Manly Peak as seen from Zabriskie Point. The colorful beds are Neogene lake sediments, which are capped to the right by conglomerates.
Badwater. I never thought that I would see students sink so low.
Jim Harris explains Pickleweed at Badwater.
At the foot of the Copper Canyon Turtleback. The pinkish rocks are Tertiary sediments that are in fault contact with Precambrian gneiss.
Devil's Golf Course.
Dr. Bybee pontificates
on pup fish at the end of the day....
....while the group looks on.
Valley Home Day