Taggart Lake
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Taggart Lake
Taggart Lake is located in Grand Teton National Park, in the U. S. state of Wyoming. The natural lake is located at the terminus of Avalanche Canyon. A number of hiking trails can be found near the lake including a roundtrip hike commencing from the Taggart Lake Trailhead parking area. The lake is approximately one mile south of Bradley Lake reckoned by trail distance. A 2005 study of the water quality of the lakes in Grand Teton National Park indicated that the lakes in the park were still considered pristine and that they had not been impacted by air or water pollution. Taggart lake was named after William Rush Taggart, an assistant surveyor to Frank Bradley as part of the Snake River division of the Hayden expedition of 1872 to document the geology and topography of the Yellowstone area. Other lakes in the area were named after the below individuals: * Bradley Lake - Frank Bradley * Taggart Lake - William Rush Taggart * Leigh Lake - Beaver Dick Leigh * Jenny Lake - Jenny Leig ...
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Taggart Lake Trail
The Taggart Lake Trail is a long round-trip hiking trail in Grand Teton National Park in the U.S. state of Wyoming. The trail is accessed from the Taggart Lake trailhead and provides access to Taggart Lake, with views of the lake and the Teton Range. At Taggart Lake, the trail intercepts the Valley Trail which heads north towards Bradley Lake or south to Death Canyon. Using the Valley Trail and the Bradley Lake Trail, a loop hike starting from the Taggart Lake Trailhead is long. See also * List of hiking trails in Grand Teton National Park The hiking trails in Grand Teton National Park range from easy nature walks on generally level surfaces to strenuous and oftentimes steep climbs over high mountain passes. Located south of Yellowstone National Park in the northwestern section of th ... References Hiking trails of Grand Teton National Park {{wyoming-geo-stub ...
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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 fo ...
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Teton County, Wyoming
Teton County is a county in the U.S. state of Wyoming. As of the 2020 United States Census, the population was 23,331. Its county seat is Jackson. Its west boundary line is also the Wyoming state boundary shared with Idaho and the southern tip of Montana. Teton County is part of the Jackson, WY- ID Micropolitan Statistical Area. Teton County contains the Jackson Hole ski area, all of Grand Teton National Park, and 40.4% of Yellowstone National Park's total area, including over 96.6% of its water area (largely in Yellowstone Lake). Previously a staunchly Republican county, which produced Governor and U.S. Senator Clifford Hansen, Teton has become the most Democratic county in Wyoming, following a broader national trend of affluent and college-educated voters drifting towards the political party. In 2020, Joe Biden beat Donald Trump 67.10% to 29.58% in Teton, an overwhelming margin that was the most for a Democrat ever in the county. History Teton County was created February ...
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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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Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-bloc ...
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Avalanche Canyon
Avalanche 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. To the north of Avalanche Canyon lies South Teton, Cloudveil Dome and Nez Perce Peak while to the southwest lie Mount Wister and Veiled Peak. Snowdrift Lake and Lake Taminah are situated at the head of the canyon. See also *Canyons of the Teton Range *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 feat ... References Canyons and gorges of Wyoming Canyons and gorges of Grand Teton National Park {{wyoming-geo-stub ...
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Hiking
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 History of Walking'', 101-24. NYU Press, 2004. Accessed March 1, 2021. http://www.jstor.org/stable/j.ctt9qg056.7. Religious pilgrimages have existed much longer but they involve walking long distances for a spiritual purpose associated with specific religions. "Hiking" is the preferred term in Canada and the United States; the term "walking" is used in these regions for shorter, particularly urban walks. In the United Kingdom and the Republic of Ireland, the word "walking" describes all forms of walking, whether it is a walk in the park or backpacking in the Alps. The word hiking is also often used in the UK, along with rambling , hillwalking, and fell walking (a term mostly used for hillwalking in northern England). The term bushwalking is end ...
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Bradley Lake
Bradley Lake is located in Grand Teton National Park, in the U. S. state of Wyoming. The glacially formed lake is located near the terminus of Garnet Canyon. Bradley Lake can be accessed by the Bradley Lake Trail, a roundtrip hike commencing from the Taggart Lake trailhead parking area. The lake is less than north of Taggart Lake. 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 feat ... References Lakes of Grand Teton National Park {{wyoming-geo-stub ...
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Leigh Lake
Leigh Lake is located in Grand Teton National Park, in the U. S. state of Wyoming. The glacially formed lake is wide and long from north to south. Situated just southeast of Mount Moran, the lake is at the terminus of both Paintbrush and Leigh Canyons. The lake can be accessed from the Leigh Lake Trail which follows the eastern shores of String Lake a distance of one mile (1.6 km) and is an easy hike over level terrain. The Leigh Lake Ranger Patrol Cabin is located on the northeast shore of the lake and is on the National Register of Historic Places. The lake was named for Richard "Beaver Dick" Leigh, a mountain guide. Aerial image of Mount Moran and Mount Woodring (view from the east).jpg, Leigh Lake (bottom left) with Paintbrush Canyon, Mount Woodring, Leigh Canyon, and Mount Moran above (from left to right) Leigh Lake and Mount Moran Grand Teton National Park.jpg, Leigh Lake See also *Geology of the Grand Teton area The geology of the Grand Teton area consis ...
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Jenny Lake
Jenny Lake is located in Grand Teton National Park in the U.S. state of Wyoming. The lake was formed approximately 12,000 years ago by glaciers pushing rock debris which carved Cascade Canyon during the last glacial maximum, forming a terminal moraine which now impounds the lake. The lake is estimated to be deep and encompasses . Jenny Lake is considered to be a major focal point in Grand Teton National Park, with many hiking trails, scenic boat rides, and quick access to the major climbing routes onto the tallest peaks of the Teton Range. Jenny and Jackson Lakes are the only lakes in Grand Teton National Park where motorboats are permitted; both lakes have scenic tours available. A 2005 study of the water quality of the lakes in Grand Teton National Park indicated that all the lakes in the park were still considered pristine and that they had not been impacted by air or water pollution. Jenny Lake is a starting point for many day and overnight hiking trips. The Jenny Lake Tra ...
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Phelps Lake (Wyoming)
Phelps Lake is located in Grand Teton National Park, in the U. S. state of Wyoming. The natural lake is located at the entrance to Death Canyon in the southern section of the park. A number of hiking trails can be found near the lake, the most popular being a 1.8 mile (2.9 km) roundtrip hike to the Phelps Lake overlook. Jumping Rock "Jumping Rock" is a popular rock that sits on the northern side of Phelps Lake. It is so called "Jumping Rock" for the reason that it performs as a natural diving board. It is a 25–30 foot drop into the lake, but the water is deep enough for those brave enough to jump in. The water is cold, even in August. 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 feat ... Cited references External linksHi-resol ...
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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 rock) ...
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