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The Mineral greenockite

Red-Orange Greenockite Microcrystals

Greenockite is a rare mineral formed mostly of the element cadmium, and it is the only cadmium mineral of importance. Its occurrence is almost always in association with Sphalerite, due to a similar paragenesis, and it often forms as thin coatings on other minerals, especially Smithsonite and Calcite. Greenockite forms in unique crystals that are asymmetrical, with the basal crystal faces forming at wider angles than the top faces.

Greenockite was named in honor of Earl Charles Murray Cathcart, also known as Lord Greenock, a British army general who subsequently became the Governor General of the Province of Canada. Lord Greenock announced the discovery of Greenockite as a new mineral from the excavation of the Bishopton tunnel, near Port Glasgow in Scotland.

Chemical Formula

CdS

Color

Yellow, orange, brown, red

Crystal System

Hexagonal

Properties

Streak
Yellow

Hardness
3 - 3.5

Transparency
Translucent to opaque

Specific Gravity
4.9 - 5.0

Luster
Adamantine to resinous

Cleavage
1,1;3,2

Fracture
Uneven

Tenacity
Brittle

Other ID Marks
May fluoresce yellow.

Crystal Habits

Crystals, which are always small, form in hemimorphic hexagonal crystals, often tapered on one end. Crystals are usually horizontally striated. Most commonly encrusting, as a globular lining in cavities, drusy, or as a dusting on matrix.

3D Crystal Atlas

Additional Information

Composition
Cadmium sulfide

In Group
Sulfides; Simple Sulfides

Striking Features
Crystals and formation habits, and mode of occurrence

Environment
In basalt traprock and hydrothermal ore veins.

Rock Type
Igneous, Sedimentary, Metamorphic

Other Names

Cadmium Ochre

Varieties

Xanthochroite

- Variant of the mineral Greenockite with an with an amorphous crystal structure and earthy habit.

Uses

Greenockite is the only ore mineral of the element cadmium. Due to the rarity of Greenockite, most cadmium is actually produced as a by-product of lead and zinc ores, especially Sphalerite. Greenockite was once used as a yellow pigment and known as cadmium ochre. Elemental cadmium has many uses, including electronics and batteries (nickel-cadmium), electroplating, and forming of high temperature alloys.

Greenockite is considered a rare collector's mineral, and is much sought after by mineral collectors when in crystallized specimens.

Noteworthy Localities

Some of the best Greenockite crystals, often on matrix, have come from the Andesite quarry in Kreimbach-Kaulbach, Rhineland-Palatinate, Germany. Drusy brownish crystals have come from the Kateřina Coal Mine, Radvanice, near Trutnov (Trautenau), Bohemia, Czech Republic; and yellow encrustations from the Paglio Pignolino Mine, Dossena, Bergamo Province, Italy. Small crystals of excellent form were found at the type locality of the Bishopton Tunnel, Strathclyde, Scotland. In Boliva, microcrystal crustings with a bright red color are found in Llallagua, Potosí Department.

In the U.S., yellow Greenockite coatings and crusts are well known from Joplin, Jasper Co., Missouri and the surrounding area in the Tri-State District. Greenockite microcrystals over Smithsonite have been found at Rush, Marion Co., Arkansas; and bright yellow coatings once occurred at Friedensville, Upper Saucon Township, Lehigh Co., Pennsylvania. Perhaps the best U.S. locality in the U.S. for visible crystals is the Summit Quarry, near Springfield, Union Co., New Jersey, where small crystals were found in a limited find in the 1960's. Yellow Greenockite crusts were found in a one-time construction project at the Route 25 Road cut, Trumbull, Fairfield County, Connecticut.