Copy the page URI to the clipboard
Butcher, F. E.G.; Conway, S. J. and Arnold, N. S.
(2016).
URL: http://www.hou.usra.edu/meetings/marspolar2016/pdf...
Abstract
The Dorsa Argentea (DA) are an assemblage of ridges in Mars’ southern high latitudes (70°-80°S, 56°W-6°E). Glacial eskers and inverted channels remain as active hypotheses for their formation. The esker interpretation is widely used as a basis for reconstructions of meltwater production beneath a putative former ice sheet in the region of the DA during Mars’ Hesperian period, despite a lack of rigorous quantitative testing of the esker hypothesis. We undertake the first large-scale quantitative analysis of the plan view geometries of the DA in a comparison to >5900 terrestrial esker systems in Canada. Statistical tests for esker-like topographic relationships are also completed. Our results support the esker hypothesis and highlight that future studies of the DA and its parent ice sheet should more closely consider the ongoing debate over the spatio-temporal nature of terrestrial esker formation, and its implications for reconstructions of ice sheet meltwater production.
Viewing alternatives
Download history
Item Actions
Export
About
- Item ORO ID
- 47704
- Item Type
- Conference or Workshop Item
- Project Funding Details
-
Funded Project Name Project ID Funding Body The Geomorphology of Glacial Landscapes on Mars - PhD Studentship ST/N50421X/1 STFC (Science and Technology Facilities Council) Leverhulme Trust Grant RPG-397 The Leverhulme Trust - Keywords
- Mars; polar geology; martian surface; geological processes; geomorphology; planetary science; geology; glaciers; remote sensing
- Academic Unit or School
-
Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM) - Copyright Holders
- © 2016 The Authors
- Related URLs
- Depositing User
- Frances Butcher