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feed. [Illustration] Such additions are frequent for the next 45 miles or so downstream, as the North Branch in its narrow valley swells into a mountain river with the water of brooks and creeks flowing off ridges pocked with coal mines old and new. The river and such tributaries sustain no aquatic life at all among the discolored stones in their channels. This mine-derived pollution has been much studied but is still not well understood. Sulphuric acid is its most damaging component, but may be accompanied by iron salts and other substances also leached from materials in and around the vast coal beds of Appalachia. Some acid entered the streams there naturally, before men ever touched the coal, but it has increased to deadly proportions with widespread mining. It issues from both surface strip mines and the old-fashioned underground sort, though the latter furnish by far the most--an estimated 75 to 90 percent. The overall magnitude of the problem is indicated by the fact that the more than 60,000 square miles of the Appalachian region underlain by coal, including the Potomac fraction, contributes five to ten million tons of sulphuric acid annually to streams and rivers, a rate of production that is expected to continue for at least a thousand years. At Westernport the North Branch enters more populated realms, and receives one of its latter big doses of acid from Georges Creek, which drains a devastated, economically depressed valley mined since very early days. This creek may be the single most unfortunate stream in the Potomac Basin, for the accumulation of raw wastes it brings down from the valley's communities is pickled rather than assimilated by its heavily acid water. [Illustration] In the 40 or 50 miles below that point, the North Branch accumulates great quantities of more usual kinds of pollution as it runs down a broadening valley past towns and industries that have grown up because of the conjunction of coal, timber, water, and railways--and in the old days water transport, for flatboats used to shoot the river at high water, and later the C. & O. Canal operated upriver as far as Cumberland. Treatment of wastes in this reach is spotty and mainly inadequate. Some industries and towns sluice them raw into the dark, sad water, and others give only perfunctory primary treatment; the city of Cumberland releases the equivalent of about 18,000 persons' body wastes each day as effluent, besides extr
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