Bryce Canyon National Park is an American national park located in southwestern Utah. The major feature of the park is Bryce Canyon, which despite its name, is not a canyon, but a collection of giant natural amphitheaters along the eastern side of the Paunsaugunt Plateau. Bryce is distinctive due to geological structures called hoodoos, formed by frost weathering and stream erosion of the river and lake bed sedimentary rock. The red, orange, and white colors of the rocks provide spectacular views for park visitors. Bryce Canyon National Park is much smaller and sits at a much higher elevation than nearby Zion National Park. The rim at Bryce varies from 8,000 to 9,000 feet.
Rainbow Bridge is a natural arch in southern Utah, United States. With a span of 275 feet (84 m), as reported in 1974 by the Bureau of Reclamation, and height of 290 feet (88 m), it is one of the largest natural arches in the world. At the top it is 42 feet (13 m) thick and 33 feet (10 m) wide. The bridge, which is of cultural importance to a number of area Native American tribes, has been designated a Traditional Cultural Property by the National Park Service. Rainbow Bridge National Monument was protected in 1910, and it is administered by Glen Canyon National Recreation Area.
Capitol Reef National Park is an American national park in south-central Utah. The park is approximately 60 miles (100 km) long on its north–south axis and just 6 miles (10 km) wide on average. The park was established in 1971 to preserve 241,904 acres of desert landscape and is open all year, with May through September being the highest visitation months.
The Colorado Plateau, also known as the Colorado Plateau Province, is a physiographic and desert region of the Intermontane Plateaus, roughly centered on the Four Corners region of the southwestern United States. This province covers an area of 336,700 km2 (130,000 mi2) within western Colorado, northwestern New Mexico, southern and eastern Utah, northern Arizona, and a tiny fraction in the extreme southeast of Nevada. About 90% of the area is drained by the Colorado River and its main tributaries: the Green, San Juan, and Little Colorado. Most of the remainder of the plateau is drained by the Rio Grande and its tributaries.
Glen Canyon National Recreation Area is a national recreation area and conservation unit of the United States National Park Service that encompasses the area around Lake Powell and lower Cataract Canyon in Utah and Arizona, covering 1,254,429 acres (5,076.49 km2) of mostly rugged high desert terrain. The recreation area is named for Glen Canyon, which was flooded by the Glen Canyon Dam, completed in 1966, and is now mostly submerged beneath the waters of Lake Powell.
The exposed geology of the Capitol Reef area presents a record of mostly Mesozoic-aged sedimentation in an area of North America in and around Capitol Reef National Park, on the Colorado Plateau in southeastern Utah.
The Wingate Sandstone is a geologic formation in the Glen Canyon Group of the Colorado Plateau province of the United States which crops out in northern Arizona, northwest Colorado, Nevada, and Utah.
The Kayenta Formation is a geological formation in the Glen Canyon Group that is spread across the Colorado Plateau province of the United States, including northern Arizona, northwest Colorado, Nevada, and Utah. Traditionally has been suggested as Sinemurian-Pliensbachian, but more recent dating of detrital zircons has yielded a depositional age of 183.7 ± 2.7 Ma, thus a Pliensbachian-Toarcian age is more likely. A previous depth work recovered a solid "Carixian" age from measurements done in the Tenney Canyon. More recent works have provided varied datations for the layers, with samples from Colorado and Arizona suggesting 197.0±1.5-195.2±5.5 Ma, while the topmost section is likely Toarcian or close in age, maybe even recovering terrestrial deposits coeval with the Toarcian Oceanic Anoxic Event. This last age asignation also correlated the Toarcian Vulcanism on the west Cordilleran Magmatic Arc, as the number of grains from this event correlate with the silt content in the sandstones of the upper layers.
Arches National Park is a national park in eastern Utah, United States. The park is adjacent to the Colorado River, 4 mi (6 km) north of Moab, Utah. The park contains more than 2,000 natural sandstone arches, including the well-known Delicate Arch, which constitute the highest density of natural arches in the world. It also contains a variety of other unique geological resources and formations. The national park lies above an underground evaporite layer or salt bed, which is the main cause of the formation of the arches, spires, balanced rocks, sandstone fins, and eroded monoliths in the area.
Zion National Park is an American national park located in southwestern Utah near the town of Springdale. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park has a unique geography and a variety of life zones that allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals, and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches. The lowest point in the park is 3,666 ft (1,117 m) at Coalpits Wash and the highest peak is 8,726 ft (2,660 m) at Horse Ranch Mountain. A prominent feature of the 229-square-mile (590 km2) park is Zion Canyon, which is 15 miles (24 km) long and up to 2,640 ft (800 m) deep. The canyon walls are reddish and tan-colored Navajo Sandstone eroded by the North Fork of the Virgin River. The park attracted 5 million visitors in 2023.
Bridge Mountain is a 6,803-foot (2,074 m) mountain made of Navajo Sandstone in Zion National Park in Washington County, of southwest Utah, United States.
The West Temple is a prominent 7,810-foot mountain summit composed of Navajo Sandstone in Zion National Park in Washington County of Utah, United States. The West Temple, the highest feature in Zion Canyon, was originally called "Temp-o-i-tin-car-ur" meaning "Mountain without a trail" by the Paiute people. It was called Steamboat Mountain by local Mormon settlers before 1934, when the USGS officially changed it to its present name, which was applied by John Wesley Powell during his explorations in 1872. West Temple is situated two miles northwest of Springdale, Utah, one mile northeast of Mount Kinesava, and two miles west of the park headquarters. It is one of the notable landmarks in the park. The nearest higher peak is Windy Peak, 10.46 miles (16.83 km) to the north. Precipitation runoff from the mountain drains into tributaries of the Virgin River.
Chimney Rock is a 6,420-foot (1,960 m) summit in Capitol Reef National Park in Wayne County, Utah, United States. This landmark is situated 2.5 mi (4.0 km) northwest of the park's visitor center, towering over 300 feet (91 m) above Utah State Route 24. Chimney Rock is also 2.5 mi (4.0 km) northwest of another of the park's landmarks, The Castle. Precipitation runoff from this feature ends up in the Colorado River drainage basin. The Chimney Rock Trail is a 3.5-mile loop trail that takes hikers to a view of Chimney Rock from above Mummy Cliffs.
Ferns Nipple is a 7,065-foot (2,153-meter) elevation summit located in Capitol Reef National Park, in Wayne County of Utah, United States. This iconic landmark is situated 4 mi (6.4 km) southeast of the park's visitor center. Precipitation runoff from this feature is drained by tributaries of the Fremont River, which in turn is within the Colorado River drainage basin. Folklore attributes this geological feature's naming to outlaw Butch Cassidy and his favored girlfriend named Fern.
Pectols Pyramid is a 6,211-foot (1,893-meter) elevation summit located in Capitol Reef National Park, in Wayne County of Utah, United States. This iconic landmark is situated 2 mi (3.2 km) southeast of the park's visitor center, 1 mi (1.6 km) south of Navajo Dome, and 0.5 mi (0.80 km) southwest of Capitol Dome. Precipitation runoff from this feature is drained by the Fremont River, which in turn is within the Colorado River drainage basin. This geological feature's name honors Ephraim Portman Pectol (1875–1947), booster and founder of what would become Capitol Reef National Monument in 1937.
Capitol Dome is a 6,120-foot-elevation (1,870 m) summit located in Capitol Reef National Park, in Wayne County, Utah, United States. This iconic landmark is situated 2.5 miles (4.0 km) east of the park's visitor center, and 0.85 mi (1.37 km) southeast of Navajo Dome. Precipitation runoff from this feature is drained by tributaries of the Fremont River, which in turn is within the Colorado River drainage basin. It towers 800 feet (240 m) above the Fremont River and State Route 24. This geological feature's dome-like shape reminded early explorers and settlers of the dome of the United States Capitol in Washington D.C., and lent the park its name.
Navajo Dome is a 6,489-foot (1,978-meter) elevation summit located in Capitol Reef National Park, in Wayne County of Utah, United States. This iconic landmark is situated 2 mi (3.2 km) east of the park's visitor center, and 0.85 mi (1.37 km) northwest of Capitol Dome. Precipitation runoff from this feature is drained by the Fremont River, which in turn is within the Colorado River drainage basin. It rises 1,100 feet above the Fremont River and Highway 24, from which it is visible. The approach to the base of this peak is made via the Hickman Bridge Trail. This geological feature's descriptive name derives from its Navajo Sandstone composition and dome-like shape.
Eph Hanks Tower is a 6,540-foot (1,990-meter) elevation summit located in Capitol Reef National Park, in Wayne County of Utah, United States. This landmark is situated 8 mi (13 km) southeast of the park's visitor center, 3.5 mi (5.6 km) south-southeast of Ferns Nipple, and 1.4 mi (2.3 km) south-southwest of Golden Throne, at the mouth of Capitol Gorge where the Capitol Reef Scenic Drive road ends. It towers 900 feet above the picnic area below its north aspect. Precipitation runoff from this feature is drained by Capitol Wash and Pleasant Creek, a tributary of the Fremont River, which in turn is within the Colorado River drainage basin. This geological feature is named after Ephraim Knowlton Hanks (1826–1896), a Mormon pioneer and first permanent settler in the Capitol Reef area, who with his family homesteaded in the Pleasant Creek area of Capitol Reef in 1881. Ephraim Hanks' Floral Ranch on Pleasant Creek supposedly offered a safe retreat for polygamists along the Mormon underground railroad.
Cathedral Mountain is a 6,924-foot (2,110 m) summit located in Capitol Reef National Park, in Wayne County of Utah, United States.
Cassidy Arch is a large natural arch located in Capitol Reef National Park, Utah. The formation is considered one of the more popular attractions in the park. The arch sits 400 feet above the Scenic Drive and the Grand Wash Trail.
