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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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.
The Richmond Basin is a rift basin, making a north to south double pointed oval, with the eastern edge over the Swift Creek Reservoir, with the northern point at interstate 64, spanning the James River, with the southern point at the Appomattox River.
The Richmond Basin is 205 to 245 million years old. Pangea divided and many small rifts split opened in the earth in addition to the large one that became the Atlantic Ocean. When Richmond rift opened and filled with swamps from water in the Pamunkey River, sediment filled in over the swamps and the sedimentary pressure converted organic plant material into coal. This weight is less pressure than coal deposits produced when the continents were pushing together and raising up mountains. Semi-anthracite and anthracite are often formed by such tectonic squeezing when continents push together. The Richmond Basin has Bituminous coal, formed by the sedimentary weight only. [1]
The coal deposits were on a thin shale and sandstone layer over the granite bedrock. Oolite or small round grains of calcium carbonate was over the coal. Some coke with and without sulphur was with the coal. [2]
To the northwest of the basin is the Goochland Terrane, and between them is the Boscobel complex. [3]
The Richmond Basin is located near Midlothian, Virginia, in Chesterfield County, Virginia. It was mined in the early 18th century. Coal was carried on the Chesterfield Railroad in gravity and mule-pulled carts to Manchester, Richmond, Virginia and Richmond, Virginia. Wood burning trains, such as the Clover Hill Railroad then the Brighthope Railway transported the coal found at Clover Hill in later years. The coal from Midlothian, Virginia was mainly used in Richmond, Virginia and Petersburg, Virginia. The Clover Hill Pits in Winterpock, Virginia were sold as far away as New York City from the 1840s to the 1890s. [4] [5] The supply was not as great and as cheap to mine as the Pocahontas coalfield, however and mining the Richmond Basin was ended around 1890. Richmond and Petersburg grew economically because of manufacturing supported by the James River and Appomattox River waterpower, more than from coal brought out of Midlothian and Clover Hill." [1]
Chesterfield County is located just south of Richmond in the Commonwealth of Virginia. The county's borders are primarily defined by the James River to the north and the Appomattox River to the south. Its county seat is Chesterfield Court House.
The Appomattox River is a tributary of the James River, approximately 157 miles (253 km) long, in central and eastern Virginia, named for the Appomattocs Indian tribe who lived along its lower banks in the 17th century. It drains a cotton and tobacco-growing region of the Piedmont and coastal plain southwest of Richmond.
The Greater Richmond Region, the Richmond metropolitan area or Central Virginia, is a region and metropolitan area in the U.S. state of Virginia, centered on Richmond. The U.S. Office of Management and Budget (OMB) defines the area as the Richmond, VA Metropolitan Statistical Area, a Metropolitan Statistical Area (MSA) used by the U.S. Census Bureau and other entities. The OMB defines the area as comprising 17 county-level jurisdictions, including the independent cities of Richmond, Petersburg, Hopewell, and Colonial Heights. As of 2016, it had a population of 1,263,617, making it the 45th largest MSA in the country.
The Chesterfield Railroad was located in Chesterfield County, Virginia. It was a 13-mile (21-kilometer) long mule-and-gravity powered line that connected the Midlothian coal mines with wharves that were located at the head of navigation on the James River just below the Fall Line at Manchester. It began operating in 1831 as Virginia's first common carrier railroad.
Midlothian is an unincorporated area in Chesterfield County, Virginia, U.S. Settled as a coal town, Midlothian village experienced suburbanization effects and is now part of the western suburbs of Richmond, Virginia south of the James River in the Greater Richmond Region. Because of its unincorporated status, Midlothian has no formal government, and the name is used to represent the original small Village of Midlothian and a vast expanse of Chesterfield County in the northwest portion of Southside Richmond served by the Midlothian post office.
The Southside of Richmond is an area of the Metropolitan Statistical Area surrounding Richmond, Virginia. It generally includes all portions of the City of Richmond that lie south of the James River, and includes all of the former city of Manchester. Depending on context, the term "Southside of Richmond" can include some northern areas of adjacent Chesterfield County, Virginia in the Richmond-Petersburg region. With minor exceptions near Bon Air, VA, the Chippenham Parkway forms the border between Chesterfield County and the City of Richmond portions of Southside, with some news agencies using the term "South Richmond" to refer to the locations in Southside located in the city proper.
Chesterfield County Public Schools is the public school system of Chesterfield County, Virginia, United States. As of 2020, there are about 63,000 students enrolled in 64 schools. There are 39 elementary schools, 12 middle schools, and 11 high schools. Additionally, high school students can enroll in 13 specialty centers, two technical centers, and two Governor's Schools.
The Richmond and Petersburg Railroad moved passengers and goods between Richmond and Petersburg from 1838 to 1898. It survived the American Civil War and eventually merged into the Atlantic Coast Line Railroad in 1900.
Black Heath was a house and coal mine located along the Old Buckingham Road in the present Midlothian area of Chesterfield County, Virginia. The Black Heath coal mining enterprises were operated by the Heth family between 1785 and 1844, when the mine closed following a fatal explosion.
The geology of Massachusetts includes numerous units of volcanic, intrusive igneous, metamorphic and sedimentary rocks formed within the last 1.2 billion years. The oldest formations are gneiss rocks in the Berkshires, which were metamorphosed from older rocks during the Proterozoic Grenville orogeny as the proto-North American continent Laurentia collided against proto-South America. Throughout the Paleozoic, overlapping the rapid diversification of multi-cellular life, a series of six island arcs collided with the Laurentian continental margin. Also termed continental terranes, these sections of continental rock typically formed offshore or onshore of the proto-African continent Gondwana and in many cases had experienced volcanic events and faulting before joining the Laurentian continent. These sequential collisions metamorphosed new rocks from sediments, created uplands and faults and resulted in widespread volcanic activity. Simultaneously, the collisions raised the Appalachian Mountains to the height of the current day Himalayas.
Eppington is a historic plantation house located near Winterpock, Chesterfield County, Virginia. It was built about 1768, and consists of a three-bay, 2+1⁄2-story, central block with hipped roof, dormers, modillion cornice, and flanking one-story wings in the Georgian style. It has a later two-story rear ell. It features two tall exterior end chimneys which rise from the roof of the wings. It was listed on the National Register of Historic Places in 1969.
In 1886, Randolph Harrison, of the Virginia department of Agriculture, cited Cumberland Mining Company, stating that the United States had purchased stock in the Brighthope Railway. He continued by citing their assertion that extending the railway into Cumberland would increase the value of farms there because they could sell consumer agricultural products such as fruit, dairy and vegetables to all markets of Virginia. The Brighthope Railway was founded in 1877 by the creditors of the Clover Hill Railroad who bought that railroad when the Clover Hill Railroad went bankrupt. The Brighthope Railway continued in the role of the Clover Hill Railroad, hauling coal from the Clover Hill Pits at Winterpock, Virginia. In addition to coal, the Bright Hope Railway transported timber and agricultural products and had passenger service. The Bright Hope Railway was narrowed from standard gauge to narrow gauge and rerouted in 1881. In 1886, much of the southern rails were changed to standard gauge. The Brighthope Railway was not changed back.
The Clover Hill Railroad was a railroad company that operated for 36 years in central Virginia near Richmond. The railroad was created to carry coal most efficiently from the Clover Hill Pits in Winterpock, Virginia, to further transportation points in Chester, Virginia, where it could be sold for a better price than on the Appomattox River in the Piedmont region. This made the railroad important to the Confederacy in the Civil War to ensure a supply of coal for munitions and iron working. The mines were dangerous for the miners, and many accidents occurred. The railroad had to be sold when coal mining declined so that new owners could find other uses for the railroad.
The Clover Hill Pits are a number of coal shafts and mines that operated in the Southside area of Richmond, Virginia from 1837 until around 1883.
The Farmville and Powhatan Railroad went bankrupt in 1905 and became the Tidewater and Western Railroad. The line survived until 1917 when it was pulled up and sent to France for the World War I effort. The Tidewater and Western Railroad carried freight and passengers along a route from Farmville, Virginia to Bermuda Hundred. The Tidewater and Western Railroad continued to have Western Union Telegraphs run along the rails. These connected to telegraphs on the Atlantic Coast Line along the East Coast of the US and to Europe.
The Upper Appomattox Canal Navigation system allowed farmers who took their wheat and corn to mills on the Appomattox River, as far way as Farmville, Virginia, to ship the flour all the way to Petersburg from 1745 to 1891. The system included a navigation, modifications on the Appomattox River, a Canal around the falls Petersburg, and a turning basin in Petersburg to turn their narrow long boats around, unload the farm products from upstream and load up with manufactured goods from Petersburg. In Petersburg, workers could put goods on ships bound for the Chesapeake Bay and load goods from far away for Farmville and plantations upstream. Canal boats would return up river with manufactured goods. People who could afford it, rode in boats on the canal as the fastest and most comfortable ride. The river was used for transportation and shipping goods for over 100 years.
The geology of Virginia began to form 1.8 billion years ago and potentially even earlier. The oldest rocks in the state were metamorphosed during the Grenville orogeny, a mountain building event beginning 1.2 billion years ago in the Proterozoic, which obscured older rocks. Throughout the Proterozoic and Paleozoic, Virginia experienced igneous intrusions, carbonate and sandstone deposition, and a series of other mountain building events which defined the terrain of the inland parts of the state. The closing of the Iapetus Ocean, to form the supercontinent Pangaea added additional small landmasses, some of which are now hidden beneath thick Atlantic Coastal Plain sediments. The region subsequently experienced the rifting open of the Atlantic Ocean in the Mesozoic, the development of the Coastal Plain, isolated volcanism and a series of marine transgressions that flooded much of the area. Virginia has extensive coal, deposits of oil and natural gas, as well as deposits of other minerals and metals, including vermiculite, kyanite and uranium.
The Richmond Coalfield was the first coalfield to be mined commercially in the United States of America. The coalfield is located several miles west of the city of Richmond, Virginia. Its bituminous coal seams are a part of the Richmond Basin, dating to the Late Triassic.
The Boscobel complex is unit of interlayered granite and gneiss within Goochland and Powhatan Counties, Virginia. The area had been mapped as the Petersburg Granite in 1970 by B. K. Goodwin.