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

AZURITE

Cu3(CO3)2(OH)2 
Monoclinic

 
 
 
  Figure 23-15. Crystal drawings of azurite from Franklin. These are two projections (A and B) of one crystal. Drawings are from Palache (1935) who provided crystallographic data.  
   

Azurite, a copper carbonate hydroxide mineral, was first described from Franklin by Vanuxem and Keating (1822b) as “blue carbonate of copper” and later was described by Palache (1928a, 1935). It is also found at Sterling Hill.

Description

Azurite occurs as very fine, albeit small (1-3 mm) crystals, which were measured, described, and extensively illustrated by Palache (1928a, 1935). The abundant crystal drawings should not be taken as an indication of abundant azurite; it was uncommon locally. Azurite is deep blue, although light-blue films have been verified from Sterling Hill. No physical, optical, or chemical data exist for local specimens. 

Occurrence and paragenesis

Azurite was found associated with malachite, goethite, aurichalcite, and rarely rosasite or hemimorphite at the north end of Mine Hill in Franklin. The matrix for many specimens is severely altered; in general, only goethite remains as a visible matrix mineral. For other specimen matrixes, magnetite persists with calcite; this assemblage may have been derived from parent chalcocite-magnetite intergrowths. Palache (1928a, 1935) noted that his specimens came from the 200 level at Franklin.

   
 
 
  Figure 23-16. Crystal drawing of azurite from Franklin. Drawing is from Palache (1935) who provided crystallographic data.   Figure 23-17. Crystal drawings of azurite from Sterling Hill; these are two projections (A and B) of one crystal. Drawings are from Palache (1935) who provided crystallographic data.  
       

Similar specimens are known from Sterling Hill, commonly in veins. Some specimens seem to have formed from the alteration of chalcocite, bornite, or chalcopyrite. The associated minerals are the same as at Franklin, with the addition of sparse serpentine.

   
 
 
  Figure  23-18. Crystal drawings of azurite from Sterling Hill. These are two projections (A and B) of one crystal. Drawings are from Palache (1935) who provided crystallographic data.      
       

 

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Copyright © 1995 by Pete J. Dunn
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This page created: January 13, 2001

 

CHAPTER 23. HALIDES AND CARBONATES