Mount Tukuhnikivatz
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Mount Tukuhnikivatz
Mount Tukuhnikivatz is a 12,482-foot (3,805 meter) elevation summit located in San Juan County of Utah, United States. Mount Tukuhnikivatz is the third-highest peak of the La Sal Mountains, and is the premier ski mountaineering destination in the La Sals. It is situated in a dry, rugged, sparsely settled region, and set on land administered by Manti-La Sal National Forest. Precipitation runoff from this mountain drains into tributaries of the Colorado River. The nearest town is Moab, to the northwest, and the nearest higher neighbor is Mount Peale, to the east. The mountain's name is a Native American word that translates as "Where the sun sets last." Locals call it Mount Tuk for short.Jared Hargrave, ''Backcountry Ski & Snowboard Routes Utah'', The Mountaineers Books, 2015 This mountain has a subsidiary peak unofficially called ''Little Tuk'' (12,048 feet), approximately one-half mile to the north-northwest. Climate Spring and fall are the most favorable seasons to visit Moun ...
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Mount Peale
Mount Peale is the highest point in the La Sal Mountains of San Juan County, in the southeastern part of Utah, United States. It is also the highest point in Utah outside the Uinta Mountains. It is located about southeast of Moab. The summit is the highest point in the Manti-La Sal National Forest and the Mount Peale Research Natural Area. Mount Peale was named for Albert Peale, a mineralogist on the Hayden Survey of 1875. The La Sal Mountains sit on the arid Colorado Plateau, near such famous desert landmarks as Canyonlands National Park and Arches National Park. However, due to their height, the La Sals are heavily forested and usually snow-capped until early summer (there is one snowfield on the north side that usually lasts year round).Michael R. Kelsey, ''Guide to the World's Mountains'' (third edition), Kelsey Publishing, 1996, , pp. 682–683. Mount Peale can be seen on a clear day from the Wasatch Plateau of central Utah, near Orangeville, over away. Mount Peale ca ...
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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 ...
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Mountains Of Utah
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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List Of Mountain Peaks Of Utah
This article comprises three sortable tables of major mountain peaksThis article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence. All summits in this article have at least 500 meters of topographic prominence. An ultra-prominent summit is a summit with at least of topographic prominence. of the U.S. State of Utah. The summit of a mountain or hill may be measured in three principal ways: #The topographic elevation of a summit measures the height of the summit above a geodetic sea level.All elevations in this article include an elevation adjustment from the National Geodetic Vertical Datum of 1929 (NGVD 29) to the North American Vertical Datum of 1988 (NAVD 88). For further information, please see this United States National Geodetic Surveybr>noteIf the elevation or prominence of a summit is calculated as a range of values, the arithmetic mean is shown. The firs ...
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Colorado Plateau
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. The Colorado Plateau is largely made up of high desert, with scattered areas of forests. In the south-west corner of the Colorado Plateau lies the Grand Canyon of the Colorado River. Much of the Plateau's landscape is related to the Grand Canyon in both appearance and geologic history. The nickname "Red Rock Country" suggests the brightly colored ...
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Mount Mellenthin
Mount Mellenthin is a 12,645-foot (3,854 meter) elevation summit located in San Juan County of Utah, United States. Mount Mellenthin is the second-highest peak of the La Sal Mountains. It is situated in a dry, rugged, sparsely settled region, and set on land administered by Manti-La Sal National Forest. Precipitation runoff from this mountain drains into tributaries of the Colorado River. The nearest town is Moab, to the northwest, and the nearest higher neighbor is Mount Peale, to the south. The mountain's name honors Rudolf E. Mellenthin (1884–1918), forest ranger of La Sal National Forest, who was shot to death near this peak on August 23, 1918, while attempting to apprehend two draft evaders. This geographical feature's name was officially adopted in 1932 by the U.S. Board on Geographic Names. Climate Spring and fall are the most favorable seasons to visit Mount Mellenthin. According to the Köppen climate classification system, it is located in a Cold semi-arid climat ...
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Delicate Arch
Delicate Arch is a freestanding natural arch located in Arches National Park, near Moab, Utah, Moab in Grand County, Utah, Grand County, Utah, United States. The arch is the most widely recognized landmark in Arches National Park and is depicted on Vehicle registration plates of Utah, Utah license plates and a postage stamp commemorating Utah's centennial anniversary of admission to the Union in 1996. The 2002 Winter Olympics torch relay, Olympic torch relay for the 2002 Winter Olympics passed through the arch. History Because of its distinctive shape, the arch was known as "the Chaps" and "the Schoolmarm's Bloomers (clothing), Bloomers" by local cowboys. Many other names have been applied to this arch including "Bloomers Arch", "Marys Bloomers", "Old Maids Bloomers", "Pants Crotch", "Salt Wash Arch", and "School Marms Pants". The arch was given its current name by Frank Beckwith, leader of the Arches National Monument Scientific Expedition, who explored the area in the winter o ...
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Cold Semi-arid Climate
A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes. Defining attributes of semi-arid climates A more precise definition is given by the Köppen climate classification, which treats steppe climates (''BSk'' and ''BSh'') as intermediates between desert climates (BW) and humid climates (A, C, D) in ecological characteristics and agricultural potential. Semi-arid climates tend to support short, thorny or scrubby vegetation and are usually dominated by either grasses or shrubs as it usually can't support forests. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. The method used to find the precipitation threshold (in millimeters): *multiply ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ...
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Southern Paiute Language
Colorado River Numic (also called Ute , Southern Paiute , Ute–Southern Paiute, or Ute-Chemehuevi ), of the Numic branch of the Uto-Aztecan language family, is a dialect chain that stretches from southeastern California to Colorado. Individual dialects are Chemehuevi, which is in danger of extinction, Southern Paiute (Moapa, Cedar City, Kaibab, and San Juan subdialects), and Ute (Central Utah, Northern, White Mesa, Southern subdialects). According to the ''Ethnologue'', there were a little less than two thousand speakers of Colorado River Numic Language in 1990, or around 40% out of an ethnic population of 5,000. The Southern Paiute dialect has played a significant role in linguistics, as the background for a famous article by linguist Edward Sapir and his collaborator Tony Tillohash on the nature of the phoneme. Dialects The three major dialect groups of Colorado River are Chemehuevi, Southern Paiute, and Ute, although there are no strong isoglosses. The threefold division is ...
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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 ...
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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 ...
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