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Showing 1 to 11 of 11 for “"Uinta Mountains"”.

  1. Prehistoric Timberline Adaptations in the Eastern Uinta Mountains, Utah

    … archaeological site (3350 m) in the eastern Uinta Mountains, Utah, uncovered at least three ephemeral brush structures. These temporary timberline dwellings are the highest structures excavated in Utah to date. The periods of occupation range from the early Fremont period to the post-contact …

    byu Repository record for Prehistoric Timberline Adaptations in the Eastern Uinta Mountains, Utah (opens in a new tab)

  2. Influence of structural variability on glacially-eroded steps, Uinta Mountains, UT

    … valleys on the southern slopes of the western Uinta Mountains exhibit stepped erosional profiles. These profiles consist of tall, steep, cliffs (~10m high) separated by low relief areas, which are often occupied by lakes. Directly opposite these valleys, on the northern slopes of the range, the …

    uiuc Repository record for Influence of structural variability on glacially-eroded steps, Uinta Mountains, UT (opens in a new tab)

  3. Pre-Historic Landslides on the Southeast Flank of the Uinta Mountains, Utah: Character and Causes of Slope Failure

    … been mapped along the southeast flank of the Uinta Mountains. Large landslide deposits are up to 4.6 kilometers long and have an area of approximately 5-9 km². Landslide types include multiple and successive rock slumps, debris slumps and debris flows. Most landslides have a main head scarp in …

    byu Repository record for Pre-Historic Landslides on the Southeast Flank of the Uinta Mountains, Utah: Character and Causes of Slope Failure (opens in a new tab)

  4. Mapping and Kinematic Structural Analysis of the Deep Creek Fault Zone, South Flank of the Uinta Mountains, Near Vernal, Utah

    The geology along the southern flank of the Uinta Mountains, located north of Vernal, Utah, has been mapped at the 7.5' scale within two quadrangles: the Dry Fork and Steinaker Reservoir Quadrangles. Ambiguities dealing with stratigraphy, structural geology, and geohazards are currently being …

    byu Repository record for Mapping and Kinematic Structural Analysis of the Deep Creek Fault Zone, South Flank of the Uinta Mountains, Near Vernal, Utah (opens in a new tab)

  5. Piecing Together the Triassic/Jurassic Stratigraphy Along the South Flank of the Uinta Mountains, Northeast Utah: A Stratigraphic Analysis of the Bell Springs Member of the Nugget Sandstone

    … Jurassic strata along the south flank of the Uinta Mountains has been somewhat confusing because of the position of the study area between southern Wyoming, where one set of names is used, and central/southern Utah where a different set of formation names is used. The Nugget Sandstone or Glen …

    byu Repository record for Piecing Together the Triassic/Jurassic Stratigraphy Along the South Flank of the Uinta Mountains, Northeast Utah: A Stratigraphic Analysis of the Bell Springs Member of the Nugget Sandstone (opens in a new tab)

  6. Geology of the Phil Pico Mountain Quadrangle, Daggett County, Utah, and Sweetwater County, Wyoming

    … of this section of the north flank of the Uinta Mountains. Phil Pico Mountain is largely composed of the conglomeratic facies of the early Eocene Wasatch and middle to late Eocene Bridger Formations. These formations are separated by the Henrys Fork fault which has thrust Wasatch Formation …

    byu Repository record for Geology of the Phil Pico Mountain Quadrangle, Daggett County, Utah, and Sweetwater County, Wyoming (opens in a new tab)