image by [mailto:paolo@lazzarotti-hires.com Paolo R. Lazzarotti], Italy</em><br /> | + | <em>image by [mailto:paolo@lazzarotti-hires.com" rel="nofollow Paolo R. Lazzarotti], Italy</em><br /> |
<br /> | <br /> | ||
− | Janssen is an odd crater. It has a non-circular outline which causes uncertainty in how many [http://www.lpod.org/?m=20071001 overlapping] craters form it. The fresh crater Fabricius - in shadow here - smashed into Janssen's northern floor, and the broad elevated area to its south [http://lpod.wikispaces.com/October+10%2C+2013 may be] material displaced by its formation. The elevated area - perhaps a [http://lpod.wikispaces.com/July+17%2C+2014 dome?] - is cut by Janssen's famous curved rille, which becomes much thinner and does not seem to be part of the broader rille. Rilles in highland material are very unusual - perhaps the rilles cut ejecta from the formation of the Nectaris Basin. Northwest of the broad rille are two to three overlapping degraded craters that probably are basin secondaries, also from Nectaris. <br /> | + | Janssen is an odd crater. It has a non-circular outline which causes uncertainty in how many [http://www.lpod.org/?m=20071001" rel="nofollow overlapping] craters form it. The fresh crater Fabricius - in shadow here - smashed into Janssen's northern floor, and the broad elevated area to its south [http://lpod.wikispaces.com/October+10%2C+2013 may be] material displaced by its formation. The elevated area - perhaps a [http://lpod.wikispaces.com/July+17%2C+2014 dome?] - is cut by Janssen's famous curved rille, which becomes much thinner and does not seem to be part of the broader rille. Rilles in highland material are very unusual - perhaps the rilles cut ejecta from the formation of the Nectaris Basin. Northwest of the broad rille are two to three overlapping degraded craters that probably are basin secondaries, also from Nectaris. <br /> |
<br /> | <br /> | ||
− | <em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> | + | <em>[mailto:tychocrater@yahoo.com" rel="nofollow Chuck Wood]</em><br /> |
<br /> | <br /> | ||
<strong>Technical Details</strong><br /> | <strong>Technical Details</strong><br /> | ||
− | Here is a full resolution [http://www.lazzarotti-hires.com/2014/11/ultimi-raggi-su-janssen.html?lan=english view] of this image.<br /> | + | Here is a full resolution [http://www.lazzarotti-hires.com/2014/11/ultimi-raggi-su-janssen.html?lan=english" rel="nofollow view] of this image.<br /> |
<br /> | <br /> | ||
<strong>Related Links</strong><br /> | <strong>Related Links</strong><br /> | ||
<em>[http://lpod.wikispaces.com/21st+Century+Atlas+of+the+Moon 21st Century Atlas]</em> chart 5.<br /> | <em>[http://lpod.wikispaces.com/21st+Century+Atlas+of+the+Moon 21st Century Atlas]</em> chart 5.<br /> | ||
− | Paolo's [http://www.lazzarotti-hires.com website]<br /> | + | Paolo's [http://www.lazzarotti-hires.com" rel="nofollow website]<br /> |
<br /> | <br /> | ||
<hr /> | <hr /> |
Revision as of 22:06, 4 January 2015
Most Famous Crater of Se Quadrant?
image by " rel="nofollow Paolo R. Lazzarotti, Italy
Janssen is an odd crater. It has a non-circular outline which causes uncertainty in how many " rel="nofollow overlapping craters form it. The fresh crater Fabricius - in shadow here - smashed into Janssen's northern floor, and the broad elevated area to its south may be material displaced by its formation. The elevated area - perhaps a dome? - is cut by Janssen's famous curved rille, which becomes much thinner and does not seem to be part of the broader rille. Rilles in highland material are very unusual - perhaps the rilles cut ejecta from the formation of the Nectaris Basin. Northwest of the broad rille are two to three overlapping degraded craters that probably are basin secondaries, also from Nectaris.
" rel="nofollow Chuck Wood
Technical Details
Here is a full resolution " rel="nofollow view of this image.
Related Links
21st Century Atlas chart 5.
Paolo's " rel="nofollow website