Colyer, Pennsylvania | |
|---|---|
  Colyer Location within the U.S. state of Pennsylvania | |
| Coordinates: 40°47′03″N77°40′33″W / 40.78417°N 77.67583°W | |
| Country | United States |
| State | Pennsylvania |
| County | Centre |
| Township | Potter |
| Time zone | UTC-5 (Eastern (EST)) |
| • Summer (DST) | UTC-4 (EDT) |
| GNIS feature ID | 1203313 [1] |
Colyer is a small unincorporated community south of the borough of Centre Hall in central Potter Township, Centre County, Pennsylvania, United States.
The community takes its name from Colyer's Sawmill, which once stood near the intersection of Bubb and Colyer Roads. A combined general store/post office was located nearby, but was converted to a private residence in the late 1940s. Of three churches that originally operated within Colyer's boundaries, only the Colyer Brethren in Christ (BIC) Church maintains an active congregation.
Within the Colyer geographic area is Colyer Lake, a 77-acre body of water supported by the Colyer Lake Dam. [2] Constructed in the late 1960s by the Commonwealth of Pennsylvania's Fish & Boat Commission, the dam was extensively renovated in 2017, at which time a 2.5-mile hiking trail that traverses the entire perimeter of the lake was opened to the public. [3]
The Yadkin River is one of the longest rivers in the US state of North Carolina, flowing 215 miles (346 km). It rises in the northwestern portion of the state near the Blue Ridge Parkway's Thunder Hill Overlook. Several parts of the river are impounded by dams for water, power, and flood control. The river becomes the Pee Dee River at the confluence of the Uwharrie River south of the community of Badin and east of the town of Albemarle. The river then flows into South Carolina near Cheraw, which is at the Fall Line. The entirety of the Yadkin River and the Great Pee Dee River is part of the Yadkin-Pee Dee River Basin.
Orson is a village in Preston Township, Wayne County, Pennsylvania, United States, situated in the Lake Region of the Poconos. It was once an important depot of the Scranton Division of the New York, Ontario & Western (O&W) Railway, but today, when it is known outside of its immediate vicinity, it is largely for being the site of the intersection of two state roads, Belmont Turnpike and Crosstown Highway, or as the location of Independent Lake Camp (ILC), since ILC's reputation and commercial reach, like those of most rural American summer camps, extend beyond the community in which the camp is physically located.
Greenwood Furnace State Park is a 423-acre (171 ha) Pennsylvania state park in Jackson Township, Huntingdon County, Pennsylvania in the United States. The park is near the historic iron making center of Greenwood Furnace. The park includes the ghost town of Greenwood that grew up around the ironworks, old roads and charcoal hearths. Greenwood Furnace State Park is adjacent to Rothrock State Forest and on the western edge of an area of Central Pennsylvania known as the Seven Mountains. The park is on Pennsylvania Route 305, 20 miles (32 km) south of State College.
Harveys Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 14.5 miles (23.3 km) long and flows through Harveys Lake, Lake Township, Lehman Township, Jackson Township, and Plymouth Township. The creek's watershed has an area of 46.3 square miles (120 km2). The creek has four named tributaries, which are known as Bear Hollow Creek, Paint Spring Run, Pikes Creek, and East Fork Harveys Creek. The watershed is designated as a High-Quality Coldwater Fishery and a Migratory Fishery above Pikes Creek and as a Coldwater Fishery and a Migratory Fishery below it. The creek's source is Harveys Lake, the largest natural lake in Pennsylvania.
Black Moshannon State Park is a 3,480-acre (1,410 ha) Pennsylvania state park in Rush Township, Centre County, Pennsylvania, United States. It surrounds Black Moshannon Lake, formed by a dam on Black Moshannon Creek, which has given its name to the lake and park. The park is just west of the Allegheny Front, 9 miles (14 km) east of Philipsburg on Pennsylvania Route 504, and is largely surrounded by Moshannon State Forest. A bog in the park provides a habitat for diverse wildlife not common in other areas of the state, such as carnivorous plants, orchids, and species normally found farther north. As home to the "largest reconstituted bog in Pennsylvania", it was chosen by the Pennsylvania Department of Conservation and Natural Resources for its "25 Must-see Pennsylvania State Parks" list.
Prince Gallitzin State Park is a 6,249-acre (2,529 ha) Pennsylvania state park with acreage in both Chest and White Townships in Cambria County of West Central Pennsylvania in the United States, near both Gallitzin Borough, & Gallitzin Township in the greater Altoona, Pennsylvania area.
Ravensburg State Park is a Pennsylvania state park in Crawford Township in Clinton County, Pennsylvania in the United States. It is in a gorge carved by Rauchtown Run through the side of Nippenose Mountain. Ravensburg State Park is 78 acres (32 ha) of wooded land that is almost entirely surrounded by Tiadaghton State Forest. This state park is on Pennsylvania Route 880, 8 miles (13 km) north of Carroll and 8 miles (13 km) south-east of Jersey Shore. The nearest city is Williamsport.
Poe Valley State Park is a 620-acre (251 ha) Pennsylvania state park in Penn Township, Centre County, Pennsylvania in the United States. The park is surrounded by Bald Eagle State Forest. Poe Paddy State Park is 4 miles (6.4 km) to the east. The forests of the park surround the 25-acre (10 ha) Poe Lake. Poe Valley State Park is in isolated Poe Valley which lies between Potters Mills on U.S. Route 322 and Millheim on Pennsylvania Route 45. The park was closed during the 2008 and 2009 season while the lake was drained for dam repairs and the park facilities were upgraded.
Gouldsboro State Park is a 2,880-acre (1,165 ha) Pennsylvania state park in Coolbaugh Township, Monroe County and Lehigh Township, Wayne County, Pennsylvania in the United States. The park includes the 250-acre (100 ha) Gouldsboro Lake. Gouldsboro State Park is located very close to Tobyhanna State Park and Pennsylvania State Game Lands 127 and 312. It is on Pennsylvania Route 507 near the small village of Gouldsboro.
Parker Dam State Park is a 968-acre (392 ha) Pennsylvania state park in Huston Township, Clearfield County, Pennsylvania in the United States. The park is surrounded by Moshannon State Forest. Parker Dam State park is 17 miles (27 km) north of Clearfield on Pennsylvania Route 153 just off exit 111 of Interstate 80. The park was constructed during the Great Depression by the Civilian Conservation Corps; they built many of the facilities that are in use today at Parker Dam State Park.
R. B. Winter State Park is a Pennsylvania state park on 695 acres (281 ha) in Hartley Township, Union County, Pennsylvania in the United States. It is in the ridge and valley region of Pennsylvania and is surrounded by Bald Eagle State Forest. R. B. Winter State Park is in a shallow basin that is surrounded by ridges. Halfway Lake is the central recreational focus of the park. The park is 18 miles (29 km) west of Lewisburg on Pennsylvania Route 192.
Penns Valley is an eroded anticlinal valley of the Pennsylvania ridge and valley geologic region of the Appalachian Mountain range. The valley is located in southern Centre County, Pennsylvania. Along with the Nittany Valley to the north and east, it is part of the larger Nittany Anticlinorium. It is bordered by Mount Nittany to the north, the Seven Mountains range to the south, and connects to the larger Nittany Valley to the west. There are two smaller subordinate valleys typically associated with the greater valley: Georges Valley in the south, separated by Egg Hill, and Brush Valley in the north, separated by Brush Mountain.
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 and is entirely in the Sandy Hook section of Newtown in the lower block of Paugussett State Forest.
Lake Chillisquaque is a lake and reservoir in Montour County, Pennsylvania, in the United States. It has a surface area of 165 acres. The lake is situated on Middle Branch Chillisquaque Creek, which it is named after. Nearby communities include Danville and Washingtonville. The lake has an elevation of 567 feet (173 m) above sea level and is up to 40 feet (12 m) deep. It has several coves, including Goose Cove, Heron Cove, and Jellyfish Cove. The lake is dammed on its southern side by the Lake Chillisquaque Dam, which is 2,000 feet (610 m) long and 54 feet (16 m) high. The metals with the highest concentrations are calcium and iron. Nonmetals such as nitrogen and phosphorus are also found in the lake. It experiences agricultural runoff as well.
Spring Brook is a tributary of the Lackawanna River in Lackawanna County and Luzerne County, in Pennsylvania, in the United States. It is approximately 17 miles (27 km) long and flows through Covington Township, Spring Brook Township, and Moosic in Lackawanna County and Pittston Township in Luzerne County. The watershed of the stream has an area of 57.2 square miles (148 km2). It is designated as a High-Quality Coldwater Fishery and a Migratory Fishery above Interstate 476 and as a Coldwater Fishery and a Migratory Fishery below it. A section is also designated as Class A Wild Trout Waters. The stream's tributaries include Panther Creek, Plank Bridge Creek, Rattlesnake Creek, Green Run, Monument Creek, and Covey Swamp Creek. It has a relatively high level of water quality and is very slightly acidic, with a pH of 6.4 to 6.9.
Covey Swamp Creek is a tributary of Spring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 2.2 miles (3.5 km) long and flows through Moosic. Dams in the watershed of the creek include the Glenwood Lake Dam, the Covey Dam, and the Stark Dam. All three dams have associated reservoirs. The creek is a small mountain stream.
White Oak Run is a tributary of Roaring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 2.3 miles (3.7 km) long and flows through Jefferson Township, Madison Township, and Roaring Brook Township. The watershed of the stream has an area of 3.22 square miles (8.3 km2). The stream flows through the Curtis Reservoir, which is dammed by the Curtis Dam. The surficial geology in the vicinity of the stream's mouth includes alluvium, Wisconsinan Till, and bedrock.
Lake Run is a tributary of Roaring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 1.6 miles (2.6 km) long and flows through Covington Township. The watershed of the stream has an area of 3.44 square miles (8.9 km2). It has one named tributary, which is known as Emerson Run. Lake Run is considered to be Class A Wild Trout Waters. The surficial geology in its vicinity consists of Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, Boulder Colluvium, alluvium, bedrock, sand and gravel pits, fill, wetlands, peat bogs, and a lake.
The West Branch Lackawanna River is a tributary of the Lackawanna River in Susquehanna County, Pennsylvania, in the United States. It is approximately 9.5 miles (15.3 km) long and flows through Ararat Township, Herrick Township, and Union Dale. The watershed of the river has an area of 16.8 square miles (44 km2). The river is not designated as an impaired stream and it has a high level of water quality. Lakes and wetlands in the river's watershed include Ball Lake, Fiddle Lake, Hathaway Lake, Lake Romobe, Lewis Lake, Lowe Lake, and Sink Hole Swamp. The river is also dammed by at least two dams: the Romobe Lake Dam and the Hathaway Pond Dam.
Partners Creek is a tributary of Tunkhannock Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately 6.4 miles (10.3 km) long and flows through Harford Township and Lenox Township. The watershed of the creek has an area of 5.84 square miles (15.1 km2). The creek has one named tributary, which is known as Sterling Brook. The drainage basin of Partners Creek is classified as a Coldwater Fishery and a Migratory Fishery. The surficial geology in the vicinity of the creek consists of Wisconsinan Till, alluvium, bedrock, wetlands, lakes, and alluvial fan.
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