Ring-Mold Craters (RMC) in Lobate Debris Aprons (LDA) In the Deuteronilus Mensae Region of Mars: Evidence for Shallow Subsurface Glacial Ice in Lobate Debris Aprons

Details Ring-Mold Craters (RMC) in Lobate Debris Aprons (LDA) In the Deuteronilus Mensae Region of Mars: Evidence for Shallow Subsurface Glacial Ice in Lobate Debris Aprons Ring-Mold Craters (RMC) in Lobate Debris Aprons (LDA) In the Deuteronilus Mensae Region of Mars: Evidence for Shallow Subsurface Glacial Ice in Lobate Debris Aprons

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.2422o&link_type=abstract

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

Physics

1

Scientific paper

Ring-mold shaped craters, interpreted to represent impacts into
relatively pure ice and resulting spallation, are common in lobate
debris aprons near the dichotomy boundary on Mars; their abundance
suggests a debris-covered glacial origin for LDA.

Affiliated with

Also associated with

No associations

Rating

Ring-Mold Craters (RMC) in Lobate Debris Aprons (LDA) In the Deuteronilus Mensae Region of Mars: Evidence for Shallow Subsurface Glacial Ice in Lobate Debris Aprons 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 (RMC) in Lobate Debris Aprons (LDA) In the Deuteronilus Mensae Region of Mars: Evidence for Shallow Subsurface Glacial Ice in Lobate Debris Aprons, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Ring-Mold Craters (RMC) in Lobate Debris Aprons (LDA) In the Deuteronilus Mensae Region of Mars: Evidence for Shallow Subsurface Glacial Ice in Lobate Debris Aprons will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-775178