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This Franklin specimen features large, dark reddish-brown to purplish willemite masses and crystals on a calcite matrix. The distinctive reddish-purple coloration is the origin of the collector term “grape willemite,” an unusual variety of willemite associated with the world-famous Franklin mineral deposit. This classic combination of fluorescent willemite and calcite from Franklin, New Jersey produces the green-and-red color contrast for which Franklin fluorescent minerals are internationally recognized.
Ex. Richard C. Bostwick Collection.
This specimen originates from the renowned collection of Richard C. “Dick” Bostwick, one of the foremost authorities and collectors of fluorescent minerals from Franklin and Sterling Hill, New Jersey.
Beginning his collection in 1960, Bostwick devoted more than six decades to studying, documenting, and preserving the extraordinary fluorescent mineralogy of this historic mining district. His connection to Sterling Hill extended underground. Bostwick worked at the Sterling Hill Mine during the 1970s, giving him firsthand access to and knowledge of the mines.
Over his lifetime, Bostwick assembled what has been recognized as the world’s largest reference collection of fluorescent minerals from Franklin and Sterling Hill. His contributions to the field were ultimately honored with induction into the Fluorescent Mineral Society Hall of Fame, and the rare Franklin mineral bostwickite was named in recognition of his contributions.