Posted by jbridges in Mars Science Laboratory Blog on January 31, 2015
The second attempt at drilling Mojave has been succesfull by both the minidrill and main drill hole (diameter 1.5 cm, depth ~6 cm). Now we are analysing the tailings with ChemCam and APXS. We will get X-ray diffraction identification from the extracted powder. Mojave may have formed with more evaporating water, in acid conditions rather than the more neutral conditions that we studied in the underlying horizons like Yellowknife Bay.
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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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