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Carnegie Rupes

Escarpment on Mercury From Wikipedia, the free encyclopedia

Carnegie Rupes
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Discovery Rupes is an escarpment on Mercury, approximately 267 kilometers (166 mi) long, located at latitude 58.52 N and longitude 53.25 W.[1] It was formed by a thrust fault, thought to have occurred due to the shrinkage of the planet's core as it cooled over time. The scarp cuts through Duccio crater.

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The rupes are named after the Carnegie, a wooden (non-magnetic) American ship used to carry out magnetic observations.

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