Anthracite and it is found most abundantly in areas that have been subjected to considerable stresses and pressures, such as the flanks of great mountain ranges. Anthracite is associated with strongly deformed sedimentary rocks that were subjected to higher pressures and temperatures (but short of metamorphic conditions) just as bituminous coal is generally associated with less deformed or flat-lying sedimentary rocks. For example, the compressed layers of anthracite that are deep mined in the folded Ridge and Valley Province of the Appalachian Mountains of the Coal Region of East-central Pennsylvania are extensions of the same layers of bituminous coal that are
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