Bryce Canyon

Bryce Canyon National Park is a national park located in southwestern Utah in the United States. Contained within the park is Bryce Canyon. Despite its name, this is not actually a canyon, but rather a giant natural amphitheater created by erosion along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to its geological structures, called hoodoos, formed from wind, water, and ice erosion of the river and lakebed sedimentary rocks. The red, orange and white colors of the rocks provide spectacular views to visitors. Bryce is at a much higher elevation than nearby Zion National Park and the Grand Canyon. The rim at Bryce varies from 8,000 to 9,000 feet (2,400 to 2,700 m), whereas the south rim of the Grand Canyon sits at 7,000 feet (2,100 m) above sea level.

The Bryce area was settled by Mormon pioneers in the 1850s and was named after Ebenezer Bryce, who homesteaded in the area in 1874.[1] The area around Bryce Canyon became a U.S. National Monument in 1923 and was designated as a national park the next year. The park covers 56 square miles (145 km2) and receives relatively few visitors compared to Zion Canyon and the Grand Canyon, largely due to its remote location. The town of Kanab, Utah, is situated at a central point between these three parks.

The national park lies within the Colorado Plateau geographic province of North America and straddles the southeastern edge of the Paunsagunt Plateau west of the Paunsagunt Fault (Paunsagunt is Paiute for "home of the beaver").[5] Park visitors arrive from the plateau part of the park and look over the plateau's edge toward a valley containing the fault and the Paria River just beyond it (Paria is Paiute for "muddy or elk water"). The edge of the Kaiparowits Plateau bounds the opposite side of the valley.

Bryce Canyon was not formed from erosion initiated from a central stream, meaning it technically is not a canyon. Instead headward erosion has excavated large amphitheater-shaped features in the Cenozoic-aged rocks of the Paunsagunt Plateau.[5] This erosion exposed delicate and colorful pinnacles called hoodoos that are up to 200 feet high. A series of amphitheaters extends more than 20 miles north-to-south within the park. The largest is Bryce Amphitheater, which is 12 miles long, 3 miles wide and 800 feet deep. A nearby example of amphitheaters with hoodoos in the same formation but at a higher elevation, is in Cedar Breaks National Monument, which is 25 miles to the west on the Markagunt Plateau

Weather

Latest Bryce, Utah, weather

History

Little is known about early human habitation in the Bryce Canyon area. Archaeological surveys of Bryce Canyon National Park and the Paunsaugunt Plateau show that people have been in the area for at least 10,000 years. Basketmaker-period Anasazi artifacts several thousand years old have been found south of the park. Other artifacts from the Pueblo-period Anasazi and the Fremont culture (up to the mid-12th century) have also been found.

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Guided tours of the Grand Canyon and the Southwest.