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Image credit: NASA / JPL / University of Arizona / USGS. |
“There is ice under roughly a third of the Martian surface, which records the recent geologic history of Mars,” said lead author Dr. Colin Dundas, a research geologist with the Astrogeology Science Center at the U.S. Geological Survey. “What we’ve seen here are cross-sections through the ice that give us a 3D view with more detail than ever before.”
To gain this data, the team examined north and south pole-facing erosional slopes, known as scarps, in eight locations around Mars. Similar to ice cores extracted from Earth, these Martian ice scarps preserve a record of ice deposition and past climates on Mars.
Details of the scarps have revealed that ice layers with different proportions of ice and dust could have formed under varying climate conditions. “This means that relatively pure water ice, capped by only a thin layer of ice-cemented rock and dust, may be readily accessible to future exploration missions.”
Read more about this fascinating story at: http://www.sci-news.com/space/hirise-structure-martian-ice-sheets-05623.html
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