*Note: Please make sure to right-click and print (or save) ID card located in the photo gallery for your records*
Fibrous sussexite and mooreite are rare and classic minerals found together in the historic zinc-manganese-iron ore deposits of the Sterling Hill Mine and surrounding Franklin Mining District in Sussex County, New Jersey. A manganese borate mineral (Mn²⁺BO₂(OH)) that commonly occurs in silky, fibrous or asbestiform veinlets traversing the ore. It was named after Sussex County, New Jersey.
In daylight, fibrous sussexite typically appears as silky white, gray veins. Under ultraviolet (UV) light, it remains inert (dark). However, it frequently cuts right through masses of calcite and willemite, creating non-glowing, distinct fibrous paths that break up the bright colors of the matrix.
The Franklin-Ogdensburg area is a world-famous type locality for hundreds of unique mineral species, many of which are fluorescent. It's known as the "Fluorescent Mineral Capital of the World".
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.