Woodallite

woodallite

lizardite

iowaite

tochilinite

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Formula: Mg6Cr2(OH)16Cl2.4H2O
Hydroxide, hydrotalcite group, hydrotalcite supergroup, chromium-bearing mineral
Crystal System: Trigonal
Specific gravity: 2.062 measured, 2.023 g/cm3 (Calculated)calculated
Hardness: 1&~189; to 2
Streak: Pale pink to white
Colour: Purple to deep magenta
Environments

Hydrothermal environments

Localities

At the type locality, the Mount Keith Open Pit, Mount Keith, Wiluna Shire, Western Australia, woodallite is a new (in 2020) chromium-rich member of the hydrotalcite group from the large, low-grade Mount Keith nickel deposit. Woodallite occurs as whorls and clusters of minute platelets up to 6 mm across in lizardite + brucite altered dunite. Individual platelets are typically 10–100 μm in maximum dimension and are often curved. Associated minerals include chromite, lizardite, iowaite, pentlandite, magnetite, tochilinite and brucite.
Woodallite forms as a result of hydrothermal alteration of primary magmatic chromite by chlorine-rich solutions at temperatures less than 320°C. Relict chromite fragments are frequently present in the whorls, and associated magnetite is altered extensively to iowaite (MM 65.427-436).

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