1st November 2013 Sol 439

We have driven right up to the Cooperstown outcrop.  The rdige (a few tens of cm high) is composed of a resistant layer of sedimentary rock.  This is the most extensive and detailed sedimentary outcrop since we left Yellowknife Bay.

Its also a  fantastic view of the crater rim, a bit dusty but you can see what look like ancient landslides as the rim has degraded over billions of years since Gale Crater formed about 3.6 billion years ago.

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jbridges

About jbridges

This blog is a record of my experiences and work during the Mars Science Laboratory mission, from the preparation, landing on August 5th 2012 Pacific Time, and onwards... I will also post updates about our other Mars work on meteorites, ExoMars and new missions. You can also follow the planetary science activities with @LeicsPlanets Professor John Bridges, School of Physics and Astronomy

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