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A white quartz dike, which angles across the gorge halfway up the falls, is the result of hot silica- rich liquid escaping from within the earth 400 million years ago. The liquid forced itself upwards along a weakness in the gorge. The water of the brook has cut away enough rock to make the seam visible. (from The BerkshireWeb)
Posted by: Nick Cannata 27-May-2007 07:04

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