Wilkes-Barre is a city in and the county seat of Luzerne County, Pennsylvania, United States. Located at the center of the Wyoming Valley in Northeastern Pennsylvania, it had a population of 44,328 in the 2020 census. It is the second-largest city, after Scranton, in the Scranton–Wilkes-Barre–Hazleton, PA Metropolitan Statistical Area, which had a population of 567,559 as of the 2020 census, making it the fifth-largest metropolitan area in Pennsylvania after the Delaware Valley, Greater Pittsburgh, the Lehigh Valley, and Greater Harrisburg.
Luzerne County is a county in the Commonwealth of Pennsylvania. According to the United States Census Bureau, the county has a total area of 906 square miles (2,350 km2), of which 890 square miles (2,300 km2) is land and 16 square miles (41 km2) is water. It is Northeastern Pennsylvania's second-largest county by total area. As of the 2020 census, the population was 325,594, making it the most populous county in the northeastern part of the state. The county seat and most populous city is Wilkes-Barre. Other populous communities include Hazleton, Kingston, Nanticoke, and Pittston. Luzerne County is included in the Scranton–Wilkes-Barre–Hazleton Metropolitan Statistical Area, which has a total population of 555,426 as of 2017. The county is part of the Northeastern Pennsylvania region of the state.
Plains Township is a township in Luzerne County, Pennsylvania, United States. The population was 9,816 at the 2020 census. The municipality is the birthplace of Chicago White Sox hall of famer Ed Walsh and John J. Yeosock, a United States Army general who commanded the 3rd U.S. Army during Operation Desert Shield and Operation Desert Storm. Mohegan Pennsylvania is a casino in Plains Township.
White Haven is a borough in Luzerne County, Pennsylvania, United States. It is located along the Lehigh River. The population was 1,163 at the 2020 census.
Penobscot Knob, also Penobscot Mountain, is a summit that is located in the western fringe of the Poconos nearest to Mountain Top, Pennsylvania. The Solomon Gap pass below it contains an important multi-modal transportation corridor.
The Wyoming Valley is a historic industrialized region of Northeastern Pennsylvania. The region is historically notable for its influence in helping fuel the American Industrial Revolution with its many anthracite coal-mines. As a metropolitan area, it is known as the Scranton–Wilkes-Barre metropolitan area, after its principal cities, Scranton and Wilkes-Barre. With a population of 567,559 as of the 2020 United States census, it is the fifth-largest metropolitan area in Pennsylvania, after the Delaware Valley, Greater Pittsburgh, the Lehigh Valley, and the Harrisburg–Carlisle metropolitan statistical areas.
The Lackawanna & Wyoming Valley Railroad, more commonly known as the Laurel Line, was a Pennsylvania third rail electric interurban streetcar line which operated commuter train service from 1903 to 1952, and freight service until 1976. Its main line ran from Scranton to Wilkes-Barre.
Northeastern Pennsylvania is a region of the U.S. state of Pennsylvania that includes the Pocono Mountains, the Endless Mountains, and the industrial cities of Scranton, Wilkes-Barre, Pittston, Hazleton, Nanticoke, and Carbondale. A portion of this region is located in the New York City metropolitan area. Recently, Pennsylvania tourism boards have described Northeastern Pennsylvania as Upstate Pennsylvania.
The Luzerne County Historical Society is one of the oldest continually operating local historical societies in America. It was founded on February 11, 1858, in recognition of the 50th anniversary of the first successful burning of anthracite coal by Jesse Fell, and was originally named the Wyoming Historical and Geological Society. The organization operates the historic Swetland Homestead in Wyoming, Pennsylvania and the Luzerne County Museum which also features a separate research library in Wilkes-Barre, Pennsylvania. It also administers the Nathan Denison house.
Charles Miner was an anti-slavery advocate and politician who served in the Pennsylvania State House of Representatives from 1807 to 1808 and the United States House of Representatives from 1825 to 1829. He was a member of the Federalist Party. During his terms in Congress, he proposed to end the slave trade in the District of Columbia and gradually abolish slavery across the city.
The history of coal mining in the United States starts with the first commercial use in 1701, within the Manakin-Sabot area of Richmond, Virginia. Coal was the dominant power source in the late 1800s and early 1900s, and although in rapid decline it remains a significant source of energy in 2024.
Duryea Yard is a railroad yard in the Wyoming Valley region of Northeastern Pennsylvania currently operated by the Reading Blue Mountain and Northern Railroad. Originally constructed in 1870 by Lehigh Valley Railroad as a turn-around and staging hub for coal transport from the Coal Region to Eastern big-city markets, the yard remains a hub for the energy extraction industry today.
The Wyoming Division Canal was an anthracite canal in Luzerne County, Pennsylvania, in the United States. It was a branch of the North Branch Canal, which was one of only two major canals in Pennsylvania to be owned by the state. The creek went from West Nanticoke to Pittston, going through Luzerne County.
Solomon Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 8.8 miles (14.2 km) long and flows through Fairview Township, Hanover Township, and Wilkes-Barre. The creek is affected by acid mine drainage and has significant loads of iron, aluminum, and manganese. The creek's named tributaries are Spring Run, Sugar Notch Run, and Pine Creek. The Solomon Creek watershed is located in the Anthracite Valley section of the ridge-and-valley geographical province. Major rock formations in the watershed include the Mauch Chunk Formation, the Spechty Kopf Formation, and the Catskill Formation.
There are two types of coal found in Pennsylvania: anthracite, the hard coal found in Northeastern Pennsylvania below the Allegheny Ridge southwest to Harrisburg, and bituminous, the soft coal found west of the Allegheny Front escarpment). Anthracite coal is a natural mineral with a high carbon and energy content that gives off light and heat produced energy when burned, making it useful as a fuel. It was possibly first used in Pennsylvania as a fuel in 1769, but its history begins with a documented discovery near Summit Hill and the founding of the Lehigh Coal Mine Company in 1792 to periodically send expeditions to the wilderness atop Pisgah Ridge to mine the deposits, mostly with notable lack of great success, over the next 22 years.
Coal Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 2.9 miles (4.7 km) long and flows through Plymouth Township and Plymouth. The watershed of the creek has an area of 1.46 square miles (3.8 km2). A reservoir known as Spring Brook Reservoir Number Four is situated on the creek. The surficial geology near the creek includes Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, alluvium, coal dumps, and bedrock consisting of sandstone and shale. On July 3, 2011, Coal Creek flooded when 5 inches (13 cm) of rain fell in the watershed in less than 90 minutes. The flood caused $5 million in damage. The creek is designated as a Coldwater Fishery and a Migratory Fishery.
The Westmoreland Club is a private social club that was established in 1873 in Wilkes-Barre, Pennsylvania. Members are Northeastern Pennsylvania "leaders in the arts, business, education, government, and industry”.
Haystack Mountain (Pennsylvania), is an otherwise non-descript 1871 ft peak forming the steep southwestern faces of the Solomon Gap mountain pass's saddle connecting and dividing the Wyoming Valley from the Lehigh Valley.
Plymouth, Pennsylvania, sits on the west side of Pennsylvania's Wyoming Valley, wedged between the Susquehanna River and the Shawnee Mountain range. Just below the mountain are hills that surround the town and form a natural amphitheater that separates the town from the rest of the valley. Below the hills, the flat lands are formed in the shape of a frying pan, the pan being the Shawnee flats, once the center of the town's agricultural activities, and the handle being a spit of narrow land extending east from the flats, where the center of town is located. At the beginning of the 19th century, Plymouth's primary industry was agriculture. However, vast anthracite coal beds lay below the surface at various depths, and by the 1850s, coal mining had become the town's primary occupation.
Plymouth, Pennsylvania sits on the west side of Pennsylvania's Wyoming Valley, wedged between the Susquehanna River and the Shawnee Mountain range. Just below the mountain are hills that surround the town and form a natural amphitheater that separates the town from the rest of the valley. Below the hills, the flat lands are formed in the shape of a frying pan, the pan being the Shawnee flats, once the center of the town's agricultural activities, and the handle being a spit of narrow land extending east from the flats, where the center of town is located. At the beginning of the 19th century, Plymouth's primary industry was agriculture. However, vast anthracite coal beds lay below the surface at various depths, and by the 1850s, coal mining had become the town's primary occupation.
