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Death Canyon Shelf
Death Canyon Shelf is a narrow plateau located in Grand Teton National Park in the U.S. state of Wyoming. The plateau extends from Fox Creek Pass to Mount Meek Pass, a distance of almost . The Death Canyon Shelf parallels much of Death Canyon to the east and has cliffs rising several hundred feet to the west for most of the shelf's length. Camping is permitted on Death Canyon Shelf with a permit. The shelf is traversed by the Teton Crest Trail for its entire length, but it is deep in the backcountry, requiring a hike from the Death Canyon trailhead to access. See also *Geology of the Grand Teton area The geology of the Grand Teton area consists of some of the oldest rocks and one of the youngest mountain ranges in North America. The Teton Range, partly located in Grand Teton National Park, started to grow some 9 million years ago. An older fe ... References Landforms of Grand Teton National Park Plateaus of the United States Landforms of Teton County, Wyoming {{wyom ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grand Teton National Park
Grand Teton National Park is an American national park in northwestern Wyoming. At approximately , the park includes the major peaks of the Teton Range as well as most of the northern sections of the valley known as Jackson Hole. Grand Teton National Park is only south of Yellowstone National Park, to which it is connected by the National Park Service–managed John D. Rockefeller Jr. Memorial Parkway. Along with surrounding national forests, these three protected areas constitute the almost Greater Yellowstone Ecosystem, one of the world's largest intact mid-latitude temperate ecosystems. The human history of the Grand Teton region dates back at least 11,000 years when the first nomadic hunter-gatherer Paleo-Indians began migrating into the region during warmer months to pursue food and supplies. In the early 19th century, the first white explorers encountered the eastern Shoshone natives. Between 1810 and 1840, the region attracted fur trading companies that vied ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wyoming
Wyoming () is a state in the 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 least populous state despite being the 10th largest by area, with the second-lowest population density after Alaska. The state capital and most populous city is 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. It is drier and windier than the rest of the country, being split between semi-arid and continental climates with greater temperature extremes. Almost half of the land in Wyoming is owned by the federal government, generally protected for public uses. The stat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fox Creek Pass
Fox Creek Pass is a pedestrian mountain pass located in the Teton Range, Grand Teton National Park, in the U.S. state of Wyoming. The pass is situated at above sea level and is at the head of Death Canyon. Fox Creek Pass can be accessed by way of the Teton Crest Trail or the Death Canyon Trail from the east. To the north lies the Death Canyon Shelf Death Canyon Shelf is a narrow plateau located in Grand Teton National Park in the U.S. state of Wyoming. The plateau extends from Fox Creek Pass to Mount Meek Pass, a distance of almost . The Death Canyon Shelf parallels much of Death Canyon to th ... in Grand Teton National Park while Fossil Mountain and Caribou-Targhee National Forest are to the west and south, respectively. References Mountain passes of Wyoming Mountain passes of Teton County, Wyoming {{wyoming-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Meek Pass
Mount Meek Pass is a pedestrian mountain pass located in the Teton Range, Grand Teton National Park, in the U.S. state of Wyoming. The pass is situated at above sea level and is accessed by way of the Teton Crest Trail and is immediately east of Mount Meek. Mount Meek Pass is more than from the nearest trailhead. To the south of the pass lies Death Canyon Shelf within Grand Teton National Park, while to the north can be found the region known as Alaska Basin Alaska Basin is a subalpine basin on the west slopes of the Teton Range, in the U.S. state of Wyoming. Located on the western border of Grand Teton National Park, Alaska Basin is within the Jedediah Smith Wilderness of Caribou-Targhee National Fo ..., which is in Caribou-Targhee National Forest. References Mountain passes of Wyoming Mountain passes of Teton County, Wyoming {{wyoming-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Death Canyon
Death 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 trailhead for the canyon is located on a side road off the Moose-Wilson Road, approximately from the park headquarters at Moose, Wyoming. At the base of the canyon is Phelps Lake which was created by glacial activity. The Death Canyon Trail extends the length of the canyon to Fox Creek Pass, at which point the Death Canyon Shelf, a relative narrow and level plateau, can be traversed. The canyon has many Whitebark Pine stands, particularly near the tree line. At the junction of the Death Canyon and the Alaska Basin trails, the historic Death Canyon Barn is preserved after being listed on the National Register of Historic Places in 1998. See also *Canyons of the Teton Range The canyons of the Teton Range lie almost entirely within Grand ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teton Crest Trail
The Teton Crest Trail is a long hiking trail in the U.S. state of Wyoming that extends from Phillips Pass, on the border of Bridger Teton and Caribou-Targhee National Forests, to String Lake in Grand Teton National Park. ''Backpacker Magazine'' calls the Trail one of the "Best Hikes Ever," with "mesmerizing and constant views of jagged peaks." Beginning in the south, the Teton Crest Trail can be accessed in several ways. From inside the National Park, the Granite Canyon Trail provides a gradual ascent into the Range, where it connects with the TCT. The Trail is most easily accessed by riding the Jackson Hole Aerial Tram, which transports sightseers and hikers from the Teton Village Resort to the top of Rendezvous Mountain. From outside the Park, the Teton Crest Trail can be accessed via the Phillips Pass Trail, one of several routes through adjacent National Forest lands. Continuing from the south, it is a trek to String Lake, passing in and out of Bridger-Teton National Fore ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Grand Teton Area
The geology of the Grand Teton area consists of some of the oldest rocks and one of the youngest mountain ranges in North America. The Teton Range, partly located in Grand Teton National Park, started to grow some 9 million years ago. An older feature, Jackson Hole, is a basin that sits aside the range. The 2.5 billion year old metamorphic rocks that make up the east face of the Tetons are marine in origin and include some volcanic deposits. These same rocks are today buried deep inside Jackson Hole. Paleozoic rocks were deposited in warm shallow seas while Mesozoic deposition transitioned back and forth from marine to non-marine sediments with the Cretaceous Seaway periodically covering the area late in that era. Precambrian deposition, metamorphism, and intrusion Perhaps 3 billion years ago in Precambrian time, sand, limey ooze, silt and clay were deposited in a marine trough (accurate dating is not possible, due to subsequent partial recrystallization of the resulting roc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Grand Teton National Park
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, plateau ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateaus Of The United States
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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