| Braden River | |
|---|---|
 Braden River near bridge at 53rd Avenue East | |
 | |
| Location | |
| Country | United States |
| Physical characteristics | |
| Mouth | |
• location | Manatee River |
| Length | 21 mi (34 km) |
| Basin size | 83 sq mi (210 km2) |
The Braden River is a 21-mile (34 km) waterway that drains an 83-square-mile (210 km2) area watershed in west-central Florida and is the largest tributary of the Manatee River.
The hydrology of the Braden River was altered in 1936 when the city of Bradenton created Ward Lake, a reservoir with an 838-foot (255 m) broad-crested weir 6 miles (9.7 km) upstream from the mouth. In 1985 the reservoir was expanded and supplies an annual average of 5.7 million US gallons (22,000 m3) of water per day. [1]
The Braden River can be hydrologically divided into three distinct sections that include an 8.6-mile (13.8 km) reach of naturally incised, free-flowing channel; a 6.4-mile (10.3 km) reach of impounded river created by the Ward Lake reservoir and weir; and a 6-mile (9.7 km) reach of tidal estuary. [1]
The Eastern Continental Divide, Eastern Divide or Appalachian Divide is a hydrological divide in eastern North America that separates the easterly Atlantic Seaboard watershed from the westerly Gulf of Mexico watershed. The divide nearly spans the United States from south of Lake Ontario through the Florida peninsula, and consists of raised terrain including the Appalachian Mountains to the north, the southern Piedmont Plateau and lowland ridges in the Atlantic Coastal Plain to the south. Water including rainfall and snowfall, lakes, streams and rivers on the eastern/southern side of the divide drains to the Atlantic Ocean; water on the western/northern side of the divide drains to the Gulf of Mexico. The ECD is one of six continental hydrological divides of North America which define several drainage basins, each of which drains to a particular body of water.
The Apalachicola River is a river, approximately 160 miles (260 km) long, in the state of Florida. The river's large watershed, known as the Apalachicola, Chattahoochee and Flint (ACF) River Basin, drains an area of approximately 19,500 square miles (50,500 km2) into the Gulf of Mexico. The distance to its farthest head waters in northeast Georgia is approximately 500 miles (800 km). Its name comes from Apalachicola Province, an association of Native American towns located on what is now the Chattahoochee River. The Spanish included what is now called the Chattahoochee River as part of one river, calling all of it from its origins in the southern Appalachian foothills down to the Gulf of Mexico the Apalachicola.
The Pit River is a major river draining from northeastern California into the state's Central Valley. The Pit, the Klamath and the Columbia are the only three rivers in the U.S. that cross the Cascade Range.
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 Caloosahatchee River is a river on the southwest Gulf Coast of Florida in the United States, approximately 67 miles (108 km) long. It drains rural areas on the northern edge of the Everglades, east of Fort Myers. An important link in the Okeechobee Waterway, a manmade inland waterway system of southern Florida, the river forms a tidal estuary along most of its course and has become the subject of efforts to restore and preserve the Everglades.
The Chilkoot River is a river in Southeast Alaska, United States, that extends about 20 miles (32 km) from its source and covers a watershed area of 100 square miles (260 km2). The source of the river is in the Takshanuk Mountains to the west and the Freebee glacier and unnamed mountains to the east. From its source, the upper reach of the river extends approximately 16 miles (26 km) to the point where it enters Chilkoot Lake. From the downstream end of the lake, the lower reach of the river flows for about 1.5 miles (2.4 km) until it enters the Chilkoot Inlet, a branch at the northern end of the Lynn Canal.
The Little Sandy River is a tributary of the Ohio River in northeastern Kentucky in the United States. It is 85.4 miles (137.4 km) long drains an area of 724.2 square miles (1,876 km2). Via the Ohio, it is part of the Mississippi River watershed.
The Bull Run River is a 21.9-mile (35.2 km) tributary of the Sandy River in the U.S. state of Oregon. Beginning at the lower end of Bull Run Lake in the Cascade Range, it flows generally west through the Bull Run Watershed Management Unit (BRWMU), a restricted area meant to protect the river and its tributaries from contamination. The river, impounded by two artificial storage reservoirs as well as the lake, is the primary source of drinking water for the city of Portland, Oregon.
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 Manatee River is a 36-mile-long (58 km) river in Manatee County, Florida. The river forms in the northeastern corner of Manatee County and flows into the Gulf of Mexico at the southern edge of Tampa Bay.
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.
The Klamath Basin is the region in the U.S. states of Oregon and California drained by the Klamath River. It contains most of Klamath County and parts of Lake and Jackson counties in Oregon, and parts of Del Norte, Humboldt, Modoc, Siskiyou, and Trinity counties in California. The 15,751-square-mile (40,790 km2) drainage basin is 35% in Oregon and 65% in California. In Oregon, the watershed typically lies east of the Cascade Range, while California contains most of the river's segment that passes through the mountains. In the Oregon-far northern California segment of the river, the watershed is semi-desert at lower elevations and dry alpine in the upper elevations. In the western part of the basin, in California, however, the climate is more of temperate rainforest, and the Trinity River watershed consists of a more typical alpine climate.
Deep Creek is a tributary of Pine Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately 22.9 miles (36.9 km) long and flows through Barry Township, Hegins Township, and Hubley Township. Its watershed has an area of 31.80 square miles (82.4 km2). Major tributaries of the creek include Hans Yost Creek.
The Barre Falls Dam is located on the Ware River in Barre, Massachusetts, about 0.3 miles (0.48 km) below the junction of the river's east and west branches and 13 miles (21 km) northwest of Worcester, Massachusetts.
The Presumpscot River is a 25.8-mile-long (41.5 km) river located in Cumberland County, Maine, United States. It is the main outlet of Sebago Lake. The river provided an early transportation corridor with reliable water power for industrial development of the city of Westbrook and the village of South Windham.
Mansfield Hollow Lake is a reservoir resting on the border of Windham County and Tolland County, Connecticut. The reservoir provides drinking water for Willimantic and helps control flooding in the 159-square-mile Thames River watershed. It was created by the Mansfield Hollow Dam and is entirely contained within Mansfield Hollow State Park and the Mansfield Hollow Wildlife Area. Designed and constructed by the United States Army Corps of Engineers, the dam substantially reduces flooding along the Quinebaug, Shetucket, and Thames rivers. Construction of the project began in 1949 with completion in 1952 at a cost of US$6.5 million. The Mansfield Hollow reservoir is located within the Shetucket River Watershed and is part of the Thames River Basin. Access to the site is available from US Route 6 and State Route 195. The damsite, covering an area of 25 acres (10 ha), was listed on the National Register of Historic Places in 2003.
The Conant Brook Dam is located on Conant Brook in Monson, Massachusetts, about 7.4 miles (11.9 km) upstream from the confluence of Conant Brook and the Quaboag River. It is approximately 15 miles (24 km) east of Springfield, Massachusetts.
The Otter River is a short connecting stream in Minnesota, flowing from Boulder Lake Reservoir into Island Lake Reservoir. The stream's length is 0.17 miles (0.27 km). It is within the Cloquet River watershed, north of Duluth.
This page is about the Croton River watershed, a hydrological feature. For the component of the New York City water supply system with a similar name, see Croton Watershed
The Muscoot River is a short tributary of the Croton River in Putnam and Westchester counties in the state of New York. Approximately 6 mi (9.7 km) long and running north-to-south, it lies within the Croton River watershed and is part of the New York City water supply system's Croton Watershed.
Municipalities and communities of Manatee County, Florida, United States | ||
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| Cities |  | |
| Town | ||
| CDPs | ||
| Unincorporated communities | ||
| Ghost towns | ||
| Footnotes | ‡This populated place also has portions in an adjacent county or counties | |
| International | |
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| National | |
27°25′38″N82°26′27″W / 27.4271244°N 82.4407838°W
