FRANKLIN AND STERLING HILL NEW JERSEY: THE WORLD'S MOST MAGNIFICENT MINERAL DEPOSITS
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GEOCHEMISTRY FLUORESCENCE THE MINERAL ASSEMBLAGES LISTS OF MINERALS DESCRIPTIVE MINERALOGY NESOSILICATES
SOROSILICATES AND CYCLOSILICATES INOSILICATES PHYLLOSILICATES TECTOSILICATES AND SILICATES OF UNKNOWN STRUCTURE
ELEMENTS SULFIDES ARSENIDES ANTIMONIDES AND SULFOSALTS OXIDES AND HYDROXIDES HALIDES AND CARBONATES
SULFATES BORATES TUNGSTATES AND MOLYBDATES ARSENATRES ARSENIDES PHOSPHATES AND VANADATES UNNAMED MINERALS


The sulfates

ANGLESITE

ANHYDRITE

ANTLERITE

BARITE

BASSANITE

BIANCHITE

BROCHANTITE

CELESTINE

CHARLESITE

CONNELLITE

DEVILLINE

EPSOMITE

GYPSUM

HALOTRICHITE

HAUCKITE

HEXAHYDRITE

LAWSONBAUERITE

LINARITE

MOOREITE

ORTHOSERPIERITE

SERPIERITE

SPANGOLITE

STARKEYITE

TORREYITE

The borates

FLUOBORITE

MCALLISTERITE

ROWEITE

SUSSEXITE


The tungstates and molybdates

FERRIMOLYBDITE

HUEBNERITE

POWELLITE

SCHEELITE

WULFENITE

SPANGOLITE

Cu6Al(SO4)(OH)12Cl.3H2O
Hexagonal

Spangolite, a copper aluminum sulfate hydroxide chloride hydrate mineral, was first reported from Sterling Hill by Jenkins (1993a). It occurs as aggregates of 30 micron, hexagonal, bright-green, platy crystals which were verified using X-ray diffraction methods and semi-quantitative chemical analysis methods. This spangolite was found intimately associated with brochantite “in a small, partially oxidized sulfide pod in ore near the footwall contact of the east limb of the Sterling Hill orebody.” The specific site was “on the south wall of the 740 crosscut, 800 level, at approximate mine coordinates 730N, 960W” (Jenkins, 1993a). Spangolite has not been reported from Franklin.

 

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CHAPTER 24. SULFATES, BORATES, TUNGSTATES, AND MOLYBDATES