Seasonal road closures in effect
Seasonal road closures are in effect for motorized vehicles. The Teton Park Road is closed from the Taggart Lake Trailhead to the Signal Mountain Lodge. The Moose-Wilson Road is closed from the Granite Canyon Trailhead to the Death Canyon Road. More »
Avalanche hazards exist in the park
Avalanche hazards exist in the park, especially in mountain canyons and on exposed slopes. A daily avalanche forecast can be found at www:jhavalanche.org or by calling (307) 733-2664. More »
Scattering of Ashes Permit
Complete the Special Use Permit Application (short form) or SUP Application (long form) and submit it to the Grand Teton National Park Fee Office at least 10 business days before the planned date for scattering ashes.
Your request will be evaluated based on the information in your application. Applicants should attach maps, diagrams, and other information that might assist park staff in evaluating the application.
Mail or fax the completed application to:
fax (307) 739-3492
Restrictions & Conditions
A Special Use Permit does not allow the permittee to restrict park visitors from any location; therefore, sites which attract a large number of visitors should be avoided. Normal visitor use patterns will not be interrupted and are only allowed as specified in the approved permit. Permit activities may not occur simultaneously with other permitted activities or unduly conflict with scheduled public activities.
Permit activities may be restricted based on weather or seasonal conditions (fire danger, standing water, nesting season, road closures, etc.). Additional closures, use limits and /or restricted activities are listed in the Superintendent's Compendium.
Activities that may damage, significantly impact, or alter park resources are prohibited. The following are also prohibited:
Restrictions and conditions enumerated in the permit generally include the following:
Did You Know?
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.