How do I identify Cookeite?

Cookeite can be identified by its hardness of 2.5 - 3.5 on the Mohs scale, White color, Pearly, Greasy, Waxy luster, Monoclinic crystal system. Look for these key characteristics when examining specimens.

What color is Cookeite?

Cookeite typically appears in White, yellowish green, pink, brown. Color can vary depending on impurities and formation conditions.

How hard is Cookeite?

Cookeite has a hardness of 2.5 - 3.5 on the Mohs scale. This makes it a soft mineral that can be scratched easily.

Cookeite

A variety of Chlorite Group

Rare

What is Cookeite?

Cookeite occurs in translucent shades of white, green, pink, and brown, but is colorless in its purest state. This mineral is relatively soft on the Mohrs scale which measures the hardness of minerals. Cookeite was named after Josiah Parsons Cooke Jr., a Harvard chemist and mineralogist.

Uses & Applications

Cookeite is a relatively rare type of chlorite and doesn't have any industrial uses. It is kept for decorative value, on occasion, but usually plays a secondary role to larger, more impressive quartz crystals that form in the same strata. Cookeite can be found in several colors, some of which are more sought-after than others.

Cookeite Market Value Calculator

Estimate the market value of Cookeite using size, quality, and finish. This preview calculator is for quick context and is not a formal appraisal.

Cookeite Localities Map

See where Cookeite is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.

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North ZoneCentral RidgeSouth Basin

Key Characteristics

Formation of Cookeite

Chlorite is commonly found in igneous rocks as an alteration product of mafic minerals such as pyroxene, amphibole, and biotite. In this environment chlorite may be a retrograde metamorphic alteration mineral of existing ferromagnesian minerals, or it may be present as a metasomatism product via addition of Fe, Mg, or other compounds into the rock mass. Chlorite is a common mineral associated with hydrothermal ore deposits and commonly occurs with epidote, sericite, adularia and sulfide minerals. Chlorite is also a common metamorphic mineral, usually indicative of low-grade metamorphism. It is the diagnostic species of the zeolite facies and of lower greenschist facies. It occurs in the quartz, albite, sericite, chlorite, garnet assemblage of pelitic schist. Within ultramafic rocks, metamorphism can also produce predominantly clinochlore chlorite in association with talc. Experiments indicate that chlorite can be stable in peridotite of the Earth's mantle above the ocean lithosphere carried down by subduction, and chlorite may even be present in the mantle volume from which island arc magmas are generated. Chlorite occurs naturally in a variety of locations and forms. For example, chlorite is found naturally in certain parts of Wales in mineral schists. Chlorite is found in large boulders scattered on the ground surface on Ring Mountain in Marin County, California.

Composition of Cookeite

The typical general formula is: (Mg,Fe)3(Si,Al)4O10(OH)2·(Mg,Fe)3(OH)6. This formula emphasizes the structure of the group. Chlorites have a 2:1 sandwich structure (2:1 sandwich layer = tetrahedral-octahedral-tetrahedral = t-o-t...), this is often referred to as a talc layer. Unlike other 2:1 clay minerals, a chlorite's interlayer space (the space between each 2:1 sandwich filled by a cation) is composed of (Mg, Fe)(OH)6. This (Mg, Fe)(OH)6 unit is more commonly referred to as the brucite-like layer, due to its closer resemblance to the mineral brucite (Mg(OH)2). Therefore, chlorite's structure appears as follows: -t-o-t-brucite-t-o-t-brucite ... That's why they are also called 2:1:1 minerals. An older classification divided the chlorites into two subgroups: the orthochlorites and leptochlorites. The terms are seldom used and the ortho prefix is somewhat misleading as the chlorite crystal system is monoclinic and not orthorhombic.