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Thus the Coastal Ranges take on the appearance of an uplifted horst , bounded, particularly to the east, by normal faults.

The main effect of the orogeny in southeastern Utah was to uplift the Uncompahgre High, a horst composed of Precambrian strata, which is bound on its southwestern flank by a major reverse fault.

These faults bound horsts , grabens and tilted blocks.

The area is characterized by a series of low-relief Jurassic horsts and graben.

A thinner series of these rocks occurs on top of horsts of Jurassic rocks.