Granite Canyon
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Granite Canyon
Granite Canyon is located in Grand Teton National Park, in the U. S. state of Wyoming. The canyon was formed by glaciers which retreated at the end of the last glacial maximum approximately 15,000 years ago, leaving behind a U-shaped valley. The canyon lies between Rendezvous Mountain to the south and Mount Hunt to the north. The trailhead for the canyon is on the Moose–Wilson Road about north of Teton Village. One of the most popular hikes from the trailhead is to Marion Lake by way of the Granite Canyon Trail which traverses the length of the canyon. Another popular hike involves riding the aerial tram located at the Jackson Hole Mountain Resort in Teton Village to the top of Rendezvous Mountain, and then descending back to Teton Village by way of Granite Canyon. The descent from the summit of Rendezvous Peak back to Teton Village is an often steep one with an altitude loss of . The historic Upper Granite Canyon Patrol Cabin is situated near the entrance to the canyon ...
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Granite Canyon Trail
The Granite Canyon Trail is a long hiking trail in Grand Teton National Park in the U.S. state of Wyoming. The trail begins at the Granite Canyon trailhead on the Moose-Wilson Road, about north of Teton Village and ends at the junction with the Teton Crest Trail near Marion Lake. The trail follows the length of Granite Canyon. Just over a mile before the junction with the Teton Crest Trail, the Open Canyon Trail intercepts this trail from the north. An alternative route is to take the Jackson Hole Mountain Resort ski lift to the top of Rendezvous Mountain Rendezvous Mountain () is a large mountain massif located in the southern Teton Range in the U.S. state of Wyoming. The highest point on Rendezvous Mountain is Rendezvous Peak (). The western and northern flanks of the mountain are in Grand Teton ... and descend down the Rendezvous Mountain Trail to junction with the Granite Canyon Trail, a distance of and mostly downhill. There are three different camping zones in the ...
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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 territories, nine Minor Outlying Islands, and 326 Indian reservations. The United States is also in free association with three Pacific Island sovereign states: the Federated States of Micronesia, the Marshall Islands, and the Republic of Palau. It is the world's third-largest country by both land and total area. It shares land borders with Canada to its north and with Mexico to its south and has maritime borders with the Bahamas, Cuba, Russia, and other nations. With a population of over 333 million, it is the most populous country in the Americas and the third most populous in the world. The national capital of the United States is Washington, D.C. and its most populous city and principal financial center is New York City. Paleo-Americ ...
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Canyons Of The Teton Range
The canyons of the Teton Range lie almost entirely within Grand Teton National Park in the U.S. state of Wyoming. Ranging from to less than in length and up to deep, the canyons were carved primarily by glaciers over the past 250,000 years. The canyons in the Teton Range descend in altitude generally west to east and many have lakes at their outlets. The lakes were created by terminal moraines left behind by the now retreated glaciers. A few of the canyons have small glaciers that were created mostly during the Little Ice Age (1550-1850). Fast retreating Schoolroom Glacier is a tiny glacier located at the head of the South Cascade Canyon. Most of the canyons have streams from which rain and snowmelt flow towards Jackson Hole valley, and due to the sometimes rapid altitude descent, waterfalls are common. The canyons offer the easiest hiking access into the Teton Range. Teton Range canyons within Grand Teton National Park *Webb Canyon is long and originates at several alpine l ...
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Granite Canyon South Fork
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ...
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National Register Of Historic Places
The National Register of Historic Places (NRHP) is the United States federal government's official list of districts, sites, buildings, structures and objects deemed worthy of preservation for their historical significance or "great artistic value". A property listed in the National Register, or located within a National Register Historic District, may qualify for tax incentives derived from the total value of expenses incurred in preserving the property. The passage of the National Historic Preservation Act (NHPA) in 1966 established the National Register and the process for adding properties to it. Of the more than one and a half million properties on the National Register, 95,000 are listed individually. The remainder are contributing resources within historic districts. For most of its history, the National Register has been administered by the National Park Service (NPS), an agency within the U.S. Department of the Interior. Its goals are to help property owners and inte ...
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Upper Granite Canyon Patrol Cabin
The Upper Granite Canyon Patrol Cabin was built by the Civilian Conservation Corps about 1935. The log structure is located in the extreme southwest backcountry of Grand Teton National Park. The cabin was built according to a standard design for such structures, in the National Park Service Rustic style. The Moran Bay Patrol Cabin is similar. The patrol cabin is a one-story log cabin on a log sill foundation using logs. The cabin is square in plan with asphalt roll roofing on the gabled roof. The door retains its original wrought iron hardware. The interior is floored with boards, cut to a length of to fit a pack saddle. The interior logs are trimmed with split-pole chinking. The ceiling is open, with exposed log framing. The Upper Granite Canyon Patrol Cabin was placed on the National Register of Historic Places on August 19, 1998. See also * Historical buildings and structures of Grand Teton National Park The historical buildings and structures of Grand Teton National ...
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Jackson Hole Mountain Resort
Jackson Hole Mountain Resort (JHMR) is a ski resort in the western United States, at Teton Village, Wyoming. In the Teton Range of the Rocky Mountains, it is located in Teton County, northwest of Jackson and due south of Grand Teton National Park. It is named after the historically significant Jackson Hole valley and is known for its steep terrain and large continuous vertical drop of . JHMR appears frequently in the media as one of North America's most expensive ski resorts. Ski area information The ski area partially covers Rendezvous and Apres Vous Mountains and is known for its challenging terrain, including the infamous Corbet's Couloir. Half of the terrain is rated expert, 40% intermediate, and only 10% beginner. The intermediate terrain is primarily on south-facing Apres Vous Mountain, while Rendezvous Mountain has Jackson Hole's more advanced terrain, including bowls, glades, and chutes. At over 4,000 vertical feet of skiing, Jackson Hole boasts one of the greatest co ...
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Aerial Tram
An aerial tramway, sky tram, cable car, ropeway, aerial tram, telepherique, or seilbahn is a type of aerial lift which uses one or two stationary ropes for support while a third moving rope provides propulsion. With this form of lift, the grip of an aerial tramway cabin is fixed onto the propulsion rope and cannot be decoupled from it during operations. In comparison to gondola lifts, aerial tramways generally provide lower line capacities and higher wait times. Terminology Because of the proliferation of such systems in the Alpine regions of Europe, the French and German names, ''téléphérique'' and ''Seilbahn'', respectively, are often also used in an English language context. ''Cable car'' is the usual term in British English, as in British English the word ''tramway'' generally refers to a railed street tramway while in American English, ''cable car'' may additionally refer to a cable-pulled street tramway with detachable vehicles; e.g., San Francisco's cable cars. ...
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Marion Lake (Teton County, Wyoming)
There are 44 named and countless unnamed lakes in Grand Teton National Park. The largest of these is Jackson Lake, a natural glacial lake that has been enlarged with the construction of the Jackson Lake Dam. The lakes range in size as well as ease of access. In addition to mountain tarns, there are several large peidmont lakes. Nearly all the lakes are glacial in origin, formed by glacial action that carved out the valleys and left moraine behind that acted as dams to lock in water. The lakes exist in the near pristine wilderness environment of the park, and recreational use, boating and fishing varies by lake. Elevation of the region classes these as alpine lakes, with Jackson lake being the largest alpine lake in the United States. Overview At its formation in 1929, Grand Teton National Park encompassed just six main lakes at the foot of the park's major peaks, but with the expansion of the park there are now 44 named lakes within the boundary, and countless smaller unname ...
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Wyoming
Wyoming () is a U.S. state, state in the Mountain states, Mountain West subregion of the Western United States. It is bordered by Montana to the north and northwest, South Dakota and Nebraska to the east, Idaho to the west, Utah to the southwest, and Colorado to the south. With a population of 576,851 in the 2020 United States census, Wyoming is the List of U.S. states and territories by population, least populous state despite being the List of U.S. states and territories by area, 10th largest by area, with the List of U.S. states by population density, second-lowest population density after Alaska. The state capital and List of municipalities in Wyoming, most populous city is Cheyenne, Wyoming, Cheyenne, which had an estimated population of 63,957 in 2018. Wyoming's western half is covered mostly by the ranges and rangelands of the Rocky Mountains, while the eastern half of the state is high-elevation prairie called the High Plains (United States), High Plains. It is drier ...
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Rendezvous Mountain
Rendezvous Mountain () is a large mountain massif located in the southern Teton Range in the U.S. state of Wyoming. The highest point on Rendezvous Mountain is Rendezvous Peak (). The western and northern flanks of the mountain are in Grand Teton National Park, while much of the remainder of the massif is in the Bridger-Teton National Forest. The mountain massif extends for a distance of between Granite Canyon to the north and Phillips Canyon to the south. Though there are numerous summits above , the one that is most commonly visited is the North Peak, where the Jackson Hole Mountain Resort aerial tram provides access to the summit for skiers in the winter and sightseers and hikers Hiking is a long, vigorous walk, usually on trails or footpaths in the countryside. Walking for pleasure developed in Europe during the eighteenth century.AMATO, JOSEPH A. "Mind over Foot: Romantic Walking and Rambling." In ''On Foot: A Hist ... in the summer. The hike down the Rendezvous ...
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U-shaped Valley
U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight sides and a flat or rounded bottom (by contrast, valleys carved by rivers tend to be V-shaped in cross-section). Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice, called glacial till or glacial erratic. Examples of U-shaped valleys are found in mountainous regions throughout the world including the Andes, Alps, Caucasus Mountains, Himalaya, Rocky Mountains, New Zealand and the Scandinavian Mountains. They are found also in other major European mountains including the Carpathian Mountains, the Pyrenees, the Rila and Pirin mountains in Bulgaria, an ...
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