Recent Climate Change and Presence of Near-Surface Ice Deposits: Evidence from Inverted Impact Craters Located on Lineated Valley Fill, Ismenius Lacus Region, Mars

Details Recent Climate Change and Presence of Near-Surface Ice Deposits: Evidence from Inverted Impact Craters Located on Lineated Valley Fill, Ismenius Lacus Region, Mars Recent Climate Change and Presence of Near-Surface Ice Deposits: Evidence from Inverted Impact Craters Located on Lineated Valley Fill, Ismenius Lacus Region, Mars

Jul 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpico1353.3261m&link_type=abstract

Seventh International Conference on Mars, held July 9-13, 2007 in Pasadena, California, LPI Contribution No. 1353, p.3261

Physics

Scientific paper

Inverted impact craters (IICs), located in the western Ismenius Lacus
region, are evidence of episodes of near-surface ice within the past
5-10 Ma, and are results of surface-deflation due to subsequent climate
change.

Affiliated with

Also associated with

No associations

Rating

Recent Climate Change and Presence of Near-Surface Ice Deposits: Evidence from Inverted Impact Craters Located on Lineated Valley Fill, Ismenius Lacus Region, Mars 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 Recent Climate Change and Presence of Near-Surface Ice Deposits: Evidence from Inverted Impact Craters Located on Lineated Valley Fill, Ismenius Lacus Region, Mars, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Recent Climate Change and Presence of Near-Surface Ice Deposits: Evidence from Inverted Impact Craters Located on Lineated Valley Fill, Ismenius Lacus Region, Mars will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-784652