Buffalo Lakes | |
---|---|
Location | South Dakota, United States |
Type | Lake chain |
Primary outflows | James River |
Basin countries | United States |
Buffalo Lakes is a lake chain in South Dakota, in the United States. [1] Buffalo Lake is a large, permanent, natural lake with complex morphometry located in Marshall County, South Dakota. The main entrance to South Buffalo and Almos Lakes, then passes through a chain of Coteau Lakes before eventually flows into the James River. [2] The buffalo lakes include the North Buffalo lake and the South Buffalo lake. The South Buffalo lake has five unnamed tributaries that flow to the North Buffalo lake. Buffalo Lakes takes its name from Buffalo Township. [3] [4] The nearest city to this lake is Long hollow, South Dakota. [5]
This is a lake with a max depth of 3.6576 meters (12 feet) and a surface area of 1780 acres. The shoreline is 27.8 miles. [4]
This is similar to South Buffalo lake. It is 3.6576 meters deep at its maximum (12 feet) and a surface area of 1780 acres. The shoreline of this lake is 27.8 miles. [4]
Nowadays South Buffalo Lake is mainly used for bluegill, northern pike, walleye and yellow perch fishery. In total, 13 species of fish have been sampled in Buffalo Lake. [2]
Lake County is a county in the U.S. state of South Dakota. As of the 2020 census, the population was 11,059. Its county seat is Madison. The county was formed in 1873.
Harding County is a county in the U.S. state of South Dakota. As of the 2020 census, the population was 1,311, making it the third-least populous county in South Dakota. Its county seat is Buffalo.
Sargent County is a county in the U.S. state of North Dakota. Its county seat is Forman, and its most populous city is Gwinner. The county is named in honor of Homer E. Sargent, a 19th-century general manager of the Northern Pacific Railroad Company. The county spans an agricultural region between the James River and Red River valleys in southeastern North Dakota dotted with various sloughs, lakes, and hills.
Lake Agassiz was a large proglacial lake that existed in central North America during the late Pleistocene, fed by meltwater from the retreating Laurentide Ice Sheet at the end of the last glacial period. At its peak, the lake's area was larger than all of the modern Great Lakes combined.
The Coteau des Prairies is a plateau approximately 200 miles in length and 100 miles in width, rising from the prairie flatlands in eastern South Dakota, southwestern Minnesota, and northwestern Iowa in the United States. The southeast portion of the Coteau comprises one of the distinct regions of Minnesota, known as Buffalo Ridge. The tip of the feature starts in extreme south North Dakota.
The Belle Fourche River is a tributary of the Cheyenne River, approximately 290 miles (470 km) long, in the U.S. states of Wyoming and South Dakota. It is part of the Mississippi River watershed via the Cheyenne and Missouri rivers. In the latter part of the 19th century, the Belle Fourche River was known as the North Fork of the Cheyenne River. Belle Fourche is a name derived from French meaning "beautiful fork".
Lake of the Isles is a lake in Minneapolis, Minnesota, connected to Cedar Lake and Bde Maka Ska. The lake is part of the city's Chain of Lakes and has an area of 109 acres (0.4 km2), 2.86 miles (4.6 km) of shoreline with a little under three miles of paved walking and biking paths, and a maximum depth of 31 feet (9 m). Lake of the Isles is known for its two wooded islands, its long north arm, and the surrounding stately houses of the Kenwood, Lowry Hill, and East Isles neighborhoods.
Wilson Lake is a reservoir in the U.S. state of Kansas, on the border of Russell County and Lincoln County. Built and managed by the U.S. Army Corps of Engineers for flood control, it is also used for wildlife management and recreation. Several parks are located along its shoreline, including Wilson State Park.
Perry Lake is a US Army Corps of Engineers operated reservoir in northeast Kansas. Its primary purposes are flood control, water reserve for nearby areas and regional recreation. The lake is approximately 11,150 acres (45 km²) in size, with over 160 miles (260 km) of shoreline. Perry Lake's full multi-purpose pool elevation is 891.5 feet (271.7 m) above sea level. Perry Lake is located about 40 miles (64 km) west of Kansas City, just northwest of Lawrence, Kansas. Its close proximity to Kansas City, Lawrence, and the state capitol, Topeka, make it a very popular destination, with the nickname "Paradise on the Plains".
The Elk River Chain of Lakes Watershed, commonly known as the Chain of Lakes, is a 75-mile-long (121 km) waterway consisting of 14 lakes and connecting rivers in the northwestern section of the Lower Peninsula of the U.S. state of Michigan, which empty into Lake Michigan.
The Pemadumcook Chain of Lakes are a set of large lakes in north-central Maine in the United States.
Blue Lake Regional Park is a public park in Fairview, in the U.S. state of Oregon. The 101-acre (41 ha) park, near the south shore of the Columbia River in Multnomah County, includes many covered and uncovered picnic areas, playing fields for sports such as softball, a cross country course and infrastructure related to lake recreation including swimming, boating, and fishing. Encompassing wooded areas, three ponds, and a wetland in addition to the lake, the park is frequented by migrating birds and other wildlife. Paved paths run through the park, which is near the 40-Mile Loop hiking and biking trail. Park vegetation includes cottonwoods, willows, and other trees and shrubs as well as wetland plants such as cattails.
Lake Chaffee is a small, shallow, man-made lake located approximately 2 miles (3.2 km) northwest of the hamlet of Westford in the town of Ashford in Windham County, northeastern Connecticut. The lake has an area of 54 acres (22 ha) and a maximum depth of 11 feet (3.4 m). Its average surface elevation is 856 feet (261 m) above sea level.
Dickinson Dam is a dam in Stark County, North Dakota, one and a half miles west of the town of Dickinson.
Kanopolis Lake is a reservoir in Ellsworth County in the Smoky Hills of central Kansas, about 31 miles southwest of Salina and a few miles southeast of the town of Kanopolis. The lake is formed by Kanopolis Dam. Completed in 1948 as a flood control and water conservation project of the United States Army Corps of Engineers, the dam impounds the Smoky Hill River.
Heart Butte Dam is a dam in Grant County of southwestern North Dakota. The dam was a project of the United States Bureau of Reclamation completed in 1949, primarily for irrigation and flood control. The earthen dam is 142 feet in height and impounds the Heart River.
Stump Lake is a naturally formed lake located in Nelson County, North Dakota. It covers 15,742.4 acres, has 72.5 miles of shoreline, and has an average depth of 29.7 feet with a maximum depth of 73.3 feet. It is stocked by the North Dakota Department of Natural Resources with Walleye, Yellow Perch, and Northern Pike.
Rock Creek reservoir, also known as Scott King reservoir, is 7 miles (11 km) north of the city of Ardmore, Carter County, Oklahoma in the United States. Created in 1979, it is operated by the city of Ardmore as a water supply recreational area. The lake has a normal surface area of 232 acres (94 ha) with 5 miles (8 km) of shoreline and a mean depth of 14.5 feet (4.4 m). The lake has a capacity of 3,550 acre-feet (4,380,000 m3).
The Belgrade Lakes are a chain of lakes around Belgrade, Maine. The flow sequence is from East Pond to North Pond to Great Pond to Long Pond to Messalonskee Lake and thence via Messalonskee Stream to the Kennebec River at Waterville. The lakes have long been an important resort area for fishing, boating, and swimming; and shoreline development includes residences for individuals employed in the cities of Waterville and Augusta.
Lake Amon G. Carter is situated 6 miles south of Bowie in Montague county, Texas, and is situated on Big Sandy Creek. Lake Amon G. Carter is technically two lakes in one. The original lake was built in 1956 and has a different type of habitat than the 500-acre extension constructed in 1985. In the thirty-year gap between the original lake and the expansion there became a habitat in the original lake that does not exist in the new expansion. The lake has a surface area of 1,848 acres and a maximum depth of 50 feet. The conservation pool elevation is 920 feet above sea level.
45°37′03″N97°17′07″W / 45.61750°N 97.28528°W