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Contributors:
  1. Kathrine Udell
  2. Paul Schenk
  3. Jennifer Scully
  4. Carol Raymond

Date created: | Last Updated:

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Category: Project

Description: Here, we test the hypothesis that water-rich impact melt units in Occator crater on Ceres gave rise to pingo analog forming systems by quantitatively addressing whether morphology can distinguish pingo-like structures from other hill-forms. Our results indicate that the morphologies of the Occator hills and terrestrial pingos are demonstrably similar while also being quantifiably distinct from those of terrestrial volcanic cones.

License: CC-By Attribution 4.0 International

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