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Updated: May 1, 2025
Between it and its walk of gneiss occur veins of the minerals so characteristic of the locality, and for which it has become famous serpentine, asbestos, phlozopite, gurhofite pyrites, biotite, aragonite, dolomite, tremolite, and possibly others in lesser quantity. Serpentine.
Phlozopite. In a vein near the lower end of the quarry, near the asbestos locality, occurs large plates of this mineral, which is a variety of mica, and has all of the characteristics of a pure silvery white color, and from one by three inches in area to less. It is easily separable in folia, and cannot be confounded with any of the other minerals.
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