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Groundwater conditions at Foss Mine, Aberfeldy

By B.E. O Dochartaigh


The bedrock in the Foss area forms a low or very low productivity aquifer. The\ud groundwater flow direction is likely to be northwards, and flow is likely to occur\ud dominantly in the upper few tens of metres of the bedrock. Natural groundwater\ud discharge is likely to be via springs or directly to streams on the hill slopes, or directly to\ud Loch Tummel.\u

Publisher: British Geological Survey
Year: 2004
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