Basal scarp, paleoglacier, and fissure flows of Elysium Mons, Mars
Geological mapping at 1:500,000 scale of the Granicus Valles area west of Elysium Mons (MTM quadrangles 30227, 30222, and 25227) indicates that (1) the oldest deposits in the area are Upper Hesperian lavas of the Elysium shield; (2) a basal scarp formed by Early Amazonian faulting around the northwe...
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| Format: | Other/Unknown Material |
| Language: | unknown |
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1993
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| Online Access: | http://ntrs.nasa.gov/search.jsp?R=19940007676 |