Download Published Version (PDF / 341kB).pdf

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🔗 Source: oro.open.ac.uk
📊 Size: 333 KB
📄 Pages: 2 pages
⬇️ Downloads: 288

Summary

Researchers found evidence of recent wet-based crater glaciation in Tempe Terra, Mars, by studying sinuous ridges emerging from viscous flow features (VFF) in a 45 km-diameter crater. They identified two populations of sinuous ridges: a southern population that may be eskers formed by melting of glaciers, and a northern population that appears to be topographically inverted subaerial fluvial channels. The southern ridges emerge from VFF-terminal lobes and have sharp crests, while the northern ridges are wider and more flat-topped. The study suggests that the southern sinuous ridges could be eskers, which would provide evidence for past melting of mid-latitude glaciers on Mars, but the alternative hypothesis that they are inverted channels is also possible.

Description

Researchers found evidence of recent wet-based crater glaciation in Tempe Terra, Mars, by studying sinuous ridges emerging from viscous flow features (VFF) in...

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  • File Format: PDF
  • File Size: 333 KB
  • Pages: 2
  • Language: EN
  • Total Downloads: 288
  • Last Updated: 7 days ago

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