The Cuyahoga River is a river located in Northeast Ohio that bisects the City of Cleveland and feeds into Lake Erie.
The Cumberland River is a major waterway of the Southern United States. The 688-mile-long (1,107 km) river drains almost 18,000 square miles (47,000 km2) of southern Kentucky and north-central Tennessee. The river flows generally west from a source in the Appalachian Mountains to its confluence with the Ohio River near Paducah, Kentucky, and the mouth of the Tennessee River. Major tributaries include the Obey, Caney Fork, Stones, and Red Rivers.
The West Branch Susquehanna River is one of the two principal branches, along with the North Branch, of the Susquehanna River in the Northeastern United States. The North Branch, which rises in upstate New York, is generally regarded as the extension of the main branch, with the shorter West Branch being its principal tributary.
The Feather River is the principal tributary of the Sacramento River, in the Sacramento Valley of Northern California. The river's main stem is about 73 miles (117 km) long. Its length to its most distant headwater tributary is just over 210 miles (340 km). The main stem Feather River begins in Lake Oroville, where its four long tributary forks join—the South Fork, Middle Fork, North Fork, and West Branch Feather Rivers. These and other tributaries drain part of the northern Sierra Nevada, and the extreme southern Cascades, as well as a small portion of the Sacramento Valley. The total drainage basin is about 6,200 square miles (16,000 km2), with approximately 3,604 square miles (9,330 km2) above Lake Oroville.
The Guadalupe River runs from Kerr County, Texas, to San Antonio Bay on the Gulf of Mexico, with an average temperature of 17.75 degrees Celsius. It is a popular destination for rafting, fly fishing, and canoeing. Larger cities along it include Kerrville, New Braunfels, Seguin, Gonzales, Cuero, and Victoria. It has several dams along its length, the most notable of which, Canyon Dam, forms Canyon Lake northwest of New Braunfels.
The Chippewa River is a stream in Michigan, United States, that runs 91.8 miles (147.7 km) through the central Lower Peninsula. The Chippewa is a tributary of the Tittabawassee River and is thus part of the Saginaw River drainage basin. The river is named after the Chippewa people.
The Raccoon River is a 30.8-mile-long (49.6 km) tributary of the Des Moines River in central Iowa in the United States. As measured using the longest of its three forks, its length increases to 226 miles (364 km). Via the Des Moines River, it is part of the watershed of the Mississippi River. The river runs through an intensely cultivated area of croplands and livestock farming, receiving Tile drainage from slow-draining rich natural bottomland.
Black River is a 78.8-mile-long (126.8 km) river in the U.S. state of Michigan, flowing mostly northward through four Northern Michigan counties: Otsego, Montmorency, Presque Isle, and Cheboygan. The Black River flows into the Cheboygan River at 45°36′13″N84°27′47″W, just south of the city of Cheboygan, and then into Lake Huron. The main branch of the Black River originates in Charlton Township in east-central Otsego County near the boundary with Montmorency County. The East Branch of the Black River rises less than a mile to the east in Vienna Township in Montmorency County. The other major tributaries, Canada Creek, Tomahawk Creek and the Rainy River all rise in northern Montmorency County.
Arkabutla Lake is a reservoir on the Coldwater River in the U.S. state of Mississippi. It was created following the construction of the Arkabutla Dam in 1940 on the Coldwater River.
Alum Creek is a 58-mile (93 km) long creek that runs north to south in central Ohio. The creek originates in Morrow County and then flows through Delaware County and finally into Franklin County, where it ends at Big Walnut Creek, which drains into the Scioto River. Alum Creek is a source of drinking water for the city of Westerville, Ohio.
The West River is a tributary of the Connecticut River, about 53.8 miles (86.6 km) long, in southern Vermont in the United States. According to the Geographic Names Information System, it has also been known historically as "Wantastiquet" and as "Waters of the Lonely Way". Its watershed covers 423 square miles (1,100 km2); land use is about 90% forested and 3% agricultural, and the upper river supports wild native brook and wild brown trout, while Atlantic salmon occur in most of the river.
The Ompompanoosuc River is a river, about 25 mi (40 km) long, in eastern Vermont in the United States. It is a tributary of the Connecticut River, which flows to Long Island Sound. According to the Geographic Names Information System, the river has also been known by the names "Om-pom-pa-noos-uc" and "Pompanoosuc."
The Naugatuck River is a 40.2-mile-long (64.7 km) river in the U.S. state of Connecticut. Its waters carve out the Naugatuck River Valley in the western reaches of the state, flowing generally due south and eventually emptying into the Housatonic River at Derby, Connecticut and thence 11 miles (18 km) to Long Island Sound. The Plume and Atwood Dam in Thomaston, completed in 1960 following the Great Flood of 1955, creates a reservoir on the river and is the last barrier to salmon and trout migrating up from the sea.
Pohick Creek is a 14.0-mile-long (22.5 km) tributary stream of the Potomac River in Fairfax County in the U.S. state of Virginia. It takes its name from the Pohick Native American tribe once prevalent in the area.
The Ware River is a 35.4-mile-long (57.0 km) river in central Massachusetts. It has two forks, its West Branch, which begins in Hubbardston, Massachusetts, and its East Branch, which begins in Westminster, Massachusetts. The Ware River flows southwest through the middle of the state, joins the Quaboag River at Three Rivers, Massachusetts, to form the Chicopee River on its way to the Connecticut River.
Curwensville Dam is located on the West Branch Susquehanna River about 0.6 miles (0.97 km) upstream from Curwensville in Clearfield County, Pennsylvania. The dam is an earth fill structure 2,850 feet (870 m) long, rising 131 feet (40 m) above the stream bed, with a spillway and gate-controlled outlet.
The East Branch Penobscot River is a 75.3-mile-long (121.2 km) tributary of Maine's Penobscot River. It flows in Piscataquis County and Penobscot County.
The South Branch Penobscot River is a river in Somerset County, Maine. Its source, Penobscot lake, the north end of which at is about 1,000 feet (300 m) from the Canada–United States border in Sandy Bay. This section of the border runs along the height of land separating the watersheds of the Penobscot River and the Monument River, which feeds into the Saint Lawrence River.
The Saint John Ponds are a chain of shallow lakes at the headwaters of the Baker Branch Saint John River in the North Maine Woods. The flow sequence is from the Upper First Saint John Pond, through the Lower First Saint John Pond, Second Saint John Pond, Third Saint John Pond, and Fourth Saint John Pond to the Fifth Saint John Pond. Flow from one pond to the next is sometimes called Baker Stream rather than the Baker Branch Saint John River. Great Northern Paper Company dug a canal from Fifth Saint John Pond 2 miles (3.2 km) westward to the North Branch Penobscot River in 1939, and built a dam at the north end of Fifth Saint John Pond so pulpwood logs harvested in the upper Saint John River watershed could be floated down the Penobscot River to Millinocket, Maine. The canal and dam have fallen into disrepair so most drainage from the ponds again flows down the Saint John River. All upstream ponds with the exception of the first had dams to regulate discharge flow for log driving, but those dams have similarly fallen into disrepair. Moose use the ponds as summer refuge from heat and biting insects.
The Reedsburg Dam is a non-hydroelectric barrage dam crossing the Muskegon River in eastern Missaukee County in the U.S. state of Michigan. Located in rural Enterprise Township, the dam was constructed in 1940 by the Civilian Conservation Corps to alleviate flooding from Houghton Lake, which is the source of the Muskegon River approximately 6 miles (9.7 km) upstream.
