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The Snake River Canyon (also known as the Grand Canyon) is formed by the Snake River in western Wyoming, United States, south of Jackson Hole. [2] At the southern end of this canyon is the town of Alpine, Wyoming where the Snake River meets the Greys River and the Salt River at Palisades Reservoir on the Wyoming-Idaho border.
About 1 Ma, the Snake River captured the Jackson Hole watershed, draining Lake Teewinot and finally connecting the modern-day Snake headwaters to the rest of the river. [80] This landscape around the Snake headwaters was sculpted by multiple Ice Age glaciations.
The Snake River threads through the entire valley from its headwater in Yellowstone in the north to the mouth of the Snake River Canyon at the southern tip of the valley. Blacktail Butte is a prominent landform rising from the valley floor. The average elevation of the valley is over 6,500 feet (2,000 m) above sea level.
I recently stayed at Hotel Yellowstone, which opened in Jackson Hole, Wyoming, in August. The luxury adults-only resort offers views of the Tetons and Snake River Valley. My 600-square-foot room ...
The Snake River then flows through the spillways of the Jackson Lake Dam and from there southward through Jackson Hole, exiting the park just west of the Jackson Hole Airport. [84] The largest lakes in the park all drain either directly or by tributary streams into the Snake River.
Menor's Ferry was a river ferry that crossed the Snake River near the present-day Moose, Wyoming, United States. The site was homesteaded by Bill Menor in 1892-94, choosing a location where the river flowed in a single channel, rather than the braided stream that characterizes its course in most of Jackson Hole. During the 1890s it was the only ...
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