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Updated: June 4, 2025
The changes are usually such as the heat of melted matter and of the entangled steam and gases might be expected to cause. A striking example, near Plas-Newydd, in Anglesea, has been described by Professor Henslow. Strata of shale and argillaceous limestone, through which it cuts perpendicularly, are altered to a distance of 30, or even, in some places, of 35 feet from the edge of the dike.
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