Photo: Meadow and mountains

Most people visit Wyoming's Grant Teton National Park in July and August, when it's sunny and warm and the snow has melted in the high country.

Photograph by Mike Briner, submitted to My Shot

Location: Wyoming

Established: February 26, 1929

Size: 309,994 acres

The peaks of the Teton Range, regal and imposing as they stand nearly 7,000 feet above the valley floor, make one of the boldest geologic statements in the Rockies. Unencumbered by foothills, they rise through steep coniferous forest into alpine meadows strewn with wildflowers, past blue and white glaciers to naked granite pinnacles. The Grand, Middle, and South Tetons form the heart of the range. But their neighbors, especially Mount Owen, Teewinot Mountain, and Mount Moran, are no less spectacular.

A string of jewel-like lakes, fed by mountain streams, are set tightly against the steep foot of the mountains. Beyond them extends the broad valley called Jackson Hole, covered with sagebrush and punctuated by occasional forested buttes and groves of aspen trees—excellent habitats for pronghorn, deer, elk, and other animals. The Snake River, having begun its journey in southern Yellowstone National Park near the Teton Wilderness, winds leisurely past the Tetons on its way to Idaho. The braided sections of the river create wetlands that support moose, elk, deer, beavers, trumpeter swans, sandhill cranes, Canada geese, and all sorts of ducks.

The Tetons are normal faultblock mountains. About 13 million years ago, two blocks of Earth's crust began to shift along a fault line, one tilting down while the other lifted up. So far, movement has measured some 30,000 vertical feet, most of it from the subsidence of Jackson Hole.

Before Europeans arrived, the Teton area was an important plant-gathering and hunting ground for Indians of various tribes. In the early 1800s, mountain men spent time here; it was they who called this flat valley ringed by mountains Jackson's Hole after the trapper Davey Jackson. (In recent times the name has lost its apostrophe and s.) The first settlers were ranchers and farmers. Some of their buildings are historic sites today, although ranching is still practiced in the vicinity. When the park was established, it included only the mountains and the glacial lakes at their feet. Portions of the valley were added in 1950.

Today the park's 485 square miles encompass both the Teton Range and much of Jackson Hole. Park roads, all in the valley, offer an ever changing panorama of the Tetons. Most visitors never go far from the road. But the Tetons are popular with hikers; backcountry trails climb high into the mountains—and behind them. Easy trails in the valley lead around lakes and beside wetlands where visitors see moose, elk, deer, and all kinds of birds.

Did You Know?

Grand Teton National Park was actually established twice, first in 1929 to protect mountain peaks and the lakes surrounding the mountain bases, then in 1950, when the adjacent valley floors as well as the Jackson Hole National Monument, created in 1943, were incorporated into the park visitors love today. Since 1972, the John D. Rockefeller, Jr. Memorial Parkway has connected Grand Teton to Yellowstone National Park, enabling visitors to experience both the slopes of the Tetons and the volcanic landscape of Yellowstone.

Copy for this series includes excerpts from the National Geographic Guide to the National Parks of the United States, Seventh Edition, 2012, and the National Parks articles featured in "Cutting Loose" in National Geographic Traveler.

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