The Mineral Identification Key |
Table IC: Metallic or Submetallic Luster and Hardness greater than 5½: (Can not be scratched by a knife.) [Previous Table] [Next Table]
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
4 to 5½ | Black or Dark greenish or Yellowish-brown |
Pale yellowish or Brownish | BETAFITE (Ca,Na,U)2(Ti,Nb)O6(OH) |
Isometric | Massive (metamict) | Approx. 4 to 6 (variable) | Luster usually sub-metallic, but may be resinous to vitreous, highly radioactive | |
5 to 5½ | Pale Copper-red to Pinkish Silvery-white, tarnishing to Dark-grey or Black | Black | NICKELINE NiAs |
Hexagonal | Usually massive, crystals rare and usually pyramidal, often malformed, may also be reticulated or arborescent | 7.78 | May be coated with green "nickel bloom" (annabergite) | |
5 to 5½ | Dark-brown to Black, color black in ferberite, brown in hübnerite |
Dark-brown to Black | One perfect direction | FERBERITE/ HÜBNERITE ("Wolframite" series) (Fe,Mn)WO4 (Mn,Fe)WO4 |
Monoclinic | Usually massive, granular, crystals tabular to bladed with vertical striations | 7.0 to 7.5 above about 7.3 indicates ferberite, lower indicates hübnerite |
Streak darkens with increasing Fe content |
5 to 5½ | Dark-brown to Black | Yellow-brown or Yellow-ocher | One perfect direction | GOETHITE (pronounced "Ger-ta-ite.") FeO(OH) |
Orthorhombic | Usually in radiating botryoidal aggregates, mammillary, or stalactic | 4.37 | |
5 to 5½ | Dark-brown to Black, Dark yellowish-brown to Greenish-brown, Dark reddish-brown | Pale yellowish or Brownish | MICROLITE (Na,Ca)2Ta2O6(O,OH,F) |
Isometric | Usually massive, granular, crystals octahedral |
5.90-6.42 | Luster usually resinous to vitreous, but when resinous may appear sub-metallic, may contain some U and be radioactive | |
5 to 5½ | Brown to Black or Dark yellowish-brown | Light-brown to Yellowish-brown | PYROCHLORE |
Isometric | Usually massive, granular, crystals usually octahedral, modified by the cube | 4.45-4.90 | Luster usually resinous to vitreous, but when resinous may appear sub-metallic, usually contains some U and is radioactive Distinguished from microlite by its lower S.G. | |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
5 to 6 | Black | Black to Dark-brown | ROMANECHITE ( |
Orthorhombic | Usually massive, botryoidal or stalactic | 3.7 to 4.7 | Distinguished from similar Mn minerals by its greater hardness | |
5 to 6 | Black to Silvery-black | Black to Dark-brown | ILMENITE FeTiO3 |
Trigonal | Usually as platy massive or granular, crystals rare, thick tabular or acute rhombohedral | 4.72 | May be weakly magnetic | |
5 to 6 | Deep blood-red | Black to Dark-brown or Reddish-brown | Perfect in two directions | PYROPHANITE MnTiO3 |
Trigonal | Usually in fine-grained, scaly, masses | 4.54 | |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
5½ | Tin-white or Silvery-white | Black | One perfect direction | COBALTITE/ GERSDORFFITE (Co,Ni)AsS (Ni,Co)AsS |
Isometric | Usually massive, granular, cubic and pyritohedral crystals (cobaltite) or octahedral and pyritohedral crystals (gersdorffite) | 6.3 (cobaltite), 5.9 (gersdorffite) |
Difficult to distinguish end members without chemical tests, S.G. may help for samples close to the ideal end members. |
5½ | Tin-white or Silvery-white | Black | Two distinct directions, poor in one direction | SKUTTERUDITE/ NICKEL-SKUTTERUDITE (Co,Ni)As2-3 (Ni,Co,)As2-3 |
Isometric | Usually massive, crystals cubes or cubo-octahedral | 6.5 to 6.9 (skutterudite nickel-skutterudite) |
High end S.G. indicates the skutterudite end member, otherwise difficult to distinguish from one another. |
5½ | Black | Black to Dark-brown | URANINITE UO2 |
Isometric | Usually massive | 9.0 to 9.7 | ("Pitchblende"), luster actually "pitchy", may be botryoidal, radioactive | |
5½ | Brownish-black | Dark-brown | CHROMITE FeCr2O4 |
Isometric | Usually massive, granular | 4.6 | Luster actually "pitchy", often with green alteration products | |
5½ | Pale copper-red | Red-brown | BREITHAUPTITE NiSb |
Hexagonal | Usually massive, crystals rare, tabular | 7.59 to 8.23 | Rare | |
5½ to 6 | Tin-white or Silvery-white, tarnishing Brown or Bronzish | Black | One distinct direction | ARSENOPYRITE FeAsS |
Monoclinic | Usually massive, granular, crystals pseudo-orthorhombic prismatic, usually in cruciform twins or star-shaped trillings | 6.0 to 6.2 | Has garlic odor when ground or pounded poisonous arsenic fumes |
5½ to 6 | Brown, Yellowish-brown, Reddish-brown; Dark-brown to Iron-black; | White to Grayish-white or Yellowish-white | One indistinct direction | BROOKITE TiO2 |
Orthorhombic | Usually tabular, elongated and striated crystals, commonly pyramidal or pseudohexagonal | 4.08 to 4.18 | Found in alpine veins in gneiss and schist. Also found in contact metamorphic and hydrothermal veins |
5½ to 6 | Brown, Yellowish-brown, Reddish-brown, Indigo, Black; Geenish, Pale lilac, Gray, rarely Colorless | White to Pale yellow | Two perfect directions | ANATASE TiO2 |
Tetragonal | Usually pyramidal or tabular | 3.79 to 3.97 | Found in alpine veins in gneiss and schist as a secondary mineral. |
5½ to 6 | Dark-brown to Steel-grey to Black | Rust-red or Indian-red | HEMATITE Fe2O3 |
Trigonal | Usually massive in radiating, reniform, or micaceous aggregates, crystals rhombohedral | 4.8 to 5.3 | Usually black and usually harder than a knife. (See under Sections IA & IB.) | |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
6 | Black | Black | MAGNETITE Fe3O4 |
Isometric | Massive or in octahedral crystals | 5.18 | Strongly magnetic | |
6 | Black | Black to Dark-brown | One distinct direction | COLUMBITE/ TANTALITE (Fe,Mn)(Nb,Ta)2O6 |
Orthorhombic | Usually massive platy, or as thick tabular crystals | 5.2 to 6.76 (ferrocolumbite) 7.95 (ferrotantalite) |
A complex solid solution series exists within the Columbite-Group; distinguishing between species is difficult without subtle chemical tests. S.G. may be indicative for some species but not definitive. Columbite/tantalite series is now broken down into the four end-member minerals - ferrocolumbite, manganocolumbite, ferrotantalite and manganotantalite |
6 | Brownish-black | Dark-brown | FRANKLINITE (Fe,Zn,Mn)(Fe,Mn)2O4 |
Isometric | Usually massive, granular, or as octahedral crystals | 5.15 | May be slightly magnetic. Rare outside of Franklin, N.J., USA | |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
6 to 6½ | Brass-yellow | Black (may be greenish-black) | PYRITE FeS2 |
Isometric | Massive or in striated cubic, pyritohedral, or octahedral crystals, may be twinned | 5.0 | Most common brass-yellow metallic mineral | |
6 to 6½ | Brass-yellow | Black (may be greenish-black) | One distinct direction | MARCASITE FeS2 |
Orthorhombic | Usually massive, granular, crystals usually "cockscomb" clusters or radiating fibrous aggregates | 4.9 | Difficult to distinguish from pyrite without tests unless good crystals are present. |
6 to 6½ | Dark-brown to Black | Pale-brown | One distinct direction | RUTILE TiO2 |
Tetragonal | Usually in prismatic crystals, vertically striated, often needle-like as inclusions in silicate crystals, particularly quartz | 4.2 to 4.25 | Anatase and brookite are closely related species, but rarer. |
Note: The Betafite-Microlite-Pyrochlore Group and Subgroups are complex, species can be difficult to tell apart. S.G. and radioactivity may be indicative for some species, but are rarely definitive.
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