GRABENS GONE WILD: LATE CENOZOIC EXTENSION ON THE FISH LAKE PLATEAU, UTAH
Numerous graben and half graben complexes segment the FLP. In the eastern FLP, a suite of en-echelon NNW-trending grabens becomes progressively younger towards the east. Grabens offset Pliocene trachybasalt and basin-fill deposits are overlain by 0.5 to 0.9 Ma boulder diamicts on Fremont River terraces. Fish Lake occupies a large graben complex produced by up to 500 m of displacement across a suite of NE-striking faults. The Fish Lake graben complex cuts older NNW-trending grabens and truncates an established SE-trending drainage network. At its southwestern end, the Fish Lake graben is cut by WNW-striking normal faults. The NE-trending Crater Lakes graben occupies a small, internally drained complex bound by transverse faults. The NE-trending Cedarless Flat graben truncated a pre-existing drainage network and is younger than the 0.5 to 0.9 Ma Fremont River terraces.
Normal faulting on the FLP accommodated 5-10% crustal extension. The variable orientation of grabens on the FLP records orthogonal extension of the region during the last 5 My and may be the manifestation of a uniaxial stress field generated by block-segmentation associated with uplift of the region.