Monday, December 9, 2019

Brecheisen Week 7 Zabriskie Point


I visited Zabriskie Point this week to observe one of the most famous landscapes in Death Valley. Photos of this stop reveal unique lines and different colors of rocks throughout the area. There doesn’t appear to be any uniformity one would expect of layers being eroded slowly over time or being pushed up from folding. I would like to know how this area was formed. I would also like to know what causes the different colors. The rocks from each layer and the area covered by Zabriskie Point would be useful in creating a geological map of the area. From what I could learn, this area is part of the Furnace Creek formation. The area used to be the base of a large lake nine million years ago. Ashfalls from Black Mountain, saline muds, and gravel from nearby mountains were deposited at the base of this lake. The area became more arid and the lake dried up, revealing the formation. Widening and shrinking of Death Valley along with uplift of the Black Mountains created the ripple effect in the tan sandstone and clay. The dark layer was deposited as lava from volcanic eruptions from three to five million years ago. I wonder where the shoreline of this ancient lake was and a geological map could reveal this shoreline.

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