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The furthest consistent migration of elk to the refuge is currently from the southern portion of Yellowstone National Park, [4] making it the second-longest ungulate migration in the lower 48 states. (The migration of pronghorn between the Green River basin and Jackson Hole is longer).
In a 2003 study by the Jackson Hole Wildlife Foundation, it was estimated that wildlife collisions in Teton County cost $1.2 million per year. [7] More recently, the Jackson Hole Wildlife Foundation completed an economic impact assessment for 2016-2017 that found total economic loss from wildlife collisions to be $3,172,837 in Teton County. [8]
While overhunting is a significant contributing factor, the elk's near extinction is mainly attributed to human encroachment and destruction of their natural habitats and migratory corridors. A year later, twenty-one elk from Jackson Hole, Wyoming were reintroduced to South Dakota's Wind Cave National Park for population increase. [3]
And it offers easy access to Yellowstone National Park, or Jackson Hole. ... Yellowstone National Park elk forage around a Mammoth, Wyoming home in the Park in this October, 1994 file photo. ...
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Elk do not appear to benefit from thermal cover. [44] The Greater Yellowstone Ecosystem elk herds comprise as many as 40,000 individuals. [45] During the spring and fall, they take part in the longest elk migration in the continental U.S., traveling as much as 168 mi (270 km) between summer and winter ranges.
Elk and deer in Jackson Hole use exposures of bentonite as a (bitter) salt lick. Bentonite swells when wet, which causes landslides that sometimes block access roads into Jackson Hole. Cretaceous-aged rocks in the Teton region form part of a huge east-thinning wedge of crust that is locally almost 2 miles (3.2 km) thick.
The school is in the town of Gardiner at Yellowstone National Park’s north entrance — and part of the school building is actually inside the park, USA Today reported.
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