Heaving-Bedrock Hazards, Mitigation,
and Land-Use Policy:
Front Range Piedmont, Colorado

DAVID C. NOE
Colorado Geological Survey, 1313 Sherman Street, Room 715, Denver, CO 80203


FIGURE 4: Stratigraphic column of Upper Cretaceous and younger rocks in the greater Denver area (modified from LeRoy, 1955). Heaving bedrock occurs in all of the Upper Cretaceous formations where they are steeply dipping, on the flank of the Front Range uplift. The Pierre Shale is the most important formation with respect to heaving bedrock occurrence and damage.

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NOTE: This information is provided for general education only. For detailed information concerning reactive soils, you should always contact a geo-technical firm.




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