The Ubehebe Craters is a collection of maars formed during
eruptions of alkali basalt along a fault on the flanks of Tin Mountain in Death
Valley. The largest of these craters is the Ubehebe, a .5 mile across 600-foot
deep maar surrounded by a tuff ring.
Ubehebe Craters in Death Valley National Park [PHOTO: https://www.usgs.gov/center-news/short-story-ubehebe-crater-death-valley-national-park
By, Duane Champion]
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On the walls of the crater, you can clearly see the
stratum.
Sediment stripes on the walls of the Ubehebe crater [PHOTO: https://en.wikipedia.org/wiki/File:Ubehebe-walls.jpg By, Elizabeth Saxton Henry] |
I can clearly see the different layers of reddish-orange,
tan, with gray and black sediments on top post eruption. I would be interested
to know what a geologic map would have as the pre eruption geology; it looks
like in my second photo that is some faulting between the tan and reddish-orange
layers. I am sure the current day area is marked on geologic maps as
pyroclastic flow.
References
Global Volcanism Program, 2013. Volcanoes of the World, v.
4.8.8 (17 Apr 2020). Venzke, E (n.d.). Smithsonian Institution. Accessed 23 Apr
2020. https://volcano.si.edu/volcano.cfm?vn=323160.
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