KIP Theses and Dissertations

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Publication Date

January 1968

Type

Thesis

Abstract

North of the Grand Canyon, water from precipitation infiltrates into the permeable Kaibab Formation which outcrops over the Kaibab and Kanab Plateaus. Water moves vertically downward through a karst drainage network in the Kaibab and Toroweap Formations until it reaches semi-permeable clastic sediments.

Institution

University of Arizona

Keywords

Geology

Geographic Location

Arizona; Grand Canyon (Ariz.); Coconino County (Ariz.)

Language

English

Identifier

K26-01540

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