Posted by jbridges in Mars Science Laboratory Blog on November 1, 2013
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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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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