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Numerous thrust faults and related folds intersect at Turret Rock, located in the central crater. This structure indicates the complex compressional regime that existed during the formation of Upheaval Dome.

Numerous thrust faults and related folds intersect at Turret Rock, located in the central crater. This structure indicates the complex compressional regime that existed during the formation of Upheaval Dome.

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Figure 1. Oblique air photo looking west across Upheaval Dome, with...
Figure 3. Stratigraphic section for Upheaval Dome. Unless otherwise...
Figure 4. Numerous thrust faults and related folds intersect at Turret...
Figure 5. Sweeping folds like these occur throughout the central...
+34 Figure 6. These Moenkopi beds display original sedimentary structures,...
Geology and structure of Upheaval Dome, San Juan County, Utah: Salt or Impact Structure
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  • May 1995
Upheaval Dome, San Juan County, Utah, is a complexly deformed circular structure approximately 5 km in diameter, occurring within the Triassic Moenkopi, Chinle, Wingate, and Kayenta and the Jurassic Navajo Formations. The structure shows three distinct zones of deformation. The brittlely deformed central crater exhibits an intensely compressional r...
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