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Geologic map of the Kolob Arch quadrangle and part of the Kanarraville quadrangle, Washington and Iron Counties, Utah (M-217) snowmobile gallery-grade photography

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gallery-grade photography

understanding the significance of archaeological sites

With a small trim size and colorful illustrations

The Wasatch fault cuts Holocene and older unconsolidated deposits in the northeastern part of the quadrangle

This publication explores the geologic features found throughout the region

Geologic map of the Kolob Arch quadrangle and part of the Kanarraville quadrangle, Washington and Iron Counties, Utah (M-217) snowmobile gallery-grade photographyBy: R. F. Biek The Kolob Arch quadrangle is at the western margin of the Colorado Plateau, in the transition zone between the Colorado Plateau and Basin and Range physiographic provinces. The Colorado Plateau province is a relatively coherent and tectonically stable region underlain by generally horizontal sedimentary strata that are locally disrupted by early Tertiary Laramide basement block uplifts, Oligocene Miocene igneous intrusions, and late

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