Capitol Reef National Park
History
Geologic History
The Waterpocket Fold defines Capitol Reef National Park. A nearly 100-mile-long warp in the earth's crust, the fold is a classic monocline: a regional fold with one very steep side in an area of otherwise nearly horizontal rock layers. The Waterpocket Fold formed between 50 million and 70 million years ago when a major geologic shift in western North America reactivated an ancient buried fault. When the fault moved, the overlying rock layers were pushed up, bent and draped into the monocline. The fold is also known as Capitol Reef: "capitol" for the white domes of Navajo Sandstone that resemble rotundas, and "reef" for the rocky cliffs that are a barrier to travel, like an ocean reef.
Almost 10,000 feet of sedimentary strata are found in the Capitol Reef area. These rocks range in age from Permian to Cretaceous and this geologic layer cake records nearly 200 million years of history. Ancient environments revealed in the rock include rivers and swamps (Chinle and Moenkopi formations), Sahara-like deserts (Navajo and Wingate Sandstone) and shallow ocean (Mancos Shale). Cathedral Valley's freestanding monoliths are carved out of Entrada Sandstone, which was originally deposited as sandy mud on a tidal flat. Some of the cathedrals are capped by thin, hard beds of the Curtis Formation, a greenish-gray marine sandstone.
Most of the erosion that carved today's landscape occurred after the uplift of the Colorado Plateau some time within the last 20 million years. Water was the primary erosional agent; wind was a secondary influence. Today, both elements, plus the pull of gravity—in the form of rock falls or rock creep—continue to shape Capitol Reef's majestic domes, arches and canyons.
Human History
The "pockets" of the Waterpocket Fold are natural basins capable of holding thousands of gallons of rainwater. It was these water pockets and the water of the Fremont River and Sulphur Creek that attracted early human settlers. The Fremont Indian Culture began around A.D. 700. People lived here for about 600 years, farming, hunting game and gathering wild foods. Around A.D. 1300, they abandoned the area, perhaps because a prolonged drought made agriculture impossible. The Fremont people are known for their enigmatic rock writings. They left petroglyphs (carvings in rock) and -pictographs (paintings on rocks and stone walls) through-out the park. Their meaning remains a mystery.
Several hundred years passed before Capitol Reef saw any more permanent human habitation. In 1880, Mormon settlers established a community near the site of the present visitor center and campground. Using the water from the Fremont River for irrigation, they planted crops and orchards. They also grazed cattle. The pioneers lived here for less than 100 years; although President Franklin Roosevelt proclaimed the area a National Park Service national monument in 1937, the last residents left in 1969. Congress designated Capitol Reef a national park in 1971.
Still, the sandstone, limestone and shale stay on continuing to faithfully record the Earth's ever-changing environment.
Capitol Reef In Depth
- Capitol Reef National Park
- 5 Things to See in Capitol Reef
- Activities
- Flora & Fauna
- Getting To Capitol Reef
- History
- Sights To See
- Visitor Services
- Animals
- Geology
- History
- In A Nutshell
- Just For Kids
- Natural World
- Park Regulations & Safety
- Photography
- Planning Your Visit
- Plants
- Preservation
- Sights to See
- Things To Do
- Visitor Services
- Walking & Hiking
- Who's Who at the Park
- Capitol Reef Map
- Capitol Reef Photos
- Recent Capitol Reef News
News from the Parks
November 21, 2008 - 10:01am
I always look forward to getting my Frommer's newsletter every week. Not only are they budget travel saavy, they inspire me to get out there no matter the weather! Here are their top five picks for cozy camping.
November 21, 2008 - 9:56am
The Nisqually Road in Mount Rainier National Park will reopen today, a day earlier than expected. The road, and the park, have been closed since Nov. 12 when Kautz Creek jumped its banks and flooded the main road into the park.
November 21, 2008 - 9:55am
Reporting from Glacier National Park -- No one knew what to expect on the trail to Grinnell Glacier one late summer morning, but a second bull moose less than an hour out was hardly a good sign. During September and October -- mating season -- it's always best to give the spindly-legged animals plenty of room.
November 21, 2008 - 9:07am
An upcoming National Park Service (NPS) rule change could greatly benefit mountain bicycling by improving the administrative process for opening trails to bicycles. IMBA has been asking the agency to revise its policies since 1992, because the current "special regulations" process is needlessly cumbersome and treats bicycles like motorized vehicles.
November 21, 2008 - 8:55am
On our recent trip to Hawaii we had a feeling that things were less busy than usual. Now there are some numbers to back up our hunch: The national parks in the state saw a drop in attendance of more than 50,000 visitors during the month of October.
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