Devilline is a sulfate mineral with the chemical formula CaCu4(SO4)2(OH)6·3H2O. The name originates from the French chemist's name, Henri Etienne Sainte-Claire Deville (1818–1881).
via Wikipedia infobox
{{Infobox mineral | name = Devilline | category = Sulfate minerals | image = Devilline-t08-23b.jpg | caption = Devilline | formula = CaCu4(SO4)2(OH)6·3(H2O) | IMAsymbol = Dev | molweight = | strunz = 7.DD.30 | system = Monoclinic | class = Prismatic (2/m) (same H-M symbol) | symmetry = P21/c | unit cell = a = 20.870, b = 6.135 c = 22.91 [Å], β = 102.73° V = 2,861.23 Å3 | color = Green, blueish green; green in transmitted light | habit = Prismatic, lamellar, platy pseudohexagonal crystals | twinning = On {010} | cleavage = Perfect (001) distinct (110) and (101) | fracture = | tenacity = Brittle | mohs = 2.5 | luster = Vitreous, pearly | refractive = nα=1.585, nβ=1.649, nγ=1.660 | opticalprop = biaxial negative | 2V = 42° | birefringence = δ=0.075 | pleochroism = Visible | streak = Light green | gravity = | density = Measured: 3.13 g/cm3 Calculated: 3.084 g/cm3 | melt = | fusibility = | diagnostic = | solubility = Insoluble in water and concentrated H2SO4. Completely soluble in HNO3. | diaphaneity = | other = | references = }} Devilline is a sulfate mineral with the chemical formula CaCu4(SO4)2(OH)6·3H2O. The name originates from the French chemist's name, Henri Etienne Sainte-Claire Deville (1818–1881).
Devilline crystallizes in the monoclinic system. Crystallographically, it contains three vectors of unequal lengths and two pairs of vectors are perpendicular while the other pair makes an angle other than 90°. Devilline is prismatic and belongs to the crystal class 2/m. This mineral belongs to the space group P 21/c. Devilline is an anisotropic mineral, meaning that the mineral has different properties in different directions. Optically, this mineral is biaxial negative, meaning that it contains two optic axes. Devilline has a moderate mineral relief. Mineral relief refers to the way a mineral appears to stand out when viewed under polarized light and it is dependent on the mineral's index of refraction.
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).