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 mica group

common micas

BIOTITE

HENDRICKSITE-1M

MUSCOVITE-1M

PHLOGOPITE-1M


brittle micas

ANANDITE

CLINTONITE

MARGARITE


The chlorite group

CLINOCHLORE

CHAMOSITE

PENNANTITE-1a


The stilpnomelane group

FERRISTILPNOMELANE

FERROSTILPNOMELANE

FRANKLINPHILITE

LENNILENAPEITE


The friedelite group

FRIEDELITE

MANGANPYROSMALITE

NELENITE

SCHALLERITE


The serpentine group

CLINOCHRYSOTILE

LIZARDITE

ORTHOCHRYSOTILE


The clay group

FRAIPONTITE

ILLITE

KAOLINITE

NONTRONITE

SAUCONITE


Other layer silicates

BANNISTERITE

BEMENTITE

CARYOPILITE

CHRYSOCOLLA

FLUORAPOPHYLLITE

FRANKLINFURNACEITE

GANOPHYLLITE

HYDROXYAPOPHYLLITE

KITTATINNYITE

KRAISSLITE

MARGAROSANITE

MCGOVERNITE

MINEHILLITE

PIMELITE

PREHNITE

ROEBLINGITE

SEPIOLITE

TALC

ZINALSITE

CHRYSOCOLLA

(Cu,Al)2H2Si2O5(OH)4.nH2O
Monoclinic

Chrysocolla, a copper silicate hydroxide hydrate mineral, has been known from Franklin and Sterling Hill for a long time. The first mention of it was by Beck (1839), and it may have been the material reported by Seymour (1868) and Darton (1883). Palache (1935) reported it as an unconfirmed species, and Frondel (1972) reported its verification from Franklin. It was reported from both Franklin and Sterling Hill by Cook (1973), and it has been seen by the writer associated with azurite and franklinite from Sterling Hill, but has not been studied. It is a minor mineral locally, blue in color, commonly but not consistently with dull luster, and occurring in hand-sized specimens.  

 

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CHAPTER 18. PHYLLOSILICATES - LAYER SILICATES