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3. Ice-Enriched Loess and the Formation of Periglacial Terrain in Mid-Utopia Planitia, Mars

Author

Soare, R.J., Conway, S., Pearce, G.D., and Costard, F.

Abstract

Landforms suggestive of periglacial processes are commonplace in mid-Utopia Planitia, Mars. They form syngenetically in ground-ice comprised of loess transported by katabatic wind from the NPLDs and enriched by ice through the thaw-freeze cycling of obliquity-driven precipitation.

Published
2012

4. Ice-Enriched Loess and the Formation of Periglacial Terrain in Mid-Utopia Planitia, Mars

Author

Soare, R.J., Conway, S., Pearce, G.D., Costard, F., Soare, R.J., Conway, S., Pearce, G.D., and Costard, F.

Abstract

Landforms suggestive of periglacial processes are commonplace in mid-Utopia Planitia, Mars. They form syngenetically in ground-ice comprised of loess transported by katabatic wind from the NPLDs and enriched by ice through the thaw-freeze cycling of obliquity-driven precipitation.

5. Ice-Enriched Loess and the Formation of Periglacial Terrain in Mid-Utopia Planitia, Mars

Author

Soare, R.J., Conway, S., Pearce, G.D., Costard, F., Soare, R.J., Conway, S., Pearce, G.D., and Costard, F.

Abstract

Landforms suggestive of periglacial processes are commonplace in mid-Utopia Planitia, Mars. They form syngenetically in ground-ice comprised of loess transported by katabatic wind from the NPLDs and enriched by ice through the thaw-freeze cycling of obliquity-driven precipitation.

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