Black Canyon of the Gunnison Photo Credit: Nefratiri Weeks |
Gunnison River Photo Credit: Nefratiri Weeks |
About 25 mya, the Tertiary period brought volcanic eruptions from surrounding mountain ranges – the West Elks and San Juans.
This volcanic activity resulted in pyroclastic flows that covered the area with rock and ash. Coupled with snowfall, this helped form the headwaters of the Gunnison River.
Around 2-3 mya, another “broad uplift initiated a period of active erosion” which is when the Canyon was formed (ibid., p. 20). The Gunnison River began flowing across the plateau of the soft ash sediment.
References:
Thronberry-Ehrlich, T. 2005. Black Canyon of the Gunnison National Park & Curecanti National Recreation Area Geologic Resource Evaluation Report. Natural Resource Report NPS/NRPC/GRD/NRR--2005/001. National Park Service, Denver, Colorado. http://www.nature.nps.gov/geology/inventory/publications/reports/blca_cure_gre_rpt_view.pdf. Retrieved October 18, 2010.
USGS: Geological Survey Bulletin 1191. Black Canyon of the Gunnison Today and Yesterday: Rock Formations - Why the Black Canyon Crosses the Gunnison Uplift. http://www.nps.gov/history/history/online_books/geology/publications/bul/1191/sec3.htm. Retrieved November 29, 2010.
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