There's a lot of amazing deformation to see just standing outside the Dam visitor's center. To the south is Rattlesnake Ridge
A basic orientation of beds
Geometry of the fault plane and folding that resulted in the deformation
Looking north, the road-cut exhibits a shear-zone feature. The Cambrian shales are truncated under the Bighorn formation, the Flathead Sandstone not present in the sequence
(formations labeled)
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