Sunday, December 9, 2018

Death Valley - Week 7



This is an image of the polygonal mud cracks that formed in the Racetrack Playa. From the photo is looks like the polygons are about two to three inches in length. This is very interesting because of the polygon shape of the cracks throughout the large area. While it is obvious what caused the mud, it is not obvious why the cracks appear to have a pattern to them like they do. Not all dry mud cracks are the same which would make me wonder what would cause them. I would guess it could be soil type, how fast it dried out, and how many times the mud dried out. Obviously more factors could be at work, but that is where I would start. Sources for what type of materials are in the mud along with nearby geological features would be helpful in figuring this out.



Above is a photo of Artist’s Drive that has a variety of colors making for a beautiful and bold display. The mountains are curvy and in every direction. What is interesting is that the sediment difference is what I would have expected to make the difference in coloring, but rather the color differences are due to that along with “chemical weathering and hydrothermal alteration”. What would make me curious is if you can predictably change the color of the soil based on what you to do it and the type of soil it is. If this is known then it could be known for other areas where displays like this will occur and predictions could be made.



The photo above is of Zabriskie Point in Death Valley. Here you will find very little life and very little that will survive here. The point is made up of mudstone and sediments like silt and clay. This came from the bodies of water that were here many years ago. Due to the formation of the soil it makes it nearly impossible for the soil to give birth to plant life. Water does come to this point in Death Valley at very intense points in time. Due to the lack of plant life or anything to keep the structure of the land erosion can happen quite rapidly. What I find interesting is the shape of the mountains and how they swivel slightly. I wonder if over time this will begin to become more like a meandering river would be due to the water going back and forth. What would really help determine this would be to witness the rain and how much water volume takes place over the short period of time. This could help you predict if greater waves would appear in the badlands or not.


Frank, D. (n.d.). Death Valley geology field trip. Retrieved December 9, 2018, from https://geomaps.wr.usgs.gov/parks/deva/ftzab1.html

Frank, D. (n.d.). Death Valley geology field trip. Retrieved December 9, 2018, from https://geomaps.wr.usgs.gov/parks/deva/ftrac1.html

Frank, D. (n.d.). Death Valley geology field trip. Retrieved December 9, 2018, from https://geomaps.wr.usgs.gov/parks/deva/ftart1.html

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