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The Cathedral Group is the group of the tallest mountains of the Teton Range, all of which are located in Grand Teton National Park in the U.S. state of Wyoming. The Cathedral Group are classic alpine peaks, with pyramidal shapes caused by glacial motion .
Aerial view of the Cathedral Group of the Teton Range from the southeast with South Teton, Nez Perce Peak, Middle Teton, Grand Teton, Mount Owen, Teewinot Mountain (from left to right; see the image annotations), Taggart Lake (left), and Bradley Lake (right) The Teton Range is a mountain range of the Rocky Mountains in North America.
The Chapel of the Transfiguration is a small log chapel in Grand Teton National Park, in the community of Moose. [2] The chapel was sited and built to frame a view of the Cathedral Group of peaks in a large window behind the altar.
Grand Teton is the highest mountain of the Teton Range in Grand Teton National Park at 13,775 feet (4,199 m) [2] in Northwest Wyoming. Below its north face is Teton Glacier . The mountain is a classic destination in American mountaineering via the Owen-Spalding route (II, 5.4), the North Ridge and North Face .
South of the central Cathedral Group the Teton Range tapers off near Teton Pass and blends into the Snake River Range. [74] West to east trending canyons provides easier access by foot into the heart of the range as no vehicular roads traverse the range except at Teton Pass, which is south of the park.
Cloudveil Dome (12,031 feet (3,667 m)) is located in the Teton Range, Grand Teton National Park, Wyoming, immediately southeast of Grand Teton. [3] The peak is in the central portions of the range, immediately east of South Teton and is sometimes considered to be part of what is collectively known as the Cathedral Group.
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Mount Owen is part of the Cathedral Group of high Teton peaks, a collection of peaks in the central section of the range that are particularly rugged. The 40-mile (64 km) long Teton Range is the youngest mountain chain in the Rocky Mountains, and began its uplift 9 million years ago, during the Miocene. [5]
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