Definitions

from The Century Dictionary and Cyclopedia

  • n. A subvariety of magnesian carbonate of lime or dolomite, found near Gurhof in Lower Austria. It is snow-white, and has a dull, slightly conchoidal or even fracture.

Etymologies

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Examples

  • Frequently these specimens may be obtained with a layer of gurhofite above them, and separated by the serpentine; this assortment is very interesting, revealing to us the manner in which they were formed, which was by a process termed segregation.

    Scientific American Supplement, No. 415, December 15, 1883

  • Dolomite occurs to a limited extent as such; most of it, being in the form of gurhofite crystals, may be occasionally found with aragonite of

    Scientific American Supplement, No. 415, December 15, 1883

  • 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.

    Scientific American Supplement, No. 415, December 15, 1883

  • Much of the magnesite in this serpentine contains more or less lime, and is consequently in places almost pure dolomite, although crystals are seldom to be found in this outcrop, it all occurring as veins about a half-inch thick and resembling somewhat the gurhofite of Staten Island, only that it is softer and less homogeneous in appearance.

    Scientific American Supplement, No. 363, December 16, 1882

  • This gurhofite, called bone by the quarrymen, occurs in white, dense looking masses, intermingled with the serpentine, especially in the upper end of the quarry, where veins six and eight inches in thickness are abundant, and from which specimens may be readily obtained showing the fibrous structure of the gurhofite and the association with the serpentine, to which it is found attached; it is quite different from the limestone in appearance, and need not be mistaken for it.

    Scientific American Supplement, No. 415, December 15, 1883

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