Cracks as Evidence for Water Evaporation and Condensation Associated with Temperature Changes in Hydrous Sulfate Sands

Details Cracks as Evidence for Water Evaporation and Condensation Associated with Temperature Changes in Hydrous Sulfate Sands Cracks as Evidence for Water Evaporation and Condensation Associated with Temperature Changes in Hydrous Sulfate Sands

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.2246c&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

Scientific paper

Mineral-atmospheric water cycling promotes crack formation in the
hydrous sulfate (gypsum) sands at White Sands National Monument, New
Mexico. A similar water cycling process may promote crack formation in
sulfate outcrops on Meridiani Planum, Mars.

Affiliated with

Also associated with

No associations

Rating

Cracks as Evidence for Water Evaporation and Condensation Associated with Temperature Changes in Hydrous Sulfate Sands 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 Cracks as Evidence for Water Evaporation and Condensation Associated with Temperature Changes in Hydrous Sulfate Sands, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Cracks as Evidence for Water Evaporation and Condensation Associated with Temperature Changes in Hydrous Sulfate Sands will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1823399