Steven Dutch, Professor Emeritus, Natural and Applied Sciences, Universityof Wisconsin - Green Bay
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Northern entry to Grand Teton National Park on U.S. 89. Below: looking south along Jackson Lake with the Tetons in the distance. |
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Above: northern peaks of the Tetons. Left and below: looking south along the Teton front. |
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Left: Mount Moran |
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The Tetons near Mount Moran |
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Left and below: Grand Teton |
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Foothills of the Absaroka Range east of the Tetons. |
Views from U.S. 26 coming down off the Absaroka Range.
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Left: looking south along the Absaroka Range Below: The northern Teton Range |
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Panorama from just east of Jackson Lake. The two highest peaks are Grand Teton (left) and Mount Moran (right). The straight front of the range is a fault. The range is made up of Archean gneiss and Proterozoic granite, mantled by Paleozoic rocks around the northern, western and southern edges and deeply sculpted by glaciation.
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Panoramas of the Tetons across Jackson Lake
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Left and below: Mount Moran |
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Left and below: between Mount Moran and Grand Teton, showing spectacular glacial topography. The Tetons are possibly the most "Alpine" mountain range in the United States. |
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Below: Grand Teton | Readers are invited to look up "teton" in a French dictionary. |
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Left and below: South of Grand Teton. |
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Looking north along the Teton front. The highest peak is Grand Teton. |
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Southern part of the Tetons |
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Looking south along the Teton front |
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Created 14 July 2003, Last Update 07 June 2020