Marathon Uplift

Marathon Uplift
Marathon Uplift
Uplift
Exposed ridges of the Ouachita orogeny trend northeast near Marathon, Texas.
Country United States
State Texas
District Brewster County
Coordinates 30°12′27″N 103°14′36″W / 30.2075°N 103.24333°W / 30.2075; -103.24333
Timezone Central (UTC-6)
 - summer (DST) CDT (UTC-5)
location of Marathon Uplift in Texas

The Marathon Uplift is a Tertiary-age domal uplift, approximately 78 miles (126 km) in diameter, in southwest Texas.[1] The Marathon Basin was created by erosion of Cretaceous and younger strata from the crest of the uplift. Northeast trending ridges of pre-Permian Paleozoic strata in the basin were formed by the Ouachita orogeny, which also formed the Ouachita Mountains of Arkansas and Oklahoma.

References

  1. ^ McBride, Earle F. (1998). "Geology of the Marathon Uplift, west Texas". Geological Society of America Centennial Field Guide—South-Central Section. http://rockfractureandstress.com/Burnett%20Ranch/Geology%20of%20the%20Marathon%20Uplift,%20west%20Texas.pdf. 
Novaculite flatirons in the Marathon Uplift



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