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Cookeite (pronounced Cook-ite) is an uncommon member of the Chlorite group, and is best known for its occurrence in granite pegmatites associated with Tourmaline, where it often forms as a growth layer upon the Tourmaline. Cookeite is named in honor of Josiah Parsons Cooke Jr. (1827-1894), a Harvard University scientist who was instrumental in the measurement of atomic weights.
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Chemical Formula |
LiAl5Si3O10(OH)8 |
Composition |
Basic lithium magnesium aluminum silicate |
Color |
White, beige, yellow, orange, green, light blue, light brown, light pink |
Streak |
white |
Hardness |
2.5 |
Crystal System |
Monoclinic |
Crystal Forms and Aggregates |
Crystals, which are always small, are in tabular pseudohexagonal form. Most often in radiating and botryoidal aggregates, as ball-shaped spheres, and in micaceous crusts, flakes, and small rosettes.
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Transparency |
Translucent |
Specific Gravity |
2.58 - 2.69 |
Luster |
Pearly, waxy |
Cleavage |
1,1 |
Fracture |
Uneven |
Tenacity |
Flexible but not elastic. |
Other ID Marks |
May have a slightly greasy feel. |
In Group |
Silicates; Phyllosilicates; Chlorite Group |
Striking Features |
Crystal habits, localities, and mineral associations |
Environment |
As an alteration mineral in lithium-rich granite pegmatites.
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Rock Type |
Igneous |
Popularity (1-4)
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3 |
Prevalence (1-3)
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3 |
Demand (1-3) |
2 |
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Cookeite is best known from the pegmatite quarries in Oxford Co., Maine. Specific localities there include Mt. Rubellite, Hebron; Mt Mica, Paris; Plumbago Mountain, Newry; the Tamminen Quarry, Greenwood; and the Bennett Quarry, Buckfield. Cookeite also comes from the Gillette Quarry, Haddam; and at the Strickland Quarry, Portland; both in Middlesex Co., Connecticut.
Some of the best bluish and greenish Cookeite, in interesting ball aggregates with Quartz, comes from Saline Co., Arkansas, especially at the
Stand-on-Your-Head mine in Bland. Good Cookeite also comes from the Tourmaline mines around Pala, San Diego Co., California; as well as the Tourmaline mines of of Minas Gerais, Brazil, especially at Conselheiro Pena in the Doce valley.
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Muscovite and other micas - Are more elastic. Talc - Softer (1).
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