Geology in Zion National Park

Geology

Zion is located at the western edge of the Colorado Plateau.

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Geology Details

Zion National Park is located at the western edge of the Colorado Plateau, which over the millennia has been uplifted, tilted and eroded into a series of stepped cliffs called the Grand Staircase. Slowly, this uplift caused the Zion area to rise from near sea level to over 10,000 feet in some places. When Zion was still a low, flat basin 240 million years ago, it was filled with sand, gravel and mud carried by streams from the surrounding mountains. Over time, layers of these materials were compacted into stone, while the rising land and a changing climate transformed a shallow sea into a desert. Later in its history, a landslide dammed the Virgin River, forming a lake. The river eventually breached the dam and the lake drained, leaving behind a flat-bottomed valley. You can still see evidence of these changes while touring Zion National Park.

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Learn About the Park

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Compare nearby parks around Geology when deciding whether to expand the route after this stop.

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Nearby Points of Interest Around Geology

Use nearby POIs to quickly expand your options beyond Geology while the map context is still fresh.

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Jessie Benton Fremont

An early advocate of the Park, without her work behind the scenes, Yosemite might not exist today.

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Traffic & Travel Tips

Plan ahead!

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ZERO LANDFILL IN THE PARKS:

THE YOSEMITE, GRAND TETON AND DENALI PROGRAM

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30-Minute Helicopter Ride

Fly rim-to-rim in a half-hour.

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50-Minute Airplane Tour

The ultimate Canyon airplane tour.

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50-Minute Helicopter Tour

Offering aerial tours of the North and South Rims as well as the Grand Canyon's East Rim.