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Cedar Mesa
Cedar Mesa is a plateau in San Juan County in the southeastern portion of the U.S. state of Utah. It extends from Elk Ridge in the north, Comb Wash to the east, the gorge of the San Juan River to the south, and Grand Gulch to the west, an area of over . The center of the mesa is located at approximately 37°26'N and 109°55'W, at an elevation of . The surrounding terrain has a typical elevation of just Most of Cedar Mesa is included in the newly declared (2016) Bears Ears National Monument. This large difference in elevation has led to the formation of numerous canyons, cliffs, and other erosional features on the edges of the mesa. To the east are several canyons draining into Comb Wash, including Arch, Texas, Mule, Owl, Fish, McCloyd, and Road Canyons. Scattered throughout these canyons are cliff dwellings of the Ancient Puebloans. To the southeast is an eroded area called the Valley of the Gods, and to the southwest is a deep gorge of the San Juan River, called the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of San Juan County, Utah
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, Stratum, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hill A hill is a landform that extends above the surrounding terrain. It often has a distinct Summit (topography), summit. Terminology The distinct ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Formations Of Utah
Rock most often refers to: * Rock (geology), a naturally occurring solid aggregate of minerals or mineraloids * Rock music, a genre of popular music Rock or Rocks may also refer to: Places United Kingdom * Rock, Caerphilly, a location in Wales * Rock, Cornwall, a village in England * Rock, County Tyrone, a village in Northern Ireland * Rock, Devon, a location in England * Rock, Neath Port Talbot, a location in Wales * Rock, Northumberland, a village in England * Rock, Somerset, a location in Wales * Rock, West Sussex, a hamlet in Washington, England * Rock, Worcestershire, a village and civil parish in England United States * Rock, Kansas, an unincorporated community * Rock, Michigan, an unincorporated community * Rock, West Virginia, an unincorporated community * Rock, Rock County, Wisconsin, a town in southern Wisconsin * Rock, Wood County, Wisconsin, a town in central Wisconsin Elsewhere * Corregidor, an island in the Philippines also known as "The Rock" * Jamaica, an isla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesas Of Utah
A mesa is an isolated, flat-topped elevation, ridge or hill, which is bounded from all sides by steep escarpments and stands distinctly above a surrounding plain. Mesas characteristically consist of flat-lying soft sedimentary rocks capped by a more resistant layer or layers of harder rock, e.g. shales overlain by sandstones. The resistant layer acts as a caprock that forms the flat summit of a mesa. The caprock can consist of either sedimentary rocks such as sandstone and limestone; dissected lava flows; or a deeply eroded duricrust. Unlike ''plateau'', whose usage does not imply horizontal layers of bedrock, e.g. Tibetan Plateau, the term ''mesa'' applies exclusively to the landforms built of flat-lying strata. Instead, flat-topped plateaus are specifically known as '' tablelands''.Duszyński, F., Migoń, P. and Strzelecki, M.C., 2019. ''Escarpment retreat in sedimentary tablelands and cuesta landscapes–Landforms, mechanisms and patterns.'' ''Earth-Science Reviews, no. 102890 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cedar Mesa Sandstone
Cedar Mesa Sandstone (also known as the Cedar Mesa Formation) is a sandstone memberThe Cutler Formation is sometimes classified as the Cutler Group, in which case Cedar Mesa Sandstone is classified as a formation rather than a member. of the Cutler Formation, found in southeast Utah, southwest Colorado, northwest New Mexico, and northeast Arizona. Description The Cedar Mesa Sandstone consists mainly of red and white sandstone showing cross-bedding typical of an eolian sandstone. The thick beds of cross-bedded sandstone are separated by thin layers of siltstone or other softer rock that erodes more easily, forming horizontal recesses. These have been traced for over and contain rhizoliths (fossil roots) and other indications that a thin soil layer developed. At its type location at Cedar Mesa near the San Juan River in Utah, the sandstone is to over thick. Drill holes near Glen Canyon have penetrated more than of Ceder Mesa beds. To the southeast, at the limits of surface ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Americas
The Americas, which are sometimes collectively called America, are a landmass comprising the totality of North America, North and South America. The Americas make up most of the land in Earth's Western Hemisphere and comprise the New World. Along with their Lists of islands of the Americas, associated islands, the Americas cover 8% of Earth's total surface area and 28.4% of its land area. The topography is dominated by the American Cordillera, a long chain of mountains that runs the length of the west coast. The flatter eastern side of the Americas is dominated by large river basins, such as the Amazon river basin, Amazon, St. Lawrence River–Great Lakes basin, Mississippi river basin, Mississippi, and La Plata river basin, La Plata. Since the Americas extend from north to south, the climate and ecology vary widely, from the arctic tundra of Northern Canada, Greenland, and Alaska, to the tropical rain forests in Central America and South America. Humans first Settlement o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clovis Culture
The Clovis culture is a prehistoric Paleoamerican culture, named for distinct stone and bone tools found in close association with Pleistocene fauna, particularly two mammoths, at Blackwater Locality No. 1 near Clovis, New Mexico, in 1936 and 1937 (though Paleoindian artifacts had been found at the site since the 1920s). It appears around 11,500–11,000 uncalibrated years before present (YBP)"Clovis Culture" entry in the ''Concise Oxford Dictionary of Archaeology'': "9,500–9,000 BC". at the end of the last glacial period and is characterized by the manufacture of " Clovis points" and distinctive bone and ivory tools. Archaeologists' most precise determinations at present suggest this radiocarbon age is equal to roughly 13,200 to 12,900 calendar years ago. The only human burial that has been directly associated with tools from the Clovis culture included the remains of an infant boy researchers named Anzick-1. Paleogenetic analyses of Anzick-1's ancient nuclear, mitoc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utah State Route 261
State Route 261 is a state highway located entirely within south-central San Juan County, Utah. It runs north, from the junction of U.S. Route 163 ( north of Mexican Hat), to the junction with State Route 95, just east of Natural Bridges National Monument. The highway is part of the Utah section of the Trail of the Ancients, a National Scenic Byway. It includes steep switchbacks as it traverses the Moki Dugway. from a website Route description From its southern terminus north of Mexican Hat, SR-261 commences in a westerly direction. After turning north, the route encounters ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utah State Route 95
State Route 95 or Bicentennial Highway is a state highway located in the southeast of the U.S. state of Utah. The highway is an access road for tourism in the Lake Powell and Cedar Mesa areas, notably bisecting Bears Ears National Monument and providing the only access to Natural Bridges National Monument. The highway does not serve any cities, but the small town of Hanksville is its western terminus. Although the highway has existed since the 1930s as a primitive dirt road, it received its name at its dedication as a paved state highway coincident with the U.S. Bicentennial in 1976. The highway forms part of the Trail of the Ancients National Scenic Byway. Route description It runs west from the junction of U.S. Route 191 (4.3 miles south of the town of Blanding), to the junction of SR-24 in the town of Hanksville. It crosses Cottonwood Wash just west of the US-191 junction; follows and crosses White Canyon; and crosses the Colorado River and the northeast end of Lake Pow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stimper Arch
Stimper Arch is a well-known rock formation in the wall of Kane Gulch on the Cedar Mesa plateau in southeast Utah, in the United States The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territorie .... The arch has a span of 20 feet and an opening height of 6 ft, and is located about 3.75 miles from the Kane Gulch Ranger Station Stimper Arch is a popular subject for amateur photographers as well as a destination for many hikers. References {{coord, 37, 30, 28, N, 109, 56, 40, W, display=title Natural arches of Utah Natural arches of San Juan County, Utah ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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