#BRYCE NATIONAL PARK SOFTWARE#
#BRYCE NATIONAL PARK SERIES#

At least one older Paiute said his culture called the hoodoos Anka-ku-wass-a-wits, which is Paiute for 'red painted faces'. They believed that hoodoos were the Legend People whom the trickster Coyote turned to stone. The Paiute in the area developed a mythology surrounding the hoodoos (pinnacles) in Bryce Canyon. These Native Americans hunted and gathered for most of their food but also supplemented their diet with some cultivated products. The Paiute Indians moved into the surrounding valleys and plateaus in the area around the same time that the other cultures left. Other artifacts from the Pueblo-period Anasazi and the Fremont culture (up to the mid-12th century) have also been found. Several-thousand-year-old Basketmaker-period Anasazi artifacts have been found south of the park. 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. Little is known about early human habitation in the Bryce Canyon area. Petroglyphs in Bryce Canyon indicate the presence of people in the area several thousand years ago, but little is known about them. Cope Canyon, where it exits the park in the north-east section is the lowest part of the park at 6,600 feet (2,011 m). From there Aquarius Plateau, Bryce Amphitheater, Henry Mountains, the Vermilion Cliffs, and the White Cliffs can be seen. The highest part of the park at 9,105 feet (2,775 m), Rainbow Point, is at the end of this scenic drive. The largest is Bryce Amphitheater, which is 12 miles long (19 km), 3 miles wide (5 km) and 800 feet deep (240 m).

#BRYCE NATIONAL PARK SERIES#

A series of amphitheaters extend more than 20 miles (30 km) within the park. This erosion exposed delicate and colorful pinnacles called hoodoos that are up to 200 feet (60 m) high. Instead headward erosion has excavated large amphitheater-shaped features in the Cenozoic-aged rocks of the Paunsagunt Plateau. The edge of the Kaiparowitz Plateau bounds the opposite side of the valley.Д«ryce Canyon was not formed from erosion initiated from a central stream, meaning it technically is not a canyon. 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 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'). A nearby example very similar to Bryce Canyon but at a higher elevation is in Cedar Breaks National Monument. The weather in Bryce Canyon is therefore cooler and the park receives more precipitation.

#BRYCE NATIONAL PARK SOFTWARE#

The national park also lends its name to Bryce, the 3D modeling software which specialises in rendering this kind of rugged landscape.Д«ryce Canyon follows a meandering course, oriented roughly north-south.Д«ryce Canyon National Park is located in southern Utah about 50 miles (80 km) northeast and 1000 feet (300 m) higher than Zion National Park. The town of Kanab, Utah is situated at a central point between these three parks.

The park receives relatively few visitors compared to Zion Canyon and the Grand Canyon, largely due to its remote location. The area around Bryce Canyon became a United States national monument in 1924 and was designated as a national park in 1928. The canyon area was settled by Mormon pioneers in the 1850s and was named after Ebenezer Bryce, who homesteaded in the area in 1875. The area therefore has a very different ecology and climate, and thus offers a contrast for visitors to the region (who often visit all three parks in a single vacation). The rim at Bryce varies from 8,000 to 9,000 feet (2400 to 2700 m), whereas the south rim of the Grand Canyon sits at 7,000 feet (2100 m) above sea level.

The red, orange and white colors of the rocks provide spectacular views.Д«ryce is at a much higher elevation than nearby Zion National Park and the Grand Canyon. Bryce is distinctive due to its unique geological structures, called hoodoos, formed from wind, water, and ice erosion of the river and lakebed sedimentary rocks. 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. Contained within the park is Bryce Canyon. Bryce Canyon National Park is a national park located in southwestern Utah in the United States.

Bryce national park