Monday, April 22, 2019

Week 7 - Death Valley Field Trip - James Di Giovanni

Panamint alluvial apron
Image Retrieved from: https://geomaps.wr.usgs.gov/parks/deva/ftgol1.html
         
At the Golden Canyon stop, there is an image of the mouth of the canyon showing large boulders strewn about. These large boulders were brought in with flash flooding and were deposited in the process. I would like to know the composition of these rocks, as well as the composition of the rocks in the surrounding area to try to find how far these rocks traveled during the flash flooding. A geological map would help me with inferring the type of rocks surrounding the canyon, while investigation could help me identify the composition of the displaced boulders. I would also look for signs of erosion on the boulders to try to estimate how long ago the flash flooding occurred.


Aerial view of Split Cinder Cone
Image Retrieved from: https://geomaps.wr.usgs.gov/parks/deva/ftcin2.html
At the Split Cindercone stop, there is an image of a cinder cone that has been split along a fault line. I would like to know if there are any other geologic features that have resulted by the shift in the fault that caused this splitting to occur. I would also like to know the size of the cindercone to have a better understanding of how dramatic of a shift has occurred to put the pieces of the cindercone where they are today.


Artist's Pallet
Image Retrieved from: https://geomaps.wr.usgs.gov/parks/deva/ftart1.html
At the Artist’s Drive stop, there is an image of a formation of rocks that are many different colors. These colors are caused by different composition of minerals, chemical weathering, and hydrothermal alteration. One question I have about the formation is “is the differential weathering pattern the result of rock composition, specific faulting, or both”. One way I could work to find this out is to study geologic maps for faults and testing the composition of the rocks.



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