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 halides

ATACAMITE

FLUORITE


The carbonates


The calcite group

CALCITE

OTAVITE

RHODOCHROSITE

SIDERITE

SMITHSONITE


The dolomite group

DOLOMITE

KUTNAHORITE


Other carbonates

ARAGONITE

AURICHALCITE

AZURITE

CANAVESITE

CERUSSITE 

DYPINGITE

HYDROTALCITE

HYDROZINCITE

LOSEYITE

MALACHITE

MONOHYDROCALCITE

PYROAURITE

ROSASITE

SCLARITE

SJÖGRENITE

STRONTIANITE

ZNUCALITE

AURICHALCITE

(Zn,Cu)5(CO3)2(OH)6
Orthorhombic

Aurichalcite, a zinc copper carbonate hydroxide mineral, was reported from Franklin and Sterling Hill by Palache (1935), but is largely unstudied. It is less common than azurite or malachite, although hand-sized specimens have been preserved. No data have been published. Aurichalcite occurs as tufts and clusters of very light blue, acicular crystals, commonly on a severely altered goethite-bearing matrix at both deposits.

The occurrences are probably the same as for azurite and malachite, but may represent a later stage of oxidation. Jenkins (1992) reported an occurrence of aurichalcite associated with orthoserpierite in the Sterling Mine, and Jenkins and Misiur (1994) reported an occurrence with oxidized sulfides.

 

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CHAPTER 23. HALIDES AND CARBONATES