Day Two.  Zabriskie Point, Badwater, Copper Canyon Turtleback, Devil's Golfcourse and Salt Creek.

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 Manly Peak as seen from Zabriskie Point.  The colorful beds are Neogene lake sediments, which are capped to the right by conglomerates


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Badwater.  I never thought that I would see students sink so low


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Jim Harris explains Pickleweed at Badwater. 


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At the foot of the Copper Canyon Turtleback.  The pinkish rocks are Tertiary sediments that are in fault contact with Precambrian gneiss. 


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 Devil's Golf Course.


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Dr. Bybee pontificates on pup fish at the end of the day....                          ....while the group looks on.
 

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