FRANKLIN AND STERLING HILL NEW JERSEY: THE WORLD'S MOST MAGNIFICENT MINERAL DEPOSITS
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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


QUARTZ

 

The feldspar group

ALBITE

ANORTHITE

ANORTHOCLASE

CELSIAN

HYALOPHANE

MICROCLINE

OLIGOCLASE

ORTHOCLASE

 

The scapolite group

MARIALITE

MEIONITE

 

The zeolite group

ANALCIME

CHABAZITE

HEULANDITE

LAUMONTITE

NATROLITE

STILBITE

THOMSONITE

 

Silicates with unknown structures

BOSTWICKITE

NEOTOCITE

WAWAYANDAITE

ANORTHOCLASE

(Na,K)AlSi3O8 
Triclinic

Anorthoclase, a sodium potassium aluminum silicate mineral of the feldspar group, was first reported from Franklin by Palache (1935), who gave an analysis, said by Frondel et al. (1966) to be of impure material and thus not repeated here. Frondel (1972) noted that anorthoclase occurs as brownish granular masses in the calcium silicate units of the orebody and is less common than hyalophane. It has not been reported from Sterling Hill and has not been studied by the writer.

 

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CHAPTER 19. TECTOSILICATES AND SILICATES WITH UNKNOWN STRUCTURE