• The Cathedral Group from the Teton Park Road

    Grand Teton

    National Park Wyoming

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  • Bears are active in Grand Teton

    Black and grizzly bears are roaming throughout the park--near roads, trails and in backcountry areas. Hikers and backcountry users are advised to travel in groups of three or more, make noise and carry bear spray. Visitors must stay 100 yards from bears. More »

  • Multi-use Pathway Closures

    Intermittent closures of the park Multi-use Pathway System will occur through mid-October during asphalt sealing and safety improvement work. Pathway sections will reopen as work is completed. Follow the link for a map and more information. More »

  • Moose-Wilson Road Status

    The Moose-Wilson Road between the Death Canyon Road and the Murie Center Road is currently open to all traffic. The road may re-close at any time due to wildlife activity. For current road conditions call 307-739-3682. More »

Park Rangers Investigating the Discovery of Dead Coyote & Red Fox

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Date: January 24, 2014
Contact: Public Affairs Office, 307.739.3393

Park rangers began an investigation into the circumstances surrounding the presence of two wildlife carcasses—one coyote and one red fox— lying  alongside the road near Gros Ventre Junction and just east of Highway 26/89/191 within Grand Teton National Park.

Around 7 a.m. Friday morning, January 24, several passersby called the Teton Interagency Dispatch Center to report that two animal carcasses were located near Gros Ventre Junction. Park rangers arrived shortly after these initial calls and began an investigation to determine how these two animals died and why their carcasses were located near each other at the junction.

If anyone has further information about this incident, please phone Grand Teton's Park Watch line at 307.739.3677. Callers can remain anonymous.

Did You Know?

Close-up of a lodgepole pine cone

Did you know that lodgepole pine trees grow on glacial moraines in Jackson Hole? Glacial moraines are ridges of rocky debris left behind as Ice Age glaciers melted. The soil on these ridges retains moisture and is more hospitable to trees than the cobbly, porous soil on the outwash plain.