Viewpoint 3 Viewpoint 4 Lower Little Spring Canyon

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Date: 2006-08-14 12:23:38 Historical geology Canyonlands National Park Sedimentary rock Law of superposition Formation Stratum Mesa Geology of the Canyonlands area Geology of the Grand Canyon area Geology Utah Stratigraphy		Viewpoint 3 Viewpoint 4 Lower Little Spring Canyon Add to Reading List Source URL: www.cnha.org Download Document from Source Website File Size: 137,43 KB Share Document on Facebook

	Methods of Determining the Age of Rock Stratigraphic (Law of Superposition) Geologists generally assume that in a layer of undisturbed rocks, the older deposits are on the bottom and, as you move upwards, you encounter p DocID: 1sg21 - View Document
	Methods of Determining the Age of Rock Stratigraphic (Law of Superposition) Geologists generally assume that in a layer of undisturbed rocks, the older deposits are on the bottom and, as you move upwards, you encounter p DocID: 1rU71 - View Document
	Methods of Determining the Age of Rock Stratigraphic (Law of Superposition) Geologists generally assume that in a layer of undisturbed rocks, the older deposits are on the bottom and, as you move upwards, you encounter p DocID: 1rLBr - View Document
	Methods of Determining the Age of Rock Stratigraphic (Law of Superposition) Geologists generally assume that in a layer of undisturbed rocks, the older deposits are on the bottom and, as you move upwards, you encounter p DocID: 1owzK - View Document
	WOFR06-06 bdrock strat units_... DocID: 19hS2 - View Document