When hiking around Hungry Horse you are in a Ranger District that is located near the western boundary of Glacier National Park and northeast of Flathead Lake. Get driving directions here.
The Hungry Horse Ranger District contains the Hungry Horse Dam and Reservoir – a popular recreation site and important nesting habitat for bald eagles.
Hiking around Hungry Horse
The district also contains a portion of the Jewel Basin Hiking Area, the Middle and South Forks of the Flathead River, and the Great Bear Wilderness.

Hungry Horse Ranger Station is located 22 miles northeast of Kalispell, MT and 10 miles south of Glacier National Park. The telephone number is 406-387-3800 and they are located at 10 Hungry Horse Drive, Hungry Horse, MT 59919.
A popular campground near Hungry Horse Reservoir is Murray Bay Campground. It is located high in the Rocky Mountains. Less than 30 miles from the Continental Divide, surrounded by towering mountain peaks. Visitors can expect a variety of recreational activities, including, fishing, boating, swimming, hiking, exploring and big game hunting. The campground is 22 miles south of Martin City on the east shore of Hungry Horse Reservoir. This campground has a 16 day stay limit. Please leash your pets at all times when visiting.
Hike Flathead Lake on Phillips Trail #373. Phillips Trail #373 is 3.8 miles long and climbs about 600 feet; it intersects with Crane Mtn Road #498 and the
This short, family friendly 0.4 mile loop interpretive Flathead Lake trail. The short but steep distance down to excellent view of Flathead Lake and the western skyline. This trail was developed in partnership with the Bigfork High School.
The Flathead Lake Bear Dance Trail is 6.7 miles long and climbs about 2,200 feet. It begins off of Highway # 35 from the Beardance Trailhead and follows Forest Road #10222 and terminates at Crane Mountain Road #498. The trail is open to: hiking, horseback riding, and mountain biking.
Directions: From Bigfork go south on Highway 35 past Woods Bay and turn right after mile marker 23, entering the Beardance trailhead parking. The trailhead is on the east side of the highway.
Glacier National Park is named for the glaciers that produced its landscape. A glacier is a moving mass of snow and ice. It forms when more snow falls each winter than melts in the summer. The snow accumulates and presses the layers below it into ice. The bottom layer of ice becomes flexible and therefore allows the glacier to move. As it moves, a glacier picks up rock and gravel. With this mixture of debris, it scours and sculptures the land it moves across. This is how, over thousands of years, Glacier National Park got all its valleys, sharp mountain peaks, and lakes. There are more than 50 glaciers in the park today, though they are smaller than the huge ones that existed 20,000 years ago.
The park is unique among US parks in its relationship with the Waterton Lakes National Park in Alberta, Canada. The two parks meet at the border shared by the two countries. Though administered by separate countries, the parks are cooperatively managed in recognition that wild plants and animals ignore political boundaries and claim the natural and cultural resources on both sides of the border. In 1932, the parks were designated the first International Peace Park in recognition of the bonds of peace and friendship between the two nations. The two parks jointly share the name The Waterton-Glacier International Peace Park. Then, in 1995, The Waterton-Glacier International Peace Park was designated for inclusion as a World Heritage Site.
Recent archaeological surveys have found evidence of human use dating back over 10,000 years. These people may have been the ancestors of tribes that live in the area today. By the time the first European explorers came to this region, several different tribes inhabited the area. The Blackfeet Indians controlled the vast prairies east of the mountains. The Salish and Kootenai Indians lived and hunted in the western valleys. They also traveled east of the mountains to hunt buffalo.
The construction of the Going-to-the-Sun Road was a huge undertaking. Even today, visitors to the park marvel at how such a road could have been built. The final section of the Going-to-the-Sun Road, over Logan Pass, was completed in 1932 after 11 years of work. The road is considered an engineering feat and is a National Historic Landmark. It is one of the most scenic roads in North America. The construction of the road forever changed the way visitors would experience Glacier National Park. Future visitors would drive over sections of the park that previously had taken days of horseback riding to see.