| Flathead Lake | |
| Other Name: | |
| Coords: | 47.9017°N -114.1042°W |
| Location: | Lake / Flathead counties, Montana, US |
| Type: | Moraine-dammed lake |
| Outflow: | Flathead River |
| Catchment: | 8587sqmi |
| Basin Countries: | United States |
| Length: | 27.3miles |
| Width: | 15.5miles |
| Area: | 197sqmi |
| Depth: | 164.7feet |
| Max-Depth: | 370.7feet |
| Volume: | 5.56cumi |
| Shore: | 161.4miles |
| Elevation: | 2894feet |
| Residence Time: | 3.4 years |
| Islands: | Wild Horse Island
|
| Cities: | south of Kalispell, Montana;Polson, Montana |
| Pushpin Map: | Montana#USA |
| Pushpin Map Alt: | Location of Flathead Lake in Montana, USA. |
Flathead Lake (člq̓etkʷ|label=[[Montana Salish|Salish]], Kutenai: yawuʔnik̓ ʔa·kuq̓nuk)[1] is a large natural lake in northwest Montana, United States.
The lake is a remnant of the ancient, massive glacial dammed lake, Lake Missoula of the era of the last interglacial.[2] Flathead Lake is a natural lake along the mainline of the Flathead River. It was dammed in 1930 by Kerr Dam at its outlet on Polson Bay, slightly raising the lake level; the dam generates electricity.[3] The hydroelectric has been owned and operated by the Confederated Salish and Kootenai Tribes since 2015. It is one of the cleanest lakes in the populated world for its size and type.[4]
Located in the northwest corner of the state of Montana, 7miles south of Kalispell, it is approximately 30miles long and 16miles wide, covering 197sqmi. It is a similar size as Minnesota's Mille Lacs Lake, but smaller than Red Lake. It is about half the area of San Francisco Bay (main bay). It is larger in surface area than Lake Tahoe, but it is much smaller in volume due to Tahoe's depth.[5] Flathead Lake has a maximum depth of 370.7feet,[6] and an average of 164.7feet. This makes Flathead Lake deeper than the average depths of the Yellow Sea or the Persian Gulf. Flathead Lake is in a scenic part of Montana, 30miles southwest of Glacier National Park and is flanked by two scenic highways, which wind along its curving shoreline. On the west side is U.S. Route 93, and on the east, is Route 35.The lake is bordered on its eastern shore by the Mission Mountains and on the west by the Salish Mountains. The Flathead valley was formed by the glacial damming of the Flathead River and sustains a remarkably mild climate for a region located this far north and inland; the Pacific Ocean is almost 400miles to the west. The mild climate allows for cherry orchards on the east shore and vineyards for wine production on the west shore. There are also apple, pear and plum orchards around the lake as well as vegetables, hay, honey, nursery tree, Christmas tree, sod/turf, and wheat production bordering or near the lake.
The lake has an irregularly shaped shoreline and a dozen small islands cover 5.5sqmi. Wild Horse Island is the largest at . Melita Island is a 64acres island on Flathead Lake, located about one-half mile off the west lakeshore. At its highest point Melita is 80feet above water level. The closest access is from Walstad Landing (one and a half miles), a state-maintained landing off Highway 93, approximately 15 minutes north of Polson. The island is owned by the Montana Council of the Boy Scouts of America, and is home to Camp Melita Island, and is used and for other activities; there is a project for woodland rehabilitation run by the Montana Council.[7] There is also a bald eagle reserve which is protected by the Native Americans. Boy Scouts began using the island in the 1940s.[8]
Flathead Lake lies at the southern end of a geological feature called the Rocky Mountain Trench. The trench, which formed with the Rocky Mountains, extends north into the southern Yukon as a straight, steep valley, which also holds the headwaters of the Columbia River. During the last ice age this trench was filled by an enormous glacier. As the glacier moved southward it carved out the trench. The Polson Moraine, near present-day Polson, Montana, marks the southernmost extent of the glacier during the last ice age and thus is the site of the glacier's terminal moraine.[9]
The large size of the Polson Moraine indicates that the glacier stalled here for many years before retreating. As the climate warmed, a portion of the glacier in the Mission Valley receded more slowly than the main body, which kept the lake basin from being filled with sediment. Eventually this ice also melted, forming a lake behind the moraine. Once the water reached the top of this moraine dam, it began to cut a channel through it. Most moraine dammed lakes drain quickly because water cuts entirely through the moraine. Flathead Lake remained because a bedrock hill buried underneath the Polson Moraine prevented the moraine from being completely cut through so the meltwater never completely drained.[9]
At one time, probably when the valley was partially filled by a glacier, the level of Flathead Lake was about 500feet higher and drained through the valley west of Elmo, Montana, which is at the end of Big Arm Bay, bottom center in the aerial photo above. Water carved out a wide, flat-bottomed pass with a deeper, narrow channel at the south edge of the pass. The deeper channel and traces of the dry riverbed are still visible from Route 28.
The Flathead River and the Swan River (known also as the Bigfork River where it enters the lake) are the major tributaries of the five tributaries that are within the Flathead Watershed. Numerous small streams flow into the lake, particularly on the wetter east shore. The Seli’š Ksanka Qlispe’ Dam, formerly known as Kerr Dam and built near Polson, controls the top 10adj=midNaNadj=mid, generates hydroelectric power, and provides water for irrigation to support a federal irrigation project in the area.[10] Minimum outflow levels from Flathead Lake are designated by the Federal Energy Regulatory Commission (FERC) and are based on flood risk management, power generation requirements, and biological needs to support aquatic life in river systems.[11]
The lake is downstream of Hungry Horse Dam on the South Fork Flathead River.[12] The Hungry Horse Dam is managed by the Bureau of Reclamation to provide beneficial flow conditions and to provide safe passage for migrating juvenile fish to reach the Columbia River Estuary and the Pacific Ocean.[13] The Columbia River Technical Management Team makes operational recommendations to the agencies that control federal dams. Made up of representatives from four states, five federal agencies and six tribal nations, it prioritizes fish and wildlife above other system benefits.[14] The Columbia River system has 14 projects that must be operated to meet congressionally authorized purposes.[15]
Once known as "Salish Lake", this body of water was named for the Salish Indians. Early European explorers, like David Thompson, called them the Flathead Indians because of a misinterpretation of early Native American sign language.[16] In 1855 the United States (US) made the Treaty of Hellgate, by which it set aside the Flathead Reservation solely for use of the Flathead, encompassing an area including much of Flathead Lake.
The summer of 2023 saw abnormally low water levels.[17] Variations to the Flood Risk Management Plan were approved by the U.S. Army Corp of Engineers in 2024 in response to the continuing dry conditions.[18]
Flathead Lake is home to a number of native and non-native fishes, and is managed cooperatively by both Montana Fish, Wildlife and Parks and the Confederated Salish and Kootenai Tribes. The lake is inhabited by the native bull trout and cutthroat trout, as well as the non-native lake trout, yellow perch, and lake whitefish. Local residents have reported sighting other aquatic fauna in the lake as well, such as sturgeon and the Flathead Lake Monster.[19]
The non-native opossum shrimp, (Mysis diluviana), were introduced by Montana Department of Fish, Wildlife and Parks in the Flathead drainage basin to encourage production of larger kokanee salmon; they migrated into Flathead Lake and have altered the ecosystem.[20]
Fishermen had introduced lake trout 80 years prior but remained at low densities until the non-native Mysis became established. The bottom-dwelling mysids eliminated a recruitment bottleneck for lake trout by providing a deep water source of food where little was available previously. Lake trout subsequently flourished on mysids; this voracious piscivore now dominates the lake fishery. The formerly abundant kokanee were extirpated, and native bull and westslope cutthroat trout are imperiled. Predation by Mysis has shifted zooplankton and phytoplankton community size structure. Bayesian change point analysis of primary productivity (27-y time series) showed a significant step increase of 55 mg C m−2 d−1 (i.e., 21% rise) concurrent with the mysid invasion, but little trend before or after despite increasing nutrient loading. Mysis facilitated predation by lake trout and indirectly caused the collapse of kokanee, redirecting energy flow through the ecosystem that would otherwise have been available to other top predators (bald eagles).[21]
Like the majority of other nonnative species, the lake trout (Salvelinus namaycush) became established in the lake from the late 1800s-early 1900s. The introduction of lake trout has placed increased pressure on the ecologically similar threatened native bull trout (Salvelinus confluentus).[22] The semi-annual "Mack Days" Lake Trout fishing contest aims to reduce the non-native "Mackinaw trout" or lake trout populations, as well as educate people about the Flathead Lake Fisheries Management Plan.[23] [24] Since the inception of this event in 2002, over 402,000 lake trout have been harvested.[25]
In addition to these commonly-pursued game fish, the lake is also home to other native species that currently are not actively managed by government fish and wildlife agencies, including the longnose sucker (Catostomus catostomus), redside shiner (Richardsonius balteatus), and slimy sculpin (Cottus cognatus).