This photo shows another way that #UtahGeology can really knock you off of your feet. Don’t forget your sea legs as you look out over the vast sea of geology!
San Rafael Swell and Henry Mountains from Temple Mountain, Emery County, Utah
Photographer: Paul Kuehne; © 2014
Hey friends, we’ve finally made way with our new website! Visit geology.utah.gov to see our new look. Though, as most technical endeavors, we’ve encountered some difficulties. Switching the URLs erased our subscription list, and those who subscribed to our “New Blog,” you will have to re-subscribe. We apologize for the inconvenience, but we hope you’ll forgive us when you see this pretty picture of Utah geology.
Desolation Canyon, Uintah County, Utah
Photographer: Adam Hiscock; © 2014
The Green River forms a dramatic “gooseneck” near Sand Wash in upper Desolation Canyon. The river has incised into rocks of the Douglas Creek and Parachute Creek Members of the Tertiary-age Green River Formation, which comprises sediments that accumulated in ancient Lake Uinta.
Arches National Park, Grand County, Utah
Photographer: Gregg Beukelman; © 2014
Turret Arch viewed through North Window arch in The Windows Section of Arches National Park. The arches formed as the result of erosion through weak parts of sandstone fins composed of Jurassic-age Dewey Bridge Member of the Carmel Formation and Slick Rock Member of the Entrada Sandstone.
Colorado River, Grand County, Utah
Photographer: Adam Hiscock; © 2014
Late-winter ice still clings to the Colorado River near Big Bend, north of Moab. Boulders of Jurassic-age Wingate Sandstone and Triassic-age Chinle Formation line the banks of the river, eroded from the cliffs and ledges cut by the river as it has incised its channel over millions of years.
Zion National Park, Washington County, Utah
Photographer: Tyler Knudsen; © 2014
One of numerous slot canyons carved into Jurassic-age Navajo Sandstone in Zion National Park, Bear Trap Canyon is particularly dark and narrow. With little sunlight penetrating to the canyon floor, snow and ice often linger well into spring.