Anthracite mined on the generally flat lying and undeformed sedimentary rocks further west on the Allegheny Plateau of Kentucky and West Virginia, Eastern Ohio, and Western Pennsylvania. In the same way the anthracite region of South Wales is confined to the contorted portion west of Swansea and Llanelli, the central and eastern portions producing steam coal, coking coal and domestic house coals. Structurally, anthracite shows some alteration by the development of secondary divisional planes and fissures so that the original stratification lines are not always easily seen. The thermal conductivity is also higher; a lump of anthracite feels perceptibly colder when
History of anthracite coal mining in Pennsylvania the building of a canal. By 1840, over 250,000 tons of anthracite mined from the region annually reached Philadelphia through White and Hazard’s Lehigh River system (Dublin, Licht, 12-3). A group of Germans wanted to seek the rights to the Schuylkill River. They received a charter in 1815 to incorporate the Schuylkill Navigation Company, which would have control over the Schuylkill River. After receiving investors the Schuylkill Navigation Company was able to finance a 108-mile long river and canal system that connected the Pottsville area to Philadelphia that opened in 1825. By the early 1840s, some 500,000 tons of anthracite