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 apatite group

FLUORAPATITE

HEDYPHANE

JOHNBAUMITE

MIMETITE

TURNEAUREITE


Other arsenates, arsenites, phosphates, and vanadates

ADAMITE

ADELITE

AKROCHORDITE

ALLACTITE

ANNABERGITE

ARSENIOSIDERITE

AUSTINITE

BARIUM-
PHARMACOSIDERITE

BRANDTITE

CAHNITE

CHLOROPHOENICITE

CLINOCLASE

CONICHALCITE

DESCLOIZITE

DUFTITE

ERYTHRITE

EUCHROITE

EVEITE

FLINKITE

FLUCKITE

GUERINITE

HAIDINGERITE

JAROSEWICHITE

KOETTIGITE

LEGRANDITE

LIROCONITE

MAGNESIUM-
CHLOROPHOENICITE

MAGNUSSONITE

MANGANBERZELIITE

MANGANESE-
HOERNESITE

META-ANKOLEITE

METALODEVITE

METAZEUNERITE

NEWBERYITE

NIAHITE

OGDENSBURGITE

OJUELAITE

PARABRANDTITE

PARASYMPLESITE

PHARMACOLITE

PHARMACOSIDERITE

PICROPHARMACOLITE

PYROBELONITE

RETZIAN-(La)

RETZIAN-(Nd)

SARKINITE

SCORODITE

STERLINGHILLITE

SYNADELPHITE

TILASITE

URANOSPINITE

VILLYAELLENITE

WALLKILLDELLITE

WENDWILSONITE

YUKONITE

 

VILLYAELLENITE

Mn5(AsO3OH)2(AsO4)2.4H2O                           Monoclinic

Villyaellenite, a manganese arsenate hydrate mineral, was verified by the writer from Sterling Hill and published by Kampf and Ross (1988). Villyaellenite occurs as flattened, 7 mm wide, radial sprays of light pink crystals with vitreous luster. There is no response to ultraviolet. No other physical or optical data exist. A microprobe analysis is given in Table 25, showing minimal Mn/Ca solid solution. X-ray methods are suggested for verification.

Villyaellenite is known on but one specimen from the 340 level. It occurs with manganoan calcite in a vein in willemite/franklinite  ore. The 340 level is one which contributed mostly Fe and Zn arsenates, so this occurrence is anomalous.

 

FOOTER LBI

 
Copyright © 1995 by Pete J. Dunn
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CHAPTER 25. ARSENATES, ARSENITES, PHOSPHATES, AND VANADATES