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


SOROSILICATES

The epidote group

ALLANITE-(Ce)

CLINOZOISITE

EPIDOTE

HANCOCKITE

PIEMONTITE


Other sorosilicates

BARYLITE

BARYSILITE

CUSPIDINE

FERROAXINITE

GANOMALITE

HARDYSTONITE

HEMIMORPHITE

JUNITOITE

KENTROLITE

MANGANAXINITE

NASONITE

PUMPELLYITE-(Mg)

SAMFOWLERITE

THORTVEITITE

VESUVIANITE


CYCLOSILICATES

The tourmaline group

DRAVITE

SCHORL

UVITE

 

DRAVITE

NaMg3Al6B3Si6O27(OH,F)4
Hexagonal

 
 
 
  Figure 16-26. Prismatic dravite crystals from Franklin. Specimen is 10 cm in maximum dimension. Smithsonian Institution, #R3956. Photo by Vic Krantz.  
   

Dravite, a sodium magnesium aluminum boron silicate hydroxide mineral of the tourmaline group, is uncommon at Franklin. One specimen has been analyzed and found to be dravite (Dunn et al. 1977). These crystals are dark green, 25 mm in length, composed of trigonal prisms and pedions, and markedly prismatic in habit (Figure 16-26), quite unlike the common equant habit of most Franklin uvite. They are associated with calcite and pyrrhotite from the Franklin Marble. An analysis of these crystals is given in Table 9, together with an analysis of a black ferrian dravite which occurs as massive material associated with quartz on the 1600 level of the Sterling Mine. 

 

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Copyright © 1995 by Pete J. Dunn
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CHAPTER 16. SOROSILICATES AND CYCLOSILICATES