Tag Archive for: UGS
Kolob Canyons, Zion National Park, Washington County, Utah
Photographer: Michael Vanden Berg
Jurassic-age Navajo Sandstone forms the massive red cliffs of the often-overlooked Kolob Canyons area of Zion National Park. Hanging valleys are present where relatively small tributary streams have eroded downward at a slower rate than the larger trunk stream.
Cretaceous Mancos Shale, Uinta Basin, Utah
A research team from the Utah Geological Survey and the University of Utah presented the results of their on-going work in the Uinta Basin to members of the petroleum industry recently. Meeting in Denver on June 28, the UGS and university geologists discussed their research on the oil and gas potential of the Cretaceous Mancos Shale, which lies several thousand feet below the surface in most of the Basin. Although oil and gas from shale have made energy headlines in many states, production from the Mancos will be a challenge, due in part to its thickness compared to other U.S. shale plays. About 20 geologists and engineers representing 10 companies with interests in the Uinta Basin attended the meeting. The research is being funded by the Research Partnership to Secure Energy for America, through a contract from the U.S. Department of Energy.
See http://geology.utah.gov/emp/shalegas/cret_shalegas/index.htm for more information about the project.
Wasatch Range, Utah & Wasatch Counties, Utah
Photographer: Robert F. Biek
Framed by blooming gray rabbitbrush (Chrysothamnus nauseosus) above the east shore of Deer Creek Reservoir, Mt. Timpanogos is formed of Pennsylvanian-age, shallow- marine limestone and sandstone of the Oquirrh Formation. The small patch of snow is in Cascade Cirque, one of several glacier-carved basins on the east side of the 11,749-foot-tall mountain.
Capitol Reef National Park, Garfield County, Utah
Photographer: Paul Kuehne
The Waterpocket Fold affords a wonderful view of the geology of Grand Gulch. The Entrada Sandstone (reddish-orange rock on the right) and Navajo Sandstone (pale-orange rock on the left and middle distance) were formed in a desert environment beginning about 185 million years ago in the Jurassic Period.
Dollar Lake, High Uintas Wilderness, Duchesne County, Utah
Photographer: Mike Hylland
To the south of Dollar Lake in the Uinta Mountains, cliffs of Precambrian-age sedimentary strata rise abruptly at the head of the Henrys Fork basin. The leftmost peak lit by the morning sun is Utah’s highest mountain, Kings Peak (13,528 feet), which was named for Clarence King, first director of the U.S. Geological Survey.