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The terminology declined into unimportance as the 20th century progressed, and was probably only referred to by a few small railroads and history buffs by the 1980s. Renewed interest in industrial heritage and coal mining history has brought the old names of the coalfields before a larger audience.
The Dan River Coalfield is a coalfield in Stokes and Rockingham counties, North Carolina about which, in 1914, USGS geologist R.W. Stone wrote, "after a thorough and careful examination of the Triassic beds in the Dan River Field the conclusion is reached that there is no reason to expect to find commercially valuable coal beds in this district."
North Carolina plantation were identified by name, beginning in the 17th century. The names of families or nearby rivers or other features were used. The names assisted the owners and local record keepers in keeping track of specific parcels of land. In the early 1900s, there were 328 plantations identified in North Carolina from extant records.
In 1810, 176,000 short tons of bituminous coal, and 2,000 tons of anthracite coal, were mined in the United States. American coal mining grew rapidly in the early 1820s, doubling or tripling every decade. Anthracite mining overtook bituminous coal mining in the 1840s; from 1843 through 1868, more anthracite was mined than bituminous coal.
Coal mine in 1925. Cumnock, formerly known as Egypt, [3] is an unincorporated community in northwestern Lee County, North Carolina, United States. It lies on Cumnock Road, about a mile north of U.S. Route 421. Endor Iron Furnace is located near the community. It was listed on the National Register of Historic Places in 1974. [4]
In 1974, the Nello L. Teer Company added another layer to its activities by entering the coal mining industry. The company started a surface mining division called Webster County Coal Company. The coal stripping division started in West Virginia and Western Pennsylvania on property previously owned by the company and areas owned by established ...
Looking Glass Dome. The geology of North Carolina includes ancient Proterozoic rocks belonging to the Grenville Province in the Blue Ridge.The region experienced igneous activity and the addition of new terranes and orogeny mountain building events throughout the Paleozoic, followed by the rifting of the Atlantic Ocean and the deposition of thick sediments in the Coastal Plain and offshore waters.
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