Tag Archive for: utah
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.
On April 18, 2013, four geologists from the Hazards Program of the Utah Geological Survey flew along the Wasatch Front in a Utah Air National Guard Blackhawk helicopter. The flight was part of the Great Utah ShakeOut 2013 earthquake drill, as well as an opportunity to take high-resolution photos of the fault scarps along the Front from the air. The four geologists were Adam Hiscock, Gregg Buekelman, Mike Hylland, and Adam McKean. It was a freezing cold day in April! Over 1200 photos were taken from the air.
Adam McKean, Mike Hylland, Gregg Buekelman, and Adam Hiscock
Southeast of Salt Lake City, Salt Lake County, Utah
Photographer: Michael Vanden Berg
The White Pine rock slide covers the floor of Little Cottonwood Canyon with boulders of granitic rock of the Tertiary-age Little Cottonwood stock. These rocks broke loose from the north side of the glacially-carved canyon several thousand years ago.