Kane County is a county in the U.S. state of Utah. As of the 2010 United States Census, the population was 7,125. Its county seat and largest city is Kanab.
A canyon, or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering.
The Grand Staircase–Escalante National Monument (GSENM) is a United States national monument protecting the Grand Staircase, the Kaiparowits Plateau, and the Canyons of the Escalante in southern Utah. It was established in 1996 by President Bill Clinton under the authority of the Antiquities Act with 1.7 million acres of land, later expanded to 1,880,461 acres (7,610 km2). In 2017, the monument's size was reduced by half in a succeeding presidential proclamation, and it was restored in 2021. The land is among the most remote in the country; it was the last to be mapped in the contiguous United States.
The Wasatch Range or Wasatch Mountains is a mountain range in the western United States that runs about 160 miles (260 km) from the Utah-Idaho border south to central Utah. It is the western edge of the greater Rocky Mountains, and the eastern edge of the Great Basin region. The northern extension of the Wasatch Range, the Bear River Mountains, extends just into Idaho, constituting all of the Wasatch Range in that state.
The Grand Staircase is an immense sequence of sedimentary rock layers that stretch south from Bryce Canyon National Park and Grand Staircase–Escalante National Monument, through Zion National Park, and into Grand Canyon National Park.
The Paria River is a tributary of the Colorado River, approximately 95 miles (153 km) long, in southern Utah and northern Arizona in the United States. It drains a rugged and arid region northwest of the Colorado, flowing through roadless slot canyons along part of its course.
The Pink Cliffs are a series of highly dissected cliffs on the Colorado Plateau in Garfield, Iron, and Kane counties in southwestern Utah, United States. Contrary to the implication of the name, the cliffs are not a single set of rock formations, but actually a geological formation that manifests itself in multiple sets of rock formations.
Little Cottonwood Canyon lies within the Wasatch-Cache National Forest along the eastern side of the Salt Lake Valley, roughly 15 miles from Salt Lake City, Utah. The canyon is part of Granite, a CDP and "Community Council" designated by Salt Lake County. The canyon is a glacial trough, carved by an alpine glacier during the last ice age, 15,000 to 25,000 years ago. A number of rare and endemic plant species are found in the canyon's Albion Basin. Mountain goats inhabit the surrounding mountains.
Grosvenor Arch is a unique sandstone double arch located within Grand Staircase–Escalante National Monument in southern Kane County, Utah, United States. It is named to honor Gilbert Hovey Grosvenor (1875–1966), a president of the National Geographic Society, publishers of the National Geographic Magazine.
Road 400 is a scenic 47-mile (76 km) dirt road in Kane County, Utah, United States that connects U.S. Route 89 (US-89) with South Kodachrome Road. The road traverses portions of Grand Staircase–Escalante National Monument offering a unique view into the heart of the Monument. This road is considered impassable in wet weather and high clearance vehicles are recommended.
Cottonwood Canyon may refer to:
The Kaiparowits Plateau is a large, elevated landform located in southern Utah, in the southwestern United States. Along with the Grand Staircase and the Canyons of the Escalante, it makes up a significant portion of the Grand Staircase–Escalante National Monument. Its extension to the southeast, Fiftymile Mountain, runs nearly to the Colorado River and Lake Powell, and is a prominent part of the northern skyline from the Glen Canyon National Recreation Area.
The Hole in the Rock Trail is a historic trail running east-southeast from the town of Escalante in southern Utah in the western United States. The Mormon trailblazers who established this trail crossed the Colorado River and ended their journey in the town of Bluff. The Hole-in-the-Rock expedition established the trail in 1879. The trail is located within the borders of the Grand Staircase–Escalante National Monument, the adjacent Glen Canyon National Recreation Area and federal Bureau of Land Management (BLM) public land to the east of the Colorado River. A geologic feature called the Hole in the Rock gave the trail its name. A modern unpaved road called the Hole-in-the-Rock Road closely follows this historic trail to the point where it enters the Glen Canyon National Recreation Area. The modern road is an important access route for visiting the Canyons of the Escalante and the Devils Garden. The trail is listed on the National Register of Historic Places, being added to that list in 1982.
The Canyons of the Escalante is a collective name for the erosional landforms created by the Escalante River and its tributaries—the Escalante River Basin. Located in southern Utah in the western United States, these sandstone features include high vertical canyon walls, numerous slot canyons, waterpockets, domes, hoodoos, natural arches and bridges. This area—extending over 1,500 square miles (3,885 km2) and rising in elevation from 3,600 ft (1,097 m) to over 11,000 ft (3,353 m)—is one of the three main sections of the Grand Staircase–Escalante National Monument, and also a part of the Glen Canyon National Recreation Area, with Capitol Reef National Park being adjacent to the east.
Coyote Gulch is a tributary of the Escalante River, located in Garfield and Kane Counties in southern Utah, in the western United States. Over 25 mi (40 km) long, Coyote Gulch exhibits many of the geologic features found in the Canyons of the Escalante, including high vertical canyon walls, narrow slot canyons, domes, arches, and natural bridges. The upper sections of Coyote Gulch are located within the Grand Staircase–Escalante National Monument, while its lower sections are located in the Glen Canyon National Recreation Area.
Fortymile Gulch and Willow Gulch are tributaries of the Escalante River, located in Kane County in southern Utah, in the western United States. With a combined length of over 20 miles (30 km), they exhibit many of the geologic features found in the Canyons of the Escalante, including high vertical canyon walls, water pools, narrow slot canyons, domes, and arches. Popular recreational destinations, they are located within the Grand Staircase–Escalante National Monument.
Harris Wash is a long tributary of the Escalante River located in Garfield County in southern Utah, in the western United States. Over 40 miles (64 km) long with a drainage of 270 square miles (700 km2), it exhibits many of the geologic features found in the Canyons of the Escalante, including high vertical canyon walls and narrow slot canyons. A popular recreational destination and a historic transportation route, it is located within the Grand Staircase–Escalante National Monument.
Diabloceratops is an extinct genus of centrosaurine ceratopsian dinosaur that lived approximately 81.4-81 million years ago during the latter part of the Cretaceous Period in what is now Utah, in the United States. Diabloceratops was a medium-sized, moderately built, ground-dwelling, quadrupedal herbivore, that could grow up to an estimated 4.5 metres (15 ft) in length and 1.3 metric tons in body mass. At the time of its discovery, it was the oldest-known ceratopsid, and first centrosaurine known from latitudes south of the U.S. state of Montana. The generic name Diabloceratops means "devil-horned face," coming from Diablo, Spanish for "devil," and ceratops, Latinized Greek for "horned face." The specific name honors Jeffrey Eaton, a paleontologist at Weber State University and long time friend of the lead author Jim Kirkland. Eaton had a big role in establishing the Grand Staircase-Escalante National Monument where the specimen was found. The type species, Diabloceratops eatoni, was named and described in 2010 by James Ian Kirkland and Donald DeBlieux.
Mollie's Nipple or Molly's Nipple is the name given to as many as seven peaks, at least one butte, at least one well, and some other geological features in Utah. Some sources claim there are eleven geological features in Utah that bear this name. At least some of those names are attributed to John Kitchen – a pioneer of an early exploration of Utah, who named them to commemorate a nipple of his wife Molly.
Buckskin Mountain is a 16-mile (26 km) mountain ridge that spans from Coconino County, Arizona to Kane County, Utah in the United States, that is divided almost equally between the two counties.
