This article needs additional citations for verification .(July 2014) |
Curwensville Lake | |
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Location | Clearfield County, Pennsylvania, United States |
Coordinates | 40°57′15″N78°31′36″W / 40.95417°N 78.52667°W |
Type | reservoir |
Basin countries | United States |
Surface elevation | 1,240 ft (380 m) |
Curwensville Lake is a reservoir [1] [ failed verification ] located just to the south of the town of Curwensville, Pennsylvania. The lake was formed due to the construction of the Curwensville Dam to the north of the lake. Before the dam was built, there were several floods occurring along the West Branch Susquehanna River, affecting the towns of Curwensville, and Clearfield to the north. On September 3, 1954 a Flood Control Act was passed due to the flooding along the West Branch river basin. The dam cost $20,400,000 to construct.
Curwensville is a borough in Clearfield County, Pennsylvania, United States, 45 miles (72 km) north of Altoona on the West Branch Susquehanna River. Coal mining, tanning, and the manufacture of fire bricks were the industries at the turn of the 20th century. In 1900, 1,937 people lived in the borough, and in 1910, 2,549 lived there. As of the 2020 U.S. census, the borough had a population of 2,567. The population of the borough at its highest was 3,422 in 1940.
The Susquehanna River is a major river located in the Mid-Atlantic region of the United States, overlapping between the lower Northeast. At 444 miles (715 km) long, it is the longest river on the East Coast of the United States. By watershed area, it is the 16th-largest river in the United States, and also the longest river in the early 21st-century continental United States without commercial boat traffic.
The Chattahoochee River forms the southern half of the Alabama and Georgia border, as well as a portion of the Florida and Georgia border. It is a tributary of the Apalachicola River, a relatively short river formed by the confluence of the Chattahoochee and Flint rivers and emptying from Florida into Apalachicola Bay in the Gulf of Mexico. The Chattahoochee River is about 430 miles (690 km) long. The Chattahoochee, Flint, and Apalachicola rivers together make up the Apalachicola–Chattahoochee–Flint River Basin. The Chattahoochee makes up the largest part of the ACF's drainage basin.
The Clutha River is the second longest river in New Zealand and the longest in the South Island. It flows south-southeast 338 kilometres (210 mi) through Central and South Otago from Lake Wānaka in the Southern Alps to the Pacific Ocean, 75 kilometres (47 mi) south west of Dunedin. It is the highest volume river in New Zealand, and the swiftest, with a catchment of 21,000 square kilometres (8,100 sq mi), discharging a mean flow of 614 cubic metres per second (21,700 cu ft/s). The river is known for its scenery, gold-rush history, and swift turquoise waters. A river conservation group, the Clutha Mata-Au River Parkway Group, is working to establish a regional river parkway, with a trail, along the entire river corridor.
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 Trinity River is a 710-mile (1,140 km) river, the longest with a watershed entirely within the U.S. state of Texas. It rises in extreme northern Texas, a few miles south of the Red River. The headwaters are separated by the high bluffs on the southern side of the Red River.
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 Farmington River is a river, 46.7 miles (75.2 km) in length along its main stem, located in northwest Connecticut with major tributaries extending into southwest Massachusetts. The longest route of the river, from the origin of its West Branch, is 80.4 miles (129.4 km) long, making it the Connecticut River's longest tributary by 2.3 miles (3.7 km) over the major river directly to its north, the Westfield River. The Farmington River's watershed covers 609 square miles (1,580 km2). Historically, the river played an important role in small-scale manufacturing in towns along its course, but it is now mainly used for recreation and drinking water.
Anderson Creek is a 23.6-mile-long (38.0 km) tributary of the West Branch Susquehanna River in Clearfield County, Pennsylvania, in the United States.
The Piscataquog River is a 34.7-mile-long (55.8 km) river located in southern New Hampshire in the United States. It is a tributary of the Merrimack River, which flows to the Gulf of Maine.
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 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.
Sinnemahoning State Park is a 1,910-acre (773 ha) Pennsylvania state park in Grove Township, Cameron County and Wharton Township, Potter County, Pennsylvania, in the United States. The park is surrounded by Elk State Forest and is mountainous with deep valleys. The park is home to the rarely seen elk and bald eagle. Sinnemahoning State Park is on Pennsylvania Route 872, eight miles (13 km) north of the village of Sinnamahoning. In 1958, the park opened under the direction of the Pennsylvania Bureau of Forestry: it became a Pennsylvania State Park in 1962.
Pennsylvania Route 453 is a 43.8-mile-long (70.5 km) state highway located in Huntingdon, Blair, and Clearfield counties in Pennsylvania. The southern terminus is at U.S. Route 22 (US 22) in Water Street; the northern terminus is at PA 879 in Curwensville.
West Hill Dam Reserve is a United States Army Corps of Engineers flood control project with a recreational park and wildlife management area located at Uxbridge, Massachusetts. The West Hill Dam Project was completed in June 1961. It is located on the West River, one of the branches of the Blackstone River which flows from Worcester, MA to Providence, RI. The West River originates in Grafton, Massachusetts, at Cider Mill Pond and Silver Lake, near Upton, Massachusetts, and the Upton State Forest. The dam is unusual in that it isn't filled unless there is a flood. West Hill Dam was built after devastating floods during the 1950s; it is intended to protect the Blackstone Valley from future destructive flooding. The cities and towns downriver from Uxbridge, including Millville, Blackstone, Woonsocket, North Smithfield, Cumberland, Lincoln, Central Falls, Pawtucket and Providence, Rhode Island, suffered extensive flooding from the Blackstone during Hurricane Diane in 1955. Hurricane Donna tested this new dam in 1960 as the eyewall passed over. The West Hill Dam is located in the Blackstone River Valley National Heritage Corridor near the Blackstone River and Canal Heritage State Park. Park rangers provide visitor assistance and offer scheduled interpretative programs. Fishing, hunting, and wildlife viewing opportunities are available year-round. The park has a recreation area, 34 picnic sites, one playground, a swimming area and five miles of hiking trails. However, access to the park from West Hill Road is currently blocked as of 2021 because of landowner disagreements. West Hill Dam is also the field office for the Charles River Natural Valley Storage Area. It consists of scattered wetlands in the upper and middle Charles River watershed, between the towns of Bellingham and Needham. The wetlands provide flood storage area, fisheries, wildlife management, and recreation. The Charles River is the well-known watercourse that flows into Boston Harbor.
Curwensville Dam is located on the West Branch Susquehanna River about 0.6 miles (1 km) upstream from Curwensville in Clearfield County, Pennsylvania. The dam is an earth fill structure 2,850 feet long, rising 131 feet above the stream bed, with a spillway and gate-controlled outlet.
The Zoar Trail is a 6.5-mile (10.5 km) Blue-Blazed hiking trail "system" in the lower Housatonic River valley in Fairfield County, Connecticut and is entirely in the Sandy Hook section of Newtown in the lower block of Paugussett State Forest.
First Fork Sinnemahoning Creek is a tributary of Sinnemahoning Creek in the U.S. state of Pennsylvania.