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Mineral Encyclopedia · Search
Browse every oxides-class mineral indexed in the encyclopedia.
Browse by Mineral Class
Mineral class · Oxides
Mineral class
紫水晶
SiO₂ (quartz var.)
Amethyst is the violet to purple variety of quartz (SiO₂) colored by trace iron and natural irradiation. The February birthstone, Amethyst is…
锐钛矿
Anatase is one of the three TiO2 polymorphs (alongside rutile and brookite) and is the lowest-temperature, most metastable of the three. It…
板钛矿
Brookite is the orthorhombic, intermediate-temperature TiO2 polymorph (with rutile being the high-T tetragonal form and anatase the low-T tetragonal form). It produces…
玉髓
SiO₂ (cryptocrystalline)
Chalcedony is the cryptocrystalline form of quartz — submicroscopic interlocked quartz fibers producing a tough, waxy-lustered material. Many named varieties are Chalcedony:…
铬铁矿
FeCr₂O₄
Chromite (FeCr₂O₄) is the principal chromium ore mineral and the only economically significant Cr resource. It forms in podiform and stratiform layered…
金绿宝石
BeAl₂O₄
Chrysoberyl (BeAl₂O₄) is the third-hardest natural mineral (Mohs 8.5) after diamond and corundum. Its three gem varieties are iconic: alexandrite (color-change green-to-red,…
黄水晶
SiO₂ (quartz var.)
Citrine is the yellow to orange-brown variety of quartz, colored by Al³⁺ + Fe³⁺ + radiation defects. Most commercial citrine is heat-treated…
刚玉
Al₂O₃
Corundum (Al₂O₃) is the parent species of two of the most prized gem minerals on Earth — ruby (red, chromium-colored) and sapphire…
赤铜矿
Cuprite is the principal copper(I) oxide mineral and one of the richest Cu ores by mass. Its deep ruby-red color and adamantine…
锌铁尖晶石
Franklinite is a zinc-iron-manganese spinel-group oxide essentially restricted to the unique Franklin and Sterling Hill Zn-Fe-Mn deposit in New Jersey. It is…
锌尖晶石
Gahnite is the zinc end-member of the spinel group, a Zn-Al oxide producing dark green to bluish-black sharp octahedral crystals. It is…
针铁矿
FeO(OH)
Goethite (FeO(OH)) is iron hydroxide — the principal iron mineral of laterite, gossan, and bog iron deposits. Named after the German polymath…
赤铁矿
Fe₂O₃
Hematite (Fe₂O₃) is the principal iron ore mineral worldwide and one of the most economically important minerals on Earth. Its blood-red streak…
钛铁矿
FeTiO₃
Ilmenite (FeTiO₃) is the iron-titanium oxide and the principal ore of titanium for paint pigments (TiO₂ "titanium white"). It forms in mafic…
碧玉
SiO₂ + impurities
Jasper is the opaque cryptocrystalline form of quartz — like Chalcedony but with sufficient impurities (iron oxides, clays, organic) to render it…
纤铁矿
Lepidocrocite is the orthorhombic dimorph of FeO(OH), forming alongside or replacing goethite (the more common variety). It produces distinctive ruby-red translucent micaceous…
褐铁矿
FeO(OH)·nH₂O (mixture)
Limonite is not a single mineral species but a field-name for amorphous to cryptocrystalline iron hydroxide aggregates — primarily goethite and lepidocrocite…
磁铁矿
Fe₃O₄
Magnetite (Fe₃O₄) is the strongly magnetic iron oxide and one of the principal iron ores. Its octahedral crystal habit and natural magnetism…
水锰矿
MnO(OH)
Manganite (MnO(OH)) is a manganese oxyhydroxide and one of the historically important manganese ore minerals. It forms striking dark steel-gray to iron-black…
软锰矿
MnO₂
Pyrolusite (MnO₂) is the most common manganese ore mineral and the principal source of industrial manganese for steelmaking and battery production. While…
玫瑰石英
SiO₂ (quartz var.)
Rose Quartz is the pink to rose-red variety of quartz, colored by trace titanium and microscopic dumortierite-like fibrous inclusions. It typically forms…
金红石
TiO₂
Rutile (TiO₂) is the highest-temperature TiO₂ polymorph (with anatase low-T and brookite intermediate). Its name from Latin "rutilus" (red) reflects its diagnostic…
尖晶石
MgAl₂O₄
Spinel (MgAl₂O₄) is the parent species of the spinel oxide group and a cherished gem mineral for centuries. Famous historical "rubies" turned…
红锌矿
Zincite is one of the very few naturally occurring zinc oxide minerals, and natural specimens are essentially restricted to one place on…
锡石
SnO2
SnO2 . Tetragonal . Mohs 6-7