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Alternating bands of gneiss and schist Photo Credit: NPS.gov http://www.nps.gov/blca/naturescience/precambrian.htm |
In addition, ribbons of intrusive pegmatite are interspersed, which formed as hot magma forced its way into the rock and cooled very slowly, forming large crystalline structures. (NPS.gov).
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Large bands of Pegmatite Ribbons on the Painted Wall of the Black Canyon Photo Credit: Colorado Geology Photojournals http://www.cliffshade.com/colorado/ |
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Photo Credit: Nefratiri Weeks |
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.
NPS.gov. Natural Features and Ecosystems, Geologic Story: Precambrian. http://www.nps.gov/blca/naturescience/precambrian.htm.Retrieved November 16, 2010.
USGS: Geological Survey Bulletin 1191. Black Canyon of the Gunnison Today and Yesterday: Rock Formations - Their Attributes and Geologic Setting. http://www.nps.gov/history/history/online_books/geology/publications/bul/1191/sec4f.htm Retrieved November 16, 2010.
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