Tag Archive for: Utah Geology
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.
Fishlake National Forest, Piute County, Utah
Photographer: Tyler Knudsen
Storm clouds gather over Mount Belknap (12,137 feet) in the Tushar Mountains, Utah’s third-highest range. The smooth, rounded slopes of this summit ridge are composed of easily eroded volcanic ash and lava flows. The mountains are part of the eruptive center of the Marysvale volcanic field, an area of intense volcanic activity between 32 and 22 million years ago.
San Rafael Swell, Sevier County
Photographer: Robert F. Biek
Alluvial and wind-blown sediment partly conceals the Jurassic-age Entrada Sandstone in the Last Chance Desert, which occupies the axis of the Last Chance anticline. The narrow, jagged, black ridge at the center of the photo is a basaltic dike of probable late Tertiary age (3 to 5 million years old) that intrudes the Entrada Sandstone.
If you are interested in learning about Utah dinosaurs, you might like this blog.
http://phenomena.