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Anthracite, also known as hard coal, and black coal, is a hard, compact variety of coal that has a submetallic luster. It has the highest carbon content, the fewest impurities, and the highest energy density of all types of coal and is the highest ranking of coals.
The United Mine Workers of America is a North American labor union best known for representing coal miners. Today, the Union also represents health care workers, truck drivers, manufacturing workers and public employees in the United States and Canada. Although its main focus has always been on workers and their rights, the UMW of today also advocates for better roads, schools, and universal health care. By 2014, coal mining had largely shifted to open pit mines in Wyoming, and there were only 60,000 active coal miners. The UMW was left with 35,000 members, of whom 20,000 were coal miners, chiefly in underground mines in Kentucky and West Virginia. However it was responsible for pensions and medical benefits for 40,000 retired miners, and for 50,000 spouses and dependents.
The Schuylkill River is a river running northwest to southeast in eastern Pennsylvania. The river was improved by navigations into the Schuylkill Canal, and several of its tributaries drain major parts of Pennsylvania's Coal Region. It flows for 135 miles (217 km) from Pottsville to Philadelphia, where it joins the Delaware River as one of its largest tributaries.
The history of coal mining goes back thousands of years, with early mines documented in ancient China, the Roman Empire and other early historical economies. It became important in the Industrial Revolution of the 19th and 20th centuries, when it was primarily used to power steam engines, heat buildings and generate electricity. Coal mining continues as an important economic activity today, but has begun to decline due to the strong contribution coal plays in global warming and environmental issues, which result in decreasing demand and in some geographies, peak coal.
The Coal strike of 1902 was a strike by the United Mine Workers of America in the anthracite coalfields of eastern Pennsylvania. Miners struck for higher wages, shorter workdays, and the recognition of their union. The strike threatened to shut down the winter fuel supply to major American cities. At that time, residences were typically heated with anthracite or "hard" coal, which produces higher heat value and less smoke than "soft" or bituminous coal.
Tuscarora State Park is a Pennsylvania state park on 1,618 acres (655 ha) in Rush, Ryan, Schuylkill Townships, Schuylkill County, Pennsylvania in the United States. The most prominent features of the park are Locust Mountain and Tuscarora Lake. The park is named for the Tuscarora Indians, who lived in the area, following the Tuscarora War in North Carolina, until they were forced out by the colonial settlers of Pennsylvania. Tuscarora State Park is 2 miles (3.2 km) west of Tamaqua just off of Pennsylvania Route 54.
Georges Creek Valley is located in Allegany County, Maryland along the Georges Creek. The valley is rich in wide veins of coal, known historically as "The Big Vein." Coal was once extracted by deep mines but is only mined today through surface mining. The Georges Creek Valley was once a major center for the US coal industry.
The South Wales Coalfield extends across Pembrokeshire, Carmarthenshire, Swansea, Neath Port Talbot, Bridgend, Rhondda Cynon Taf, Merthyr Tydfil, Caerphilly, Blaenau Gwent and Torfaen. It is rich in coal deposits, especially in the South Wales Valleys.
The Winding Gulf Coalfield is located in western Raleigh County and eastern Wyoming County, in southern West Virginia. It is named after the Winding Gulf stream, a tributary of the Guyandotte River. In the early 20th century, it was promoted as the "Billion Dollar Coalfield".
The New River Coalfield is located in northeastern Raleigh County and southern Fayette County, West Virginia. Commercial mining of coal began in the 1870s and thrived into the 20th century. The coal in this field is a low volatile coal, known as "smokeless" coals. The seams of coal that have been mined include Sewell, Fire Creek, and Beckley. This is very high quality bituminous coal rated at approximately 15,000 BTU (16,000 kJ). The New River coalfield is named after the north flowing New River. Over 60 coal towns were once located there, supported by independent commercial districts at Beckley, Oak Hill, Mount Hope, and Fayetteville. By the 21st century many coal camps had partially or completely returned to nature. These company towns were located along Dunloup (Loup) Creek, Laurel Creek, White Oak Creek, lower Piney Creek, and, of course, the New River. The mainline of the Chesapeake and Ohio Railway ran right through the center of this coalfield, with spurs branching off in many directions, and rail yards were maintained at Quinnimont, Raleigh, and Thurmond, WV. The Virginian Railway's main line also passed through the western side of the field as well. Companies such as the New River Company, New River & Pocahontas Consolidated Coal Co., and Mary Frances Coal Co. were the largest operators in the New River Coalfield, but there were many smaller ones as well. These companies recruited native born whites, immigrants from Southern and Eastern Europe, and African-Americans from the South to work in their coal mines and railroads. The mines began to close down after World War II and today there are very few active coal mines in the field. The New River Gorge is now the domain of the National Park Service as the New River Gorge National Park and Preserve, and they have done what their budget allows to preserve the coal heritage of the area.
Pocahontas Coalfield, which is also known as the Flat Top-Pocahontas Coalfield, is located in Mercer County/McDowell County, West Virginia and Tazewell County, Virginia. The earliest mining of coal in the coalfield was in Pocahontas, Virginia in 1883 at Pocahontas Mine No. 1, now on the National Register of Historic Places.
The Logan Coalfield is a coalfield located in Logan County and Wyoming County of southern West Virginia, in the Appalachia region of the eastern United States.
Coal mining regions are significant resource extraction industries in many parts of the world. They provide a large amount of the fossil fuel energy in the world economy.
The Pittsburgh Coalfield is the largest of the Western Pennsylvania coalfields. It includes all or part of Allegheny, Fayette, Greene, Washington, and Westmoreland Counties in Pennsylvania. Coal has been mined in Pittsburgh since the 18th century. U.S. Steel and Bethlehem Steel owned Karen, Maple Creek, and Ellsworth mines. It is not possible to define sharp geographical boundaries for this district for none such exist or are reported differently. The largest company in this field was the Pittsburgh Coal Company, which later became CONSOL Energy. It is bordered on the west by the state of West Virginia, on the south by Panhandle Coalfield and Klondike Coalfield, on the East by Irwin Gas Coalfield, on the North by the Freeport Coalfield and at least one other coalfield. The Darr Mine Disaster occurred in this coalfield in 1907.
The history of coal mining in the United States goes back to the 1300s, when the Hopi Indians used coal. The first commercial use came in 1701, within the Manakin-Sabot area of Richmond, Virginia. Coal was the dominant power source in the United States in the late 1800s and early 1900s, and although in rapid decline it remains a significant source of energy in 2019.
Kay Moor, also known as Kaymoor, is the site of an abandoned coal mine, coal-processing plant, and coal town near Fayetteville, West Virginia. The town site is located in the New River Gorge at Kaymoor Bottom (38°03′00″N81°03′17″W). It is linked to the mine portal 560 feet (170 m) above on Sewell Bench (38°02′52″N81°03′58″W) in the wall of the Gorge by conveyors.
The Pittsburgh Coal Seam is the thickest and most extensive coal bed in the Appalachian Basin; hence, it is the most economically important coal bed in the eastern United States. The Upper Pennsylvanian Pittsburgh coal bed of the Monongahela Group is extensive and continuous, extending over 11,000 mi2 through 53 counties. It extends from Allegany County, Maryland to Belmont County, Ohio and from Allegheny County, Pennsylvania southwest to Putnam County, West Virginia.
People have worked as 'coal miners for centuries, but they became increasingly important during the Industrial revolution when coal was burnt on a large scale to fuel stationary and locomotive engines and heat buildings. Owing to coal's strategic role as a primary fuel, coal miners have figured strongly in labor and political movements since that time.
There are two types of coal found in Pennsylvania: anthracite and bituminous. Anthracite coal is a natural mineral with a high carbon and energy content that gives off light and heat when burned, making it useful as a fuel. It was possibly first used in Pennsylvania as a fuel in 1769, but its real history begins with a documented discovery near Summit Hill and the founding of the Lehigh Coal Mine Company in 1792 to sporadically send expeditions to the wilderness atop Pisgah Ridge to mine the deposits, mostly with notable lack of great success, over the next 22 years. The owners of this company were absentee management—reliant on teams of workers sent under a foreman to fell timber to build so called 'Arks', then mine coal around nine miles from the right bank Lehigh, then trek with mule loads to fill the boats for the trip down the rapid strewn Lehigh River, and then more than 60 miles (97 km) to the Lehigh Valley docks on the unimproved often log choked
The Richmond Basin was one of the Eastern North America Rift Basins. It lies over Swift Creek Reservoir from Interstate 64 to the Appomattox River.
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