Tertiary geologic history of the Salt River Canyon region, Gila County, Arizona
An early Tertiary northeast-flowing consequent drainage in the Transition Zone of east-central Arizona excavated an 1170+-m-deep, 14- to 23-km-wide, 30+-km-long, northeast-trending paleocanyon in a broad Laramide uplift west of the Canyon Creek fault, which included, but was not confined to, the Apa...
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| Language: | en |
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The University of Arizona.
1986
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| Online Access: | http://hdl.handle.net/10150/191881 |