| Bullhead Lake | |
|---|---|
 Bullhead Lake, looking towards Mount Grinnell | |
  Bullhead Lake  Bullhead Lake | |
| Location | Glacier National Park, Glacier County, Montana, US |
| Coordinates | 48°47′10″N113°44′04″W / 48.78611°N 113.73444°W , |
| Lake type | Natural |
| Primary outflows | Swiftcurrent Creek |
| Basin countries | United States |
| Surface elevation | 5,184 ft (1,580 m) [1] |
Bullhead Lake is located in Glacier National Park, in the U. S. state of Montana. Mount Wilbur is North of Bullhead Lake.
Glacier County is located in the U.S. state of Montana. As of the 2020 census, the population was 13,778. The county is located in northwestern Montana between the Great Plains and the Rocky Mountains, known to the Blackfeet as the "Backbone of the World". The county is geographically and culturally diverse and includes the Blackfeet Indian Reservation, Glacier National Park, and Lewis and Clark National Forest. The county is bordered by 75 miles of international boundary with two ports of entry open year-round and one seasonal international border crossing into Alberta, Canada.
Flathead County is a county located in the U.S. state of Montana. At the 2020 census, its population was 104,357, making it the state's fourth most populous county. Its county seat is Kalispell. Its numerical designation is 7. Its northern border is on the state's north border, making it contiguous with the Canada–US border, facing British Columbia.
Glacier National Park is an American national park located in northwestern Montana, on the Canada–United States border, adjacent to Waterton Lakes National Park in Canada—the two parks are known as the Waterton-Glacier International Peace Park. The park encompasses more than 1 million acres (4,100 km2) and includes parts of two mountain ranges, more than 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem," a region of protected land encompassing 16,000 sq mi (41,000 km2).
The Waterton-Glacier International Peace Park is the union of Waterton Lakes National Park in Canada and Glacier National Park in the United States. Both parks are declared Biosphere Reserves by UNESCO and their union as a World Heritage Site.
Grinnell Lake is located in Glacier National Park, in the U. S. state of Montana. Named after George Bird Grinnell, the lake has an opaque turquoise appearance from the rock flour (silt) which is transported to the lake from Grinnell Glacier. Grinnell Lake is accessible via the Grinnell Glacier Trail and is 3.2 miles (5.1 km) from the Many Glacier Hotel. It lies below the north face of Angel Wing.
Chenango Valley State Park is a 1,137-acre (4.60 km2) state park located in Broome County, New York in the United States. The park is located adjacent to the Chenango River in western part of the Town of Fenton.
Bullhead Lake may refer to:
The Lewis Range is a mountain range located in the Rocky Mountains of northern Montana, United States and extreme southern Alberta, Canada. It was formed as a result of the Lewis Overthrust, a geologic thrust fault resulted in the overlying of younger Cretaceous rocks by older Proterozoic rocks. The range is located within Waterton Lakes National Park in Alberta, Canada and Glacier National Park and the Bob Marshall Wilderness Complex in Montana, United States. The highest peak is Mount Cleveland at 10,479 ft (3,194 m).
Swiftcurrent Lake is located in the Many Glacier region of Glacier National Park, in the U.S. state of Montana. The Many Glacier Hotel, the largest hotel in the park, is along the east shore of the lake. Many hiking trails originate from the area and scenic tour boats provide access to the lake for visitors.
Lake Sherburne is located in the Many Glacier region of Glacier National Park, in the U.S. state of Montana. The lake is a reservoir, formed by Lake Sherburne Dam, which held back Swiftcurrent Creek and was constructed between 1914 and 1921. The construction of the dam filled up several small lakes and highly productive river transition and wetland areas, and due to its fluctuating water levels, the surrounding area supports little vegetation. However, trumpeter swans are often observed along the lake in the spring and fall. The lake stretches nearly 6 mi (9.7 km) when full. The reservoir is the principal water storage component of the U.S. Bureau of Reclamation's Milk River Project, which provides irrigation water to north central Montana farms.
Glacier View Wilderness is a 3,073-acre (1,244 ha) wilderness adjacent to the west side of Mount Rainier National Park in Washington state. It was designated as wilderness in 1984. Glacier View Wilderness has views of the glaciated slopes of Mount Rainier which lies to the east. This includes viewing points from Mt. Belijica and Glacier View Point. Glacier View Point is the former site of a fire lookout built in 1934. The wilderness is administered by the Gifford Pinchot National Forest through the Cowlitz Valley Ranger district with headquarters located in Randle, Washington.
Babb is a small unincorporated farming and ranching community in Glacier County, Montana, United States, on the Blackfeet Indian Reservation. The community experiences a large influx of tourists in the summer months as it is the gateway to the Many Glacier area of Glacier National Park. For statistical purposes, the United States Census Bureau has defined Babb as a census-designated place (CDP). It had a population of 174 at the 2010 census.
Mount Grinnell is a peak located in the heart of Glacier National Park in the U.S. state of Montana. Lying just east of the Continental Divide in the Many Glacier region of the park, the peak is flanked to the northwest by Swiftcurrent Glacier and to the south by Grinnell Glacier. Mount Grinnell is named after George Bird Grinnell. From the Many Glacier Hotel on Swiftcurrent Lake, the eastern arm of Mount Grinnell, known as Grinnell Point, hides the main summit.
The following is an alphabetical list of articles related to the U.S. state of Montana.
Lake Great Falls was a prehistoric proglacial lake which existed in what is now central Montana in the United States between 15,000 BCE and 11,000 BCE. Centered on the modern city of Great Falls, Montana, Glacial Lake Great Falls extended as far north as Cut Bank, Montana, and as far south as Holter Lake. At present-day Great Falls, the Glacial Lake Great Falls reached a depth of 600 feet.
Sky Top Glacier is in the Beartooth Mountains in the U.S. state of Montana. The glacier is situated at an elevation of 11,600 feet (3,500 m) in a cirque to the west of Granite Peak, the tallest summit in Montana. The glacier covers approximately 25 acres (0.10 km2) and a small proglacial lake is near the glacier terminus.
The Regional designations of Montana vary widely within the U.S state of Montana. The state is a large geographical area that is split by the Continental Divide, resulting in watersheds draining into the Pacific Ocean, Gulf of Mexico and Hudson's Bay. The state is approximately 545 miles (877 km) east to west along the Canada–United States border and 320 miles (510 km) north to south. The fourth largest state in land area, it has been divided up in official and unofficial ways into a variety of regions. Additionally, Montana is part of a number of larger federal government administrative regions.
The following low-power television stations broadcast on digital or analog channel 7 in the United States:
Lake Jordan was a glacial lake formed during the late Pleistocene along the Jordan River. After the Laurentide Ice Sheet retreated, water melting off the glacier accumulated between the Rocky Mountains and the ice sheet. The lake drained along the front of the ice sheet, eastward towards the Yellowstone River and Glacial Lake Glendive.
Lake Circle was a glacial lake that formed during the late Pleistocene epoch along the Redwater River in eastern Montana. After the Laurentide Ice Sheet retreated, glacial ice melt accumulated in the basin surrounded by the ridges of the preglacial valley and the retreating glacier. Southwest of Nickwall are the remnants of a broad abandoned valley with long side slopes. The valley runs north from Redwater Creek to the Missouri River. The bottom is poorly drained and about 1 mile (1.6 km) in width. It lies 2,015 to 2,020 feet above the sea level and 40 to 50 feet above the Missouri River bottomland. The upland slopes are extensive, clear and flat. The valleys surrounding it are dissected with V-shaped coulees. The difference between the Redwater valley and those around it reflect stream erosion vs. lake sedimentation. The drift in the valleys, appears to be as left by the glacier in the previously created valleys. Using the dating of lake deposits near Great Falls, Montana, the Havre lobe of the Laurentide Ice Sheet dammed the ancestral Missouri River during the late Wisconsin Glacial Period.
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