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

SERPIERITE

Ca(Cu,Zn)4(SO4)2(OH)6.3H2O
Monoclinic

Serpierite, a calcium copper sulfate hydroxide hydrate mineral, was first found by David Cook in 1971 and was subsequently verified by the writer on a number of specimens. It occurs as light blue microcrystals and thin light-blue films on calcite- bearing specimens of nondescript appearance and is rare. It is known from Sterling Hill, but not from Franklin.

 

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CHAPTER 24. SULFATES, BORATES, TUNGSTATES, AND MOLYBDATES