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Grand Teton National Park is a national park of the United States in northwestern Wyoming. At approximately 310,000 acres (1,300 km 2), the park includes the major peaks of the 40-mile-long (64 km) Teton Range as well as most of the northern sections of the valley known as Jackson Hole.
1929 U.S.G.S. Map of Grand Teton National Park, Wyoming - Geographicus - GrandTeton-USGS-1929 [a]. 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 [1] within the boundary, and countless smaller unnamed lakes and ponds.
Location: Grand Teton National Park, Teton County, Wyoming, US: Coordinates: 1]: Type: Glacial Lake: Primary inflows: Cascade Creek and String Lake: Primary outflows: Cottonwood Creek: Basin countries: United States: Max. length: 2.2 mi (3.5 km): Max. width: 1.2 mi (1.9 km): Surface area: 1,191 acres (482 ha) [2]: Max. depth: 456 ft (139 m) [2]: Surface elevation: 6,783 ft (2,067 m): Jenny ...
The Amphitheater Lake Trail is a 5-mile (8.0 km) long hiking trail in Grand Teton National Park in the U.S. state of Wyoming. [1] The trailhead is at the Lupine Meadows parking area and climbs steeply more than 3,000 feet (910 m) in just over 5 miles (8.0 km) to Amphitheater Lake. [2]
The Lake Solitude Trail is a 4.8-mile (7.7 km) long hiking trail in Grand Teton National Park in the U.S. state of Wyoming. [1] The trail begins at the Forks of Cascade Canyon and follows Cascade Creek up through North Cascade Canyon to Lake Solitude.
Surprise Lake is a lake in Grand Teton National Park, in the U. S. state of Wyoming. [2] Surprise Lake is on .20 miles (0.32 km) east of Amphitheater Lake and can be accessed via a strenuous climb of just under 10 miles (16 km) round trip from the Lupine Meadows trailhead. [3]
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The canyons of the Teton Range lie almost entirely within Grand Teton National Park in the U.S. state of Wyoming. Ranging from 9 miles (14 km) to less than 1 mile (1.6 km) in length and up to 6,000 feet (1,800 m) deep, the canyons were carved primarily by glaciers over the past 250,000 years. [ 1 ]
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