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Cottonwood Canyon (Kane County, Utah)
Cottonwood Canyon is a canyon in central Kane County, Utah United States. Description The canyon is a water-carved canyon A canyon (; archaic British English spelling: ''cañon''), gorge or chasm, 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 t ... that has eroded along weak locations in the Earth's crust at the joins between major geological regions. To the east are the lower steps of the Grand Staircase, which is not visible from the road, and to the north is the Kaiparowits Plateau. Retriev ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cottonwood Canyon Road
Cottonwood Canyon Road (also known as Road 400, Cottonwood Canyons Scenic Backway and K7000) is a scenic or dirt road that traverses Cottonwood Canyon in Kane County, Utah. The drive begins in Cannonville, just off Utah State Route 12, continues southward through Grand Staircase–Escalante National Monument, and eventually connects to U.S. Route 89. The road was originally constructed as a maintenance road for power lines following the canyon. The drive takes roughly two hours without stops. There are visitor centers in Cannonville in the north, and in Big Water near the southern terminus. Scenic attractions include Navajo Sandstone walls, Grosvenor Arch, and Kodachrome Basin State Park. The road allows access to hiking trails, such as Cottonwood Wash Narrows, Yellow Rock, Hackberry Canyon, and Cottonwood Canyon Narrows. Road Condition The road is mostly an unpaved, except for nine miles between Cannonville and Kodachrome Basin State Park. It's considered impass ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kane County, Utah
Kane County is a county in the U.S. state of Utah. As of the 2020 United States census, the population was 7,667. Its county seat and largest city is Kanab. History The county was created on January 16, 1864, by the old federal Utah Territory (1850–1896) territorial legislature, with areas partitioned off from earlier Washington County. It was named for Col. Thomas L. Kane (1822–1883), a friend of the Latter Day Saint (Mormons) settlers when they first arrived westward, led by patriarch Brigham Young (1801–1877), in the 1840s and 1850s. The county boundary was readjusted later, first in 1869, when a portion was returned back to Washington County; second in 1880, when San Juan County was partitioned off and created; and third, in 1883, when additional portions were partitioned from Kane and added to Iron and back to Washington counties. Geography Kane County lies on the south line of the state of Utah. Its south border abuts the northern border of the state of A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utah
Utah is a landlocked state in the Mountain states, Mountain West subregion of the Western United States. It is one of the Four Corners states, sharing a border with Arizona, Colorado, and New Mexico. It also borders Wyoming to the northeast, Idaho to the north, and Nevada to the west. In comparison to all the U.S. states and territories, Utah, with a population of just over three million, is the List of U.S. states and territories by area, 13th largest by area, the List of U.S. states and territories by population, 30th most populous, and the List of U.S. states by population density, 11th least densely populated. Urban development is mostly concentrated in two regions: the Wasatch Front in the north-central part of the state, which includes the state capital, Salt Lake City, and is home to roughly two-thirds of the population; and Washington County, Utah, Washington County in the southwest, which has approximately 180,000 residents. Most of the western half of Utah lies in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyon
A canyon (; archaic British English spelling: ''cañon''), gorge or chasm, 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. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grand Staircase
The Grand Staircase is an immense sequence of sedimentary rock layers that stretches south from Bryce Canyon National Park and Grand Staircase–Escalante National Monument, through Zion National Park, and into Grand Canyon National Park. Characterization In the 1870s, geologist Clarence Dutton first conceptualized this region as a huge stairway ascending out of the bottom of the Grand Canyon northward with the cliff edge of each layer forming giant steps. Dutton divided this layer cake of Earth history into five steps from the youngest (uppermost) rocks: * Pink Cliffs * Grey Cliffs * White Cliffs * Vermilion Cliffs * Chocolate Cliffs Since then, modern geologists have further divided Dutton's steps into individual rock formations. Formations in the Grand Staircase starting with the youngest (uppermost) rocks: * Claron Formation * Kaiparowits Formation * Wahweap Formation * Straight Cliffs Formation * Tropic Shale * Dakota Sandstone * Carmel Formation * Temple Cap ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaiparowits Plateau
Location of the Kaiparowits Plateau within Utah 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. Geography 350px, The Straight Cliffs, looking northwest from the eastern end of Fiftymile Mountain. Roughly triangular in shape, the Kaiparowits Plateau extends for over from near the town of Escalante in Garfield County, to the south and southwest through Kane County and nearly to the border with Arizona. At its southeastern end, the plateau rises from Lake Powell nearly to an elevation of . The northeastern edge of the plateau is defined by the Straight Clif ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Canyons And Gorges In Utah
This is a partial list of canyons in the U.S. state of Utah along with any rivers, roads, and other features (such as rail lines) that pass through them. See also External links {{DEFAULTSORT:Canyons and gorges in Utah Canyons and gorges of Utah, Lists of landforms of Utah, Canyons Lists of valleys, Utah ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyons And Gorges Of Utah
A canyon (; archaic British English spelling: ''cañon''), gorge or chasm, 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. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
