Anthracite iron century. Research into the smelting of iron using anthracite coal (without coking it first) began in the 1820s in Wales by Thomas, experiments in France, most notably by Gueymard and Robin at Vizille in 1827, and in the 1830s in Pottsville & Mauch Chunk, Pennsylvania. Early attempts tried to gradually substitute anthracite for other fuels, such as coke or charcoal, but all failed due to the use of cold blast techniques, which generated insufficient heat to keep the anthracite in regenerative combustion. In the same time-frame, Thomas had also continued experimenting with mixes of Anthracite and other fuels, before he
History of anthracite coal mining in Pennsylvania are surrounded by sandstone ridges, which help to “protect” the anthracite (Hornberger et al., 20-2). There are four different anthracite coalfields in Pennsylvania, all located on the eastern side of the state. The Northern field is located predominantly in the Luzerne, Lackawanna, Susquehanna and Wayne Counties; the Western Middle field in Northumberland, Columbia, and Schuylkill Counties; Eastern Middle field mainly in Luzerne County but extending into Schuylkill, Carbon, and Columbia Counties; the Southern field in Carbon, Schuylkill, Lebanon, and Dauphin Counties (Latzko, 8). Anthracite differs from bituminous in usage in that it has better heat quality and fewer disadvantageous by-products,