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pro vyhledávání: '"Douglas Sprinkel"'
Publikováno v:
Geology of the Intermountain West. 9:153-179
The Uinta Mountains are an east-west-trending, reverse fault-bounded, basement-cored Laramide uplift. The Eocene Duchesne River Formation and Oligocene Bishop Conglomerate represent late stage, intermontane basin fill of the Uinta Basin in northeaste
Autor:
Riley Brinkerhoff, John McBride, Sam Hudson, Douglas Sprinkel, Ron Harris, Kevin Rey, Eric Tingey
Publikováno v:
Geosites. 50:1-39
The Sand Wash fault zone is a segmented and discontinuous fault system that strikes northwest to south east in the central part of the Uinta Basin. It is approximately 34 kilometers long with an uncommonly wide damage zone, typically 100 to 200 meter
Autor:
Douglas Sprinkel
Publikováno v:
Geosites. 1:1-10
The Palisades is an impressive ridge within the Sheep Creek Canyon Geological Area—an area nestled on the north flank of the eastern Uinta Mountains not far from Flaming Gorge National Recreation Area. Sheep Creek cuts through the Palisades, as wel
Publikováno v:
Geology of the Intermountain West. 6:61-76
The outcrop belt of the Upper Jurassic Morrison Formation in the northeastern Uinta Basin and southeastern flank of the Uinta Mountains is particularly rich in dinosaurian and non-dinosaurian faunas, as well as in fossil plants. The discovery of seve