B. Geology and Paleontology The geology of the CPNA is the product of millions of years of erosion, sediment deposition, faulting, volcanism and uplift. From a geological perspective, the mountains and valleys are relati

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Date: 2015-01-23 11:05:19 Environmental soil science Carrizo Plain Pacific Coast Ranges Temblor Range Painted Rock Caliente Range Fault Soil Caliente Geography of California California Petrology		B. Geology and Paleontology The geology of the CPNA is the product of millions of years of erosion, sediment deposition, faulting, volcanism and uplift. From a geological perspective, the mountains and valleys are relati Add to Reading List Source URL: www.blm.gov Download Document from Source Website File Size: 279,80 KB Share Document on Facebook

	PS AAPG 2014 Guidebook Cover 08Apr2014 DocID: 1qT07 - View Document
	UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Aerial views in color of the San Andreas fault, California Robert E. Wallace and Sandra S. Schulz DocID: NIkM - View Document
	II. RESOURCE DESCRIPTION A. Geographical Setting This section describes the historical and current state of resources and management activities in the CPNA. 1. Physical Setting The CPNA encompasses two plains: the Elkhor DocID: MgwV - View Document
	B. Geology and Paleontology The geology of the CPNA is the product of millions of years of erosion, sediment deposition, faulting, volcanism and uplift. From a geological perspective, the mountains and valleys are relati DocID: MgcT - View Document
	I. INTRODUCTION The CPNA, lying adjacent to the southwest edge of the San Joaquin Valley, is the largest remaining tract of the San Joaquin valley biogeographic province with limited evidence of human alteration. The 253 DocID: Mg7L - View Document