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        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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