Difference between revisions of "April 24, 2005"
(2 intermediate revisions by the same user not shown) | |||
Line 1: | Line 1: | ||
__NOTOC__ | __NOTOC__ | ||
=Fabulous Fab!= | =Fabulous Fab!= | ||
+ | <!-- Start of content --> | ||
<table width="85%" border="0" align="center" cellpadding="6" cellspacing="2"> | <table width="85%" border="0" align="center" cellpadding="6" cellspacing="2"> | ||
<tr> | <tr> | ||
Line 25: | Line 26: | ||
April 15, 2005. 18" dob + Atik webcam + 5X's barlow + Baader IR passband filter.</p> | April 15, 2005. 18" dob + Atik webcam + 5X's barlow + Baader IR passband filter.</p> | ||
<p><b>Related Links:</b><br> | <p><b>Related Links:</b><br> | ||
− | [ | + | [http://www.lpi.usra.edu/resources/lunar_orbiter/images/img/iv_071_h2.jpg Lunar Orbiter IV View] |
<br>Rukl Plate 68 | <br>Rukl Plate 68 | ||
</p> | </p> | ||
Line 40: | Line 41: | ||
<p align="center" class="main_titles"><b>Author & Editor:</b><br> | <p align="center" class="main_titles"><b>Author & Editor:</b><br> | ||
[mailto:tychocrater@yahoo.com Charles A. Wood]</p> | [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 --> |
− | + | <!-- Cleanup of credits --> | |
− | < | + | <!-- Cleanup of credits --> |
− | + | <!-- Cleanup of credits --> | |
</td></tr> | </td></tr> | ||
</table> | </table> | ||
<p> </p> | <p> </p> | ||
+ | <!-- End of content --> | ||
{{wiki/ArticleFooter}} | {{wiki/ArticleFooter}} |
Latest revision as of 14:14, 15 March 2015
Fabulous Fab!
Image Credit: Mike Wirths |
Fabulous Fab! Have you ever looked carefully at Fabricius? I hadnt until I studied this great image. Usually Fabricius is seen as an obstruction hiding part of the floor of the large crater Janssen, but it is a fascinating crater in its own right. Fabricius (diameter 78 km) is mostly a Tycho-like complex crater, with terraced rim, flat floor and central peak. But the floor contains a horseshoe-like massive ridge. This is does not make Fabricius a floor-fractured crater - their concentric pattern is of rilles. I would guess that the floor arc of Fabricius formed by a terrace sliding down the crater walls. The ridge is completely free of the wall on the NW side, but is adjacent to the SE wall, like a normal terrace. On the southern portion of the floor a small crater occurs in the middle of a short rille, one of the few in a highlands crater. The rim of Fabricius has two abnormalities to notice. On the left (S), an angular scallop suggests that a large rim collapse started but didn't collapse entirely. At the bottom (W) of the crater a thin ridge extends from the rim onto the adjacent highland and then curves back. This looks like another place where a rim scallop subsided only slightly. Compare this image with the Lunar Orbiter IV image - they have essentially the same resolution! Technical Details: Related Links: Yesterday's LPOD: The Best Lava Flow on the Moon Tomorrow's LPOD: A Chain of Mystery |
Author & Editor: |
COMMENTS?
Register, Log in, and join in the comments.