Also known as MoO3
Molybdite is the naturally occurring mineral form of molybdenum trioxide MoO3. It occurs as yellow to greenish needles and crystallizes in the orthorhombic crystal system.
{{infobox mineral | name = Molybdite | image = Molybdite-Molybdenite-233200.jpg | imagesize = 260px | alt = | caption = Molybdite on molybdenite from the Questa Molybdenum Mine (size: 11.0 x 6.7 x 4.1 cm) | category = | formula = MoO3 | IMAsymbol = Myb | strunz = 4.EA.10 | dana = | system = Orthorhombic | class = Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) | symmetry = Pbnm | unit cell = a = 3.96 Å, b = 13.85 Å, c = 3.69 Å; Z = 4 | color = Light greenish yellow to nearly colorless | habit = Flattened needles or thin plates may occur in aggregates | twinning = | cleavage = Perfect on {100}, district on {001} | fracture = | tenacity = Flexible | mohs = 3 - 4 | luster = Adamantine | streak = White | diaphaneity = Transparent | gravity = 4.72 | density = | polish = | opticalprop = Biaxial (+) | refractive = | birefringence = High | pleochroism = | 2V = Large | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = | prop1 = | prop1text = | references = }} Molybdite is the naturally occurring mineral form of molybdenum trioxide MoO3. It occurs as yellow to greenish needles and crystallizes in the orthorhombic crystal system.
== Discovery and occurrence == Molybdite was first described in 1854 for and occurrence in quartz veins in the Knöttel area of Krupka, Ore Mountains, Bohemia (today in the Ústí nad Labem Region of the Czech Republic. It occurs in vein cavities and as coatings in molybdenite ore veins and quartz topaz greisens. Associated minerals include molybdenite, betpakdalite and quartz. The similar mineral ferrimolybdite is often misidentified as molybdite.
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Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).