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Parriott Mesa
Parriott Mesa is a 6,155-foot-elevation sandstone summit in Grand County of Utah, United States. Parriott Mesa is located at Castle Valley, Utah, near the city of Moab. The name honors Dale M. Parriott (1885–1958), who was a Moab settler, and owned a ranch house in Castle Valley. Parriott Mesa is a thin 0.4 mile wide, and 1.5 mile long north-to-south mesa with 400 ft vertical Wingate Sandstone walls. Precipitation runoff from the mesa drains into the Colorado River which is about a mile away. The nearest higher peak is ''The Priest'', to the east. Climate Spring and fall are the most favorable seasons to visit, when highs average 60 to 80 °F and lows average 30 to 50 °F. Summer temperatures often exceed 100 °F. Winters are cold, with highs averaging 30 to 50 °F, and lows averaging 0 to 20 °F. As part of a high desert region, it can experience wide daily temperature fluctuations. The area receives an average of less than 10 inches (25 cm) of rain annually. Climbing Routes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utah State Route 128
State Route 128 (SR-128) is a state highway in the U.S. state of Utah. The entire length of the highway has been designated the Upper Colorado River Scenic Byway, as part of the Utah Scenic Byways program. This road also forms part of the Dinosaur Diamond Prehistoric Highway, a National Scenic Byway. Residents of Moab frequently refer to SR-128 as "the river road", after the Colorado River, which the highway follows. The highway was originally constructed to connect rural cities in eastern Utah with Grand Junction, Colorado, the largest city in the region. Part of the highway was merged into the Utah state highway system in 1931; the rest was taken over by the state and assigned route number 128 in 1933. Today, the highway is used as a scenic drive for visitors to the area. The highway crosses the Colorado River at the site of the Dewey Bridge, listed on the National Register of Historic Places. This bridge was the longest suspension bridge in Utah until April 2008 when ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wingate Sandstone
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. Geology Wingate Sandstone is particularly prominent in southeastern Utah, where it forms attractions in a number of national parks and monuments. These include Capitol Reef National Park, the San Rafael Swell, and Canyonlands National Park. Wingate Sandstone frequently appears just below the Kayenta Formation and Navajo Sandstone, two other formations of the Glen Canyon group. Together, these three formations can result in immense vertical cliffs of 2000 feet (609 meters) or more. Wingate layers are typically pale orange to red in color, the remnants of wind-born sand dunes deposited approximately 200 million years ago in the Late Triassic. Fossil content Long dated to the Early Jurassic only, fossils (including a phytosaur skull) and other evidence indicate that part of the Wing ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Grand 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, 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, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...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] |
Castleton Tower
Castleton Tower (officially, Castle Rock) is a Wingate Sandstone tower standing on a 1,000 foot Moenkopi-Chinle cone above the northeastern border of Castle Valley, Utah. The tower is world-renowned as a subject for photography and for its classic rock climbing routes, the most famous of which is the Kor-Ingalls Route featured in Fifty Classic Climbs of North America. It can be accessed by a trail that begins south of the tower at a primitive camp ground. Location Castleton Tower sits at the southern terminus of a ridge made mostly of red sand, gravel, scatter boulders, and few short cliff lines. The ridge that runs north to south for about at its high point. Castleton Tower (~40'x400') shares the ridge with a structure at the ridge's Northern terminus with a similar height but considerable larger area known as ''The Rectory'' (~200'x1000'). This second structure is also referred to as ''The Priest and Nuns'' although those names are more often applied to specific structure ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Rectory (Utah)
The Rectory is a 6,565-ft (2,001 m) sandstone summit in Grand County of Utah, United States. The Rectory is located at Castle Valley, Utah, near the city of Moab. The Rectory is a thin 200 feet (61 m) wide, and 1,000 feet (305 m) long north-to-south butte with 200 ft vertical Wingate Sandstone walls tower standing on a 1,000 foot Moenkopi- Chinle base. Precipitation runoff from The Rectory drains into the nearby Colorado River. The nearest higher peak is Castleton Tower, to the south. ''Priest and Nuns'' are towers immediately north and part of The Rectory. Further northwest along the connecting ridge is The Convent, with a rock tower called Sister Superior between the two. The first ascent was made May 22, 1962, by Harvey Carter and Cleve McCarty via ''Empirical Route''. Harvey Carter named this geological feature. Climbing Routes Classic Climbing Routes on The Rectory [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Convent (Mesa)
Convent Mesa, or The Convent,The Convent Mountain Project or simply Convent, are alternative names for a 5,955-foot elevation sandstone summit in Grand County of , . The Convent is located in Professor Valley, near the city of . It is situated northeast of [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Colorado River
The Colorado River ( es, Río Colorado) is one of the principal rivers (along with the Rio Grande) in the Southwestern United States and northern Mexico. The river drains an expansive, arid drainage basin, watershed that encompasses parts of seven U.S. states and two Mexican states. The name Colorado derives from the Spanish language for "colored reddish" due to its heavy silt load. Starting in the central Rocky Mountains of Colorado, it flows generally southwest across the Colorado Plateau and through the Grand Canyon before reaching Lake Mead on the Arizona–Nevada border, where it turns south toward the Mexico–United States border, international border. After entering Mexico, the Colorado approaches the mostly dry Colorado River Delta at the tip of the Gulf of California between Baja California and Sonora. Known for its dramatic canyons, whitewater rapids, and eleven National parks of the United States, U.S. National Parks, the Colorado River and its tributaries are a v ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surface Runoff
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moab, Utah
Moab () is the largest city and county seat of Grand County in eastern Utah in the western United States, known for its dramatic scenery. The population was 5,366 at the 2020 census. Moab attracts many tourists annually, mostly visitors to the nearby Arches and Canyonlands National Parks. The town is a popular base for mountain bikers who ride the extensive network of trails including the Slickrock Trail, and for off-roaders who come for the annual Moab Jeep Safari. History Early years The Biblical name Moab refers to an area of land located on the eastern side of the Jordan River. Some historians believe the city in Utah came to use this name because of William Andrew Peirce, the first postmaster, believing that the biblical Moab and this part of Utah were both "the far country". However, others believe the name has Paiute origins, referring to the word ''moapa'', meaning "mosquito". Some of the area's early residents attempted to change the city's name, because in the Chr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utah
Utah ( , ) is a state in the Mountain West subregion of the Western United States. Utah is a landlocked U.S. state bordered to its east by Colorado, to its northeast by Wyoming, to its north by Idaho, to its south by Arizona, and to its west by Nevada. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin. Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo and Ute. The Spanish were the first Europe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Castle Valley, Utah
Castle Valley is a town in Grand County, Utah, United States. The population was 319 at the 2010 census. The town is approximately 16 miles northeast of Moab, near State Route 128. The community was named for castle-like rock formations near the town site. Geography According to the United States Census Bureau, the town has a total area of 8.1 square miles (20.9 km2), all land. Demographics At the time of 2020 census, there were 354 people residing in the town; at the time of the 2000 census, there were 349 people, 158 households, and 85 families residing in the town. The population density was 39.4 per square mile (15.2/km2). In 2000, there were 230 housing units at an average density of 28.5 per square mile (11.0/km2). The racial makeup of the town in 2000 was 97.13% White, 1.15% from other races, and 1.72% from two or more races. Hispanic or Latino of any race were 2.29% of the population. There were 158 households, of which 19.6% had children under 18 living ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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