Garnierite

Rock made of serpentine, talc, chlorite

Uncommon · (Ni,Mg)₃Si₂O₅(OH)₄ to (Ni,Mg)₃Si₄O₁₀(OH)₂ (variable)

Not a valid mineral name but a field name for the green nickel ore that fills veins and pockets in weathered, serpentinised ultramafic rocks: an intimate mixture of nickel-bearing serpentine, talc, sepiolite, smectite or chlorite, the green darkening with the nickel. An important nickel ore of laterite deposits, named in 1874 for Jules Garnier, who had announced nickel in New Caledonia in 1867.

Rock

Kind of rock
Chemical sedimentary rock
Rock family
Ultramafic rock (peridotite, serpentinite)
Deposits
Lateritic deposit
Metals
Nickel
How it forms
Nickel leached from weathering serpentinised ultramafic rock gathers in veins and pockets of the laterite.
Uses
Ore of nickel, mined in New Caledonia from the end of the nineteenth century.

Identity

Formula
(Ni,Mg)₃Si₂O₅(OH)₄ to (Ni,Mg)₃Si₄O₁₀(OH)₂ (variable)
Chemical class
Silicate
Ore of
Nickel

Crystallography

Crystal system
Amorphous
Habits
Massive, Earthy, Botryoidal
Fracture
Uneven

Physical properties

Mohs hardness
2.5
Density
2.7 g/cm³
Luster
Earthy, Waxy, Dull
Colors
green, yellow-green, dark green, emerald green
Transparency
Opaque, Translucent

Geology

Origins
Sedimentary
Host rocks
Ultramafic rock (peridotite, serpentinite)
Associated minerals
Serpentine, Talc, Chlorite, Goethite, Quartz
Geography
New Caledonia, Dominican Republic (Falcondo), USA (Riddle, Oregon), Russia (Ural Mountains)

Classification

Rarity
Uncommon
Gem quality
No

Sources

Browse the Crystal Encyclopedia — MGS Toolbox