Glad You Asked—Glacial Striations and Slickensides
What are those groovy rocks and how did they get that way?
by Carole McCalla
On a hike around Lake Blanche below Sundial Peak in Big Cottonwood Canyon, a group of hikers came across long, straight, parallel grooves on a smooth, polished rock surface. Recalling another location where they had seen similar features at the foot of the mountains north of downtown Salt Lake City, they wondered if these markings were formed in the same way. Indeed, what exactly are they and how were they formed?
Although the smooth, grooved surfaces at these two locations are similar, they were actually formed in very different ways.
Tags: Big Cottonwood Canyon, fault, gald you asked, geologic, geological, geology, glacial, glacial striations, glacier, ice-polished rock, Lake Blanche, Little Cottonwood Canyon, northeastern Utah, parallel grooves, Salt Lake County, slickensides, Sundial Peak, Survey Notes, Uinta Mountains, utah, Utah Geological Survey, wasatch fault