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Mars Organic Analyzer
This is a simulation of water-ice accumulation (millimetres per Martian year) from the atmosphere, as predicted to have taken place in the Eastern Hellas basin a few million years ago by the Martian climate computer model. Such ice accumulation is in agreement with the glacier-like landforms observed today in this region.
Credits: Lab. de Meteorologie Dynamic, IPSL (Paris, France)/MGS MOLA


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