July 11, 2022

From LPOD
Revision as of 00:05, 11 July 2022 by Api (talk | contribs) (Created page with "__NOTOC__ =Small Mystery= Originally published August 19, 2012 <!-- Start of content --> <!-- ws:start:WikiTextHeadingRule:0:<h1> --> <!-- ws:start:WikiTextLocalIma...")
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)
Jump to: navigation, search

Small Mystery

Originally published August 19, 2012 LPOD-Aug19-12.jpg
LRO WAC image from QuickMap, found by Maurice Collins, New Zealand

LPOD-Aug19b-12.jpg
See anything odd in this image? The large crater is a pretty standard small impact 1.3 km in diameter, about 25 km west of Helicon in northwestern Mare Imbrium. The semicircular arc to the south looks like a ghost crater - an impact crater that formed on an earlier lava flow that has been covered by a more recent one. But it is strange that the ghost feature cuts into the younger crater's rim. In the mid- 1960s the British scientist Gilbert Fielder, who believed that lunar craters were volcanic rings, proposed that ghost craters were volcanic features that had not completed their eruptions. They were craters that were stillborn. With such an interpretation this scene would be expected - an older crater (with the bright rim) is interrupted by a younger one only partially formed. But nobody believes lunar craters are volcanoes anymore so this relationship causes a quandry. What explanation do you offer?


Chuck Wood

Added Note: Maurice just found a lower Sun view which I've added at left. It shows a narrow ring extending 3/4 of the way around.

Related Links
Rükl plate 10

Yesterday's LPOD: Data

Tomorrow's LPOD: Wow!



COMMENTS?

Register, Log in, and join in the comments.