MINERALS INDEX

Actinolite

Albite

Allactite

Allanite

Amphibole Group

Andradite

Anglesite

Anhydrite

Anorthite

Apatite

ApatiteGroup

Apophyllite

Aragonite

Arsenates

Arsenides

Arseniosiderite

Arsenopyrite

Aurichalcite

Axinite

Azurite

Barite

Barylite

Barysilite

Bementite

Biotite

Borates

Bornite

Boroarsenates

Bustamite

Cahnite

Calamine

Calcite

Calcium larsenite

Carbonates

Celestite

Cerusite

Chalcocite

Chalcophanite

Chalcopyrite

Chloanthite

Chlorite

Chlorophoenicite

Chondrodite

Chysolite Group

Clinohedrite

Copper

Corundum

Corundum Group

Crocidolite

Cummingtonite

Cuprite

Cuspidine

Cyprine

Datolite

Desaulesite

Descloizite

Diopside

Dolomite

Edenite

Epidote

EpidoteGroup

FeldsparGroup

Ferroaxinite

Ferroschallerite

Fluoborite

Fluorite

Franklinite

Friedelite

Friedelite Group

Gageite

Gahnite

Galena

Ganophyllite

Garnet

Glaucochroite

Goethite

Graphite

Greenockite

Gypsum

Halloysite

Haloids

Hancockite

Hardystonite

Hastingsite

Hedyphane

Hematite

Hetaerolite

Heulandite

Hodgkinsonite

Holdenite

Humite Group

Hyalophane

Hydrohetaerolite

Hydrozincite

Ilmenite

Jeffersonite

Kentrolite

Larsenite

Lead

Leucaugite

Leucophoenicite

Limonite

Lollingite

Loseyite

Magnesium- chlorophoenicite

Magnetite

Malachite

Manganbrucite

Manganite

Manganosite

Marcasite

Margarosanite

Mcgovernite

Mica Group

Microcline

Millerite

Molybdenite

Mooreite

Muscovite

Nasonite

Native Elements

Neotocite

Niccolite

Norbergite

Oxides

Pargasite

Pectolite

Phlogopite

Phosphates, Arsenates and Vanadates

Prehnite

Psilomelane

Pyrite

Pyrochroite

Pyroxene Group

Pyrrhotite

Quartz

Rhodochrosite

Rhodonite

Roeblingite

Roepperite

Rutile

Scapolite

Schallerite

Schefferite

Serpentine

Serpentine Group

Siderite

Silicates

Silver

Smithsonite

Sphalerite

Spinel

Spinel Group

Stilbite

Sulphates

Sulphides and Arsenides

Sussexite

Svabite

Talc

Tennantite

Tephroite

Thomsonite

Thorite

Titanite

Tourmaline

Tremolite and Actinolite

Unconfirmed Species

Vanadates

Vesuvianite

Willemite

Xonotlite

Zeolites

Zinc schefferite

Zincite

Zircon

Zoisite

 

Chloanthite

NiAs2
Isometric

Forms
a(100), o(111), and e(210).

Habit
Chloanthite is found both crystalline and massive. The crystals are rare, small, and much distorted and are mainly octahedrons with minute modifying faces of the dodecahedron and pyritohedron. The color of the massive mineral is dull steel-gray, but the crystal faces are brilliant silver-white. The specific gravity is 6.833 (Koenig).

Composition
The chemical composition of chloanthite is shown by the following analysis:

Analysis of chloanthite
(G. A. Koenig (137), analyst)

Percent

Molecular ratio

As

70.66

0.943* 0.991
S

1.54

0.048*  
Ni

18.63

0.318†  
Co

6.37

0.108† 0.467
Fe

2.31

0.041†  
Zn

trace

   
CaCO3

0.89

   

100.40

[Figures noted with ‘*’ and ‘†’ are reflected in the values 0.991 and 0.467 shown, respectively]

The molecular ratio of (Ni,Co,Fe) to (As,S)–1:2.12–indicates a chloanthite very low in sulphur, with a ratio of nickel to cobalt, as shown by the analysis, of about 3 to 1.

Occurrence
Chloanthite is known only from the Trotter mine at Franklin, the foregoing description being taken from a paper by Koenig (137). At a depth of 340 feet the Trotter shaft passed through a segregation of nickel ores, comprising chiefly chloanthite and niccolite and their oxidation products, together with calcite, yellow sphalerite, and dark-purple fluorite. The chloanthite was in general intimately intermixed with massive niccolite, and crystals were found only where it was in contact with calcite. In one specimen a felted mass of bluish amphibole needles was cemented by massive chloanthite, crystals of that mineral being implanted on the rounded surface.

Rammelsbergite
In some lists of Franklin minerals–Nason (153), Kemp (152), Dana (146)–the name rammelsbergite appears. There is no good authority in the published literature for the listing of this mineral, and it is doubtless a mistake for chloanthite. (See appendix, b, page 130.)

Smaltite
No mention of smaltite has appeared in any publication on the district, hence its inclusion in the list of Hoadley and Broadwell (235) is probably also to be considered a mistake for chloanthite.

 


 
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