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

DEVILLINE

CaCu4(SO4)2(OH)6.3H2O
Monoclinic

 
   
 

Figure 24-9. Acicular connellite crystals on sarkinite crystal from Sterling Hill. Field of view  is 0.5 mm in maximum dimension. Photograph courtesy of Tom Peters and the Paterson Museum.

 
   

Devilline, a calcium copper sulfate hydroxide hydrate mineral, was reported from Sterling Hill by Cook (1973). He found it as bluish-green coatings and feathery microcrystals associated with brochantite, linarite, and gypsum.

Devilline was subsequently reported by Jenkins and Misiur (1994) from below the 700 level at Sterling Hill. It has not been reported from Franklin. Devilline is a rare mineral locally.

 

 

 

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CHAPTER 24. SULFATES, BORATES, TUNGSTATES, AND MOLYBDATES