Posts

POTD April 25, 2017: Yellowstone Basin

Yellowstone Basin, Uinta Mountains, Duchesne County

Photographer: Rich Emerson © 2017

 

POTD April 04, 2017: Modern dunes, Arches National Park

Modern dunes, Arches National Park
Photographer: Kent Brown © 2017

Modern dunes (foreground) consist of sand weathered from bedrock such as the Wingate Sandstone (skyline), which similarly formed from sand deposited in dunes 200 million years ago.

POTD March 28, 2017: Little Cottonwood Canyon, Salt Lake County

Little Cottonwood Canyon, Salt Lake County
Photographer: Adam McKean © 2017

Interbedded shale and quartzite of the Precambrian Big Cottonwood Formation are dramatically folded and faulted on the sheer face of Twin Peaks in Little Cottonwood Canyon. The intrusive Tertiary-age Little Cottonwood granite stock forms the light-gray, glaciated peaks in the distance.

POTD March 14, 2017: Big Cottonwood Canyon, Wasatch Range

Big Cottonwood Canyon, Wasatch Range
Photographer: Mike Hylland © 2017

The waters of Lake Blanche reflect Sundial Peak, composed of quartzite of the Big Cottonwood Formation. Rocks in this basin, which formed from sediment that accumulated along a continental margin 900 million years ago, preserve striations (parallel scratches and grooves) that record the down-valley flow of Ice Age glaciers.

POTD February 28, 2017

View east from Jackson Bottom along the Colorado River, Grand County.
Photographer: Brian Butler © 2017

POTD February 21, 2017: Goblin Valley State Park

Goblin Valley State Park

Photographer: Michael Vanden Berg © 2017

Early morning sun casts shadows on “goblins” formed within the Entrada Sandstone, which consists of sediment deposited 160 million years ago in tidal flats and coastal dunes. Erosion forms the goblins, leaving resistant sandstone boulders perched atop softer siltstone and shale layers that erode more quickly.

POTD February 07, 2017: Thor’s Hammer, Bryce Canyon National State Park

Thor’s Hammer, Bryce Canyon National State Park

Photographer: Grant Willis © 2017

Thor’s Hammer, named for the Norse God of Thunder who controlled the air and storms, is probably the best-known hoodoo in Bryce Canyon National Park, and is also the icon for the Utah Geological Survey logo. It formed as the result of differential weathering of sandstone and siltstone layers in the Claron Formation, with the softer layers weathering and eroding faster than the harder layers. The retreating escarpment that forms Bryce Canyon owes its existence to the Paunsaugunt fault, which elevated Powell Point in the distance, and which also “sank” the Sinking Ship in middle distance.

 

POTD January 31, 2017: Little Cottonwood Canyon, Wasatch Range

Little Cottonwood Canyon, Wasatch Range

Photographer: Mike Hylland © 2017

Devils Castle exposes tilted layers of limestone and dolomite of the Deseret, Gardison, and Fitchville Formations above Albion Basin at the head of Little Cottonwood Canyon. Discoveries of silver, gold, copper, lead, and zinc in the area led to establishment of the Little Cottonwood mining district and the town of Alta in the late 1800’s.