Zoisite, first known as saualpite, after its type locality, is a calcium aluminum hydroxy sorosilicate belonging to the epidote group of minerals. Its chemical formula is Ca2Al3(SiO4)(Si2O7)O(OH).
via Wikipedia infobox
{{Infobox mineral | name = Zoisite | category = Sorosilicate – epidote group | boxwidth = | boxbgcolor =#efe974 | image = Zoisite-33616.jpg | caption = Yellow zoisite crystal (1.7 × 1 × 0.8 cm) | formula = Ca2Al3(SiO4)(Si2O7)O(OH) | IMAsymbol = Zo | strunz = 9.BG.10 | dana = 58.2.1b.1 | system = Orthorhombic | class = Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) | symmetry = Pnma | color = White, gray, greenish brown, greenish gray, pink, blue, purple | habit = Prismatic crystals with striations; massive to columnar | twinning = | cleavage = Perfect {010} imperfect {100} | fracture = Uneven to conchoidal | mohs = 6 to 7 | luster = Vitreous, pearly on cleavage surfaces | refractive = nα = 1.696 – 1.700 nβ = 1.696 – 1.702 nγ = 1.702 – 1.718 | opticalprop = biaxial positive | birefringence = 0.006–0.018 | pleochroism = X = pale pink to red-violet; Y = nearly colorless to bright pink or deep blue; Z = pale yellow to yellow-green | streak = White or colorless | gravity = 3.10–3.36 | Density = | fusibility = | diagnostic = | solubility = | diaphaneity = Transparent to translucent | other = | references = | var1 = Tanzanite | var1text = Gem-quality zoisite, blue-purple | var2 = Thulite | var2text = Pink }} Zoisite, first known as saualpite, after its type locality, is a calcium aluminum hydroxy sorosilicate belonging to the epidote group of minerals. Its chemical formula is Ca2Al3(SiO4)(Si2O7)O(OH).
Zoisite occurs as prismatic, orthorhombic (2/m 2/m 2/m) crystals or in massive form, being found in metamorphic and pegmatitic rock. Zoisite may be blue to violet, green, brown, pink, yellow, gray, or colorless. Blue crystals are known under the name tanzanite. It has a vitreous luster and a conchoidal to uneven fracture. When euhedral, zoisite crystals are striated parallel to the principal axis (c-axis). Also parallel to the principal axis is one direction of perfect cleavage. The mineral is between 6 and 7 on the Mohs hardness scale, and its specific gravity ranges from 3.10 to 3.38, depending on the variety. It streaks white and is said to be brittle. Clinozoisite is a more common monoclinic polymorph of Ca2Al3(SiO4)(Si2O7)O(OH). Transparent material is fashioned into gemstones while translucent-to-opaque material is usually carved.
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).