Ring-Mold Craters on Lineated Valley Fill (LVF) and Lobate Debris Aprons (LDA) on Mars (II): Implications for the Presence of Subsurface Ice

Details Ring-Mold Craters on Lineated Valley Fill (LVF) and Lobate Debris Aprons (LDA) on Mars (II): Implications for the Presence of Subsurface Ice Ring-Mold Craters on Lineated Valley Fill (LVF) and Lobate Debris Aprons (LDA) on Mars (II): Implications for the Presence of Subsurface Ice

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1293k&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Physics

6

Scientific paper

"Ring-mold craters" (RMC) occur almost exclusively on lineated valley
fill and lobate debris aprons and are interpreted to be due to
spallation in ice substrate, suggesting that LDA/LVF are debris covered
glaciers, not ice-assisted creep of talus.

Affiliated with

Also associated with

No associations

Rating

Ring-Mold Craters on Lineated Valley Fill (LVF) and Lobate Debris Aprons (LDA) on Mars (II): Implications for the Presence of Subsurface Ice does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Ring-Mold Craters on Lineated Valley Fill (LVF) and Lobate Debris Aprons (LDA) on Mars (II): Implications for the Presence of Subsurface Ice, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Ring-Mold Craters on Lineated Valley Fill (LVF) and Lobate Debris Aprons (LDA) on Mars (II): Implications for the Presence of Subsurface Ice will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-769099