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Profile: Salt & Chemicals
In West Virginia, Native Americans would boil water from a salt spring along the Kanawha River. By 1797, a salt furnace in the Kanawha Valley at Campbell's Creek provided European-American pioneers with the means of curing butter and meat. In the early 19th century, drilling hundreds of feet into the valley had tapped salt brine, and soon there were 52 furnaces furled by coal in the "Kanawha Salines." The furnace operators united to form the Kanawha Salt Company which regulated quality and price, and discouraged foreign competition. A flood in 1861 and Civil War destruction reduced salt production to one furnace. The valley revived as a chemical producer during World War I when German imports ceased. In 1914, a plant to produce chlorine and caustic acid from salt brine opened in South Charleston. From this beginning, a large chemical industry grew up in the Kanawha Valley. During World War II, an industry arose extracting salt from rock salt deposits in first Marshall and then also Tyler counties. (see WV Geological History)
In 1833 the Pennsylvania Mainline Canal carried four million pounds of salt out of the Valley. However, the 1830s proved the high point of Conemaugh-Kiskiminetas salt production. Production continued elsewhere in western Pennsylvania, and salt wells contaminated by oil helped turn attention to the possibilities of petroleum production from deep wells. The resources needed to keep saltworks producing in the 19th century had a deleterious effect on the mountain environment, according to historian Donald Edward Davis. Of greatest consequence to the local environment were the large amounts of coal and timber needed to fuel the saltworks' continuously burning fires. The mining of coal seams precipitated acid runoff in mountain streams and the cutting of cordwood aided in the further clearing of mountain woodlands, intensifying soil erosion and the siltation of creeks and rivers. Where There Are Mountains, An Environmental History of the Southern Appalachians p. 155.
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