Grand Teton

Grand Tetons / Teton Mountains

Mountains In Grand Teton National Park

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Grand Teton National Park protects stunning mountain scenery and a diverse array of wildlife. The Teton Range is the focal point of the park, the youngest range in the Rocky Mountains. An active normal fault, the Teton Fault, lies on the 40 mile long mountain front. Rock is jetted into the sky some 7,000 feet from the flat plains, with the highest peak at 13,770 feet, the Grand Teton. more info

OARS - Grand Teton Rafting & Sea Kayaking
O.A.R.S. – First-class rafting, sea kayaking & multi-sport adventure beneath the ultra-photographic Tetons with professional guides & top-notch equipment. Leaders since 1969.
view site : map : call us (800) 346-6277
Browse Hiking Trails by Region
Information & Maps on many local hiking, biking, fishing trails in the Grand Teton and Jackson Hole area.
Virtual Tour Guide: GPS enabled Yellowstone Tour - Available in ALL park gateways. The GPS guide features location specific info as you drive. Learn about widlife, ecology & the geysers.

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Charlie Sands - Scenic River Float Trips
For over 35 years we've shown more people a "good time" than anyone. U-Paddle, guided trips, dinner & overnight packages. Perfect for family groups. Exceptional safety record.
view site : map : call us (800) 358-8184
Grand Teton Wedding Photography by James Morrissey
Specializing in capturing weddings set against the spectacular backdrop of the Grand Teton range, still with prime openings this summer of 2008. See our online portfolio.
view site : call us (212) 544-9655

Cathedral Group of the Tetons in a Pine frame
Cathedral Group of the Tetons in a Pine frame
© Peter Volf Photography
The general architecture of the range is simpler than that of most great mountain ranges of the world. The peaks are sculptured from an enormous westward-tilted fault block of ancient metamorphic and igneous rocks that are part of the central core of the continent. These basement rocks were once covered by much younger sedimentary rocks that have since been stripped by erosion. The north-south trending Teton fault lies at the foot of the range. The eastern edge of the Teton block has been raised at least 8,000 feet during the last two million years at an average rate of almost 5 inches per century. This very rapid uplift, geologically speaking, has resulted in tilted stream terraces in Jackson Hole, fresh fault scarps along the base of the range and occassional earthquakes.

Details of the mountainous landscape were developed on the uplifted Teton block by alpine glaciation . An excellent example of this topography molded by glacial erosion is the "Cathedral Group" consisting of the Grand Teton, Mt. Owen and Mt. Teewinot, and can be seen from the north vantage point. In the past 2 million years, glaciers have advanced and retreated due to several cycles of climatic cooling followed by warming. The Grand Teton is also an example of a glacial horn, a result of cirque glaciers eroding headward on three or more sides of the rock mass which created these pyramid shaped peaks.

The mountains in Grand Teton National Park are not only impressive with their geological background, but also in their accessibility and the views their summits offer. Modern highways lead virtually to the foot of the peaks. The summit of the Grand Teton is a little more than three horizontal miles from the nearest approach road. The Tetons are radiant to the climbing world, offering more than 38 distinct routes to the Grand Teton's summit, the center of interest. For those whose goals do not include the making of first ascents, there is an unlimited opportunity for hiking, on or off the 220 mile trail system.

Grand Teton National Park's mountains rise at a steady high angle. These peaks, bristled with spires and pinnacles, are topped by sharp summits. Their alure and energy has brought more than 3 million visitors a year in search of their scenic splendor. Mountains represent a piece in all of us and reconnecting with that is a remarkable and unforgetable experience.

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