Rock Identifier
Lepidolite (K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2) — metamorphic
metamorphic

Lepidolite

K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2

Hardness: 2.5–3 on Mohs scale; Color: Purple, violet, or pink; Luster: Pearly to vitreous; Crystal Structure: Monoclinic; Cleavage: Perfect basal cleavage; Specific Gravity: 2.8–3.0

Hardness
2
Color
Purple, violet, or pink
Luster
Pearly to vitreous
Identified More metamorphic
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Physical properties

Hardness: 2.5–3 on Mohs scale; Color: Purple, violet, or pink; Luster: Pearly to vitreous; Crystal Structure: Monoclinic; Cleavage: Perfect basal cleavage; Specific Gravity: 2.8–3.0

Formation & geological history

Formed in granitic pegmatites through hydrothermal processes. It is often found associated with other lithium-bearing minerals like spodumene and tourmaline. It typically dates from the Precambrian to Cenozoic eras depending on the specific deposit.

Uses & applications

Major source of lithium for batteries and glass/ceramic production; used as a decorative stone, in jewelry (cabochons), and highly valued by mineral collectors for its metaphysical associations.

Geological facts

Lepidolite was originally named 'lilalite' because of its lavender color. It is one of the primary sources of the rare alkali metals rubidium and cesium. It is often called the 'Peace Stone' in metaphysical circles.

Field identification & locations

Identify by its distinctive lilac/purple color and micaceous (flaky) structure. It is commonly found in Brazil, Canada (Manitoba), Madagascar, and the United States (California and Maine). Collectors should look for its pearly sheen and ease of scratching with a copper penny.