As an application of their criteria-based methodology for determining the mechanism of transverse drainage development, Douglass, et al. (2009) determined overflow as the mechanism for transverse drainage of the eastern portion of the Grand Canyon.
Elevation: 6886ft, 2099m.
Articles that refer to this location:
Literature Referring To This Location:
Carden, Michael W. (Edited by Dr. Robert C. Grayson, Jr.). 1993.
Southwestern U. S. Field Trip Guidebook.
Waco, Texas: Department of Geology, Baylor University, Spring 1993.
Dehler, C. M., M. Elrick, J. D. Bloch, L. J. Crossey, K. E. Karlson, and D. J. Des Marais. 2005.
High-resolution d13C stratigraphy of the Chuar Group (ca. 770-742 Ma), Grand Canyon: Implications for mid-Neoproterozoic climate change.
Douglass, John, Norman Meek, Ronald I. Dorn and Mark W. Schmeeckle. 2009.
A criteria-based methodology for determining the mechanism of transverse drainage development, with application to the southwestern United States.
Karlstrom, Karl E., Ryan S. Crow, Lisa Peters, William McIntosh, Jason Raucci, Laura J. Crossey, Paul Umhoefer, and Nelia Dunbar. 2007.
40Ar/39Ar and field studies of Quaternary basalts in Grand Canyon and model for carving Grand Canyon: Quantifying the interaction of river incision and normal faulting across the western edge of the Colorado Plateau.
Geological Society of America Bulletin.
Post, Douglas M. 1956.
Studies in the Gentianaceae:
Frasera and Swertia of North America.
Ph.D. dissertation. University of California, Berkeley. 1956..
Species collected at or near this location:
Frasera albomarginata S. Watson. (Oth)
Frasera speciosa Griseb. Elkweed (Oth)
Undet.. Unknown (Oth)
Allium nevadense S. Watson nevadense. Nevada Onion (Oth)
|Total number of taxa:|| 4
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Indentified as Weed
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Date and time this article was prepared:8:57:00 PM, 5/26/2021.