Capitol Reef National Park

 

Capitol Reef National Park was the 4thof the “Big 5” National Parks that we have seen.  The Park is most important geological feature is a wrinkle in the earth’s crust that extends for nearly 100 miles from Thousand Lake Mountain to Lake Powell. It was created over a long period of time by 3 gradual but powerful forces: deposition, uplift, and erosion. The result is a stunning example of what geologists call a monocline, or one-sided fold in the crust of the earth in what are otherwise largely horizontal rock layers. This fold runs north and south through the Utah desert. Waterpocket foldwas form about 65 million years ago when the earth’s surface buckled upwards. This was around the time the dinosaurs went extinct.

The climate in the region changed fantastically over millions of years. During the past 280 million years ago this region changed from ocean to desert to swamp and river bed. During this time 10,000 feet of sedimentary rock consisting of limestone, sandstone, and shale was deposited.

That was followed by uplift between 50 and 70 million years ago when an ancient fault was reactivated during tectonic activity. This lifted the land to the west up by 7,000 feet higher than the land in the east. The land did not crack, rather the layers folded over the fault line. 20 million years ago it was uplifted again.

After that erosive forces shaped the landscape. Much of this sculpture work occurred between 1 and 6 million years ago. Moving water and gravity were the main erosive forces. Powerful rains, flash floods and awesome freeze/thaw cycles loosen and crack the rock after which much of it is washed away. Often this left behind stunning canyons, cliffs, domes, and natural bridges or arches made of rock.

The original European explorers thought it looked like an ocean reef and thought its white domes looked like the American capitol and hence gave it the name Capitol Reef.

People have lived here for long periods of time.  As a result the park contains Ancestral Puebloan petroglyphs and a preserved Mormon homestead.

Charles Dutton the famous geologist who first scientifically explored much of the American Southwest in the 1880s described it like this, “…the light seems to flow or shine out of the rock rather than to be reflected from it.”

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