The Mineral Identification Key |
Table IB: Minerals with Metallic or Submetallic Luster & Hardness greater than 2½, but less than 5½: (Will not easily mark paper, but can be scratched with a pocket knife.) [Previous Table] [Next Table]
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
1 to 2 | Iron-black | Black | One perfect direction | PYROLUSITE MnO2 |
Tetragonal | May be splintery or in radiating fibrous masses | 4.7 | Will sometimes mark paper. |
1½ to 2 | Silvery-white | Grey | SYLVANITE (Au,Ag)Te2 |
Monoclinic | Usually granular or in bladed aggregates, often appears as skeletal forms on rocks, resembling writing (cuneiform) | 8 to 8.2 |
May mark paper. Rare | |
1½ to 2 | Metallic-blue, tarnishes to blue-black | Black | One perfect direction (basal) | COVELLITE CuS |
Trigonal | Platy masses or thin six-sided platy crystals | 4.6 | May be somewhat iridescent, turns metallic-purple when wet. Will sometimes mark paper. |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
2 | Bluish-black to Silvery-black | Grey-black | One perfect direction (prismatic), two imperfect | STIBNITE Sb2S3 |
Orthorhombic | Usually as thick bladed crystals with striations both parallel to and across the long axis; crystals often bent or "kinked" | 4.5 | Fuses in a candle flame. Will sometimes mark paper. |
2 to 2½ | Deep Ruby-red to Bright Ruby-red | Brownish-red to Scarlet or Vermilion | One distinct direction | PYRARGYRITE/
PROUSTITE Ag3(Sb,As)S3 Ag3(As,Sb)S3 |
Trigonal | Prismatic, pyramidal, rhombohedral, and scalenohedral crystals , also massive, usually as complex intergrown crystal aggregates | 5.58 (pyrargyrite), 5.57 (proustite) | Isostructural species difficult to distinguish, though pyrargyrite is usually darker in color and more common than proustite, fusible in a candle flame. Rare. |
2 to 2½ | Grey-black to Lead-grey | Black | ACANTHITE Ag2S |
Isometric | Pseudo-cubic, usually massive | 7.3 | Bright steel-grey on fresh surfaces but darkens upon exposure, easily cut with a knife (sectile). Will usually mark paper. | |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
2½ | Bluish-black to Lead-grey | Grey-Black to Black | Perfect in three directions at 90o to each other | GALENA PbS |
Isometric | Usually in cubic crystals or masses exhibiting cubic cleavage, also in granular masses | 7.6 | Will usually mark paper. Most common heavy mineral. |
2½ | Brass-yellow to Silvery-white | Yellowish to Greenish-grey | CALAVERITE AuTe2 |
Monoclinic | Usually granular, rarely in distinct elongated crystals | 9.35 | Very heavy, easily fusible in a candle flame (leaving globules of gold). May mark paper. Rare. | |
2 to 3 | Grey-black | Black | One good direction | JAMESONITE Pb4FeSb6S14 |
Monoclinic | Dense clusters or carpets of fibrous to acicular crystals; very delicate! | 5.5 to 6.0 | Fuses easily in a candle flame. |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
2½ to 3 | Grey-black | Grey to Black | BOURNONITE PbCuSbS3 |
Orthorhombic | Usually in stout prismatic crystals often as intergrown clusters with twinning exhibited by re-entrant angles | 5.8 to 5.9 | Fuses easily in a candle flame | |
2½ to 3 | Steel-grey, may tarnish to black on exposure | Grey to Black | CHALCOCITE Cu2S |
Monoclinic, pseudo- orthorhombic |
Usually in compact masses, crystals tabular to stoutly prismatic, often with a pseudo-hexagonal outline, vertically striated. | 5.7 | ||
2½ to 3 | Dark metallic Blue to Black | Black | DIGENITE Cu9S5 |
Isometric | Usually massive as small to tiny irregular grains, very rarely as octahedral crystals | 5.5 to 5.7 | Very similar to chalcocite, but much rarer in non-microscopic sizes. | |
2½ to 3 | Steel-grey, tarnishes metallic blue | Dark steel-grey | STROMEYERITE AgCuS |
Orthorhombic, pseudo- hexagonal |
Usually massive, granular, rarely as pseudo-hexagonal prismatic crystals | 6.2 to 6.3 | Rare. | |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
2½ to 3 | Lead-grey | Brown to brownish-grey | One distinct direction | BOULANGERITE Pb5Sb4S11 |
Monoclinic | Usually massive as fibrous bundles, crystals usually needle-like mats, prismatic crystals rarer | 6.0 to 6.3 | Thin acicular crystals flexible. Rare. |
2½ to 3 | Dark-red to Vermilion | Dark-red | One perfect direction | CINNABAR HgS |
Trigonal | Usually massive, crystals uncommon and usually rhombohedral, often as penetration twins | 8.10 | Luster actually adamantine, appearing metallic, heavy. |
2½ to 3 | Copper-red on fresh surfaces, tarnishes to brown or black | Coppery-red, shiny | COPPER Cu |
Isometric | Usually in irregular masses, large grains, wires, and crude dendritic crystals, crystals usually octahedral and malformed, may be cubic or other Isometric forms | 8.9 | Malleable. | |
2½ to 3 | Golden-yellow, shiny, becoming paler with increased Ag content - electrum variety | Golden-yellow, shiny | GOLD Au |
Isometric | Usually massive in irregular grains, nuggets, "leaves" and "flakes", crystals often wires crudely dendritic or as malformed octahedrons | 15.0 to 19.3 | Malleable, very heavy! Rare. Distinguished from pyrite – "fools gold" – by its malleability, softness and weight. | |
2½ to 3 | Silvery-white, tarnishes black |
Silvery-white, shiny | SILVER Ag |
Isometric | Usually massive as irregular grains, wires, and dendritic crystals | 10.5 | Malleable, heavy. Rare. May mark paper. | |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
3 | Grey-black | Black | One perfect (prismatic), two distinct, and one indistinct direction | ENARGITE Cu3AsS4 |
Orthorhombic | Usually in bladed masses | 4.4 | Crystals vertically striated |
3 | Brownish-bronze on fresh surfaces, tarnishing to metallic purple, iridescent ("peacock ore") | Grey-black | BORNITE Cu5FeS4 |
Orthorhombic, pseudo- tetrahedral |
Crystals usually pseudo-cubic, usually massive | 5.1 | Thin splinters fusible in a candle flame, giving a brittle magnetic globule. | |
3 to 3½ | Brass-yellow | Black, sometimes with a greenish tinge | MILLERITE NiS |
Trigonal | Usually in radiating groups or mats of needle-like to hair-like crystals | 5.5 | Slender crystals usually have a greenish tinge | |
3 to 3½ | Steel-grey | Steel-grey | One indistinct direction | ZINKENITE Pb9Sb22S42 |
Hexagonal | Usually massive, also in columnar and radiating fibrous aggregates of needle-like crystals | 5.2 to 5.3 | Rare |
3 to 3½ | Tin-white | Silvery-grey, shiny | One perfect, one distinct, and one imperfect direction | ANTIMONY Sb |
Trigonal | Usually massive, foliated, or granular, rarely as pseudo-cubic or thick tabular crystals | 6.6 to 6.7 | Very brittle. Rare |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
3 to 4½ | Steel-grey, may tarnish dead black upon exposure | Black (may be Brownish-black) | TETRAHEDRITE/ TENNANTITE (Cu,Fe)12Sb4S13 (Cu,Fe)12As4S13 |
Isometric | Usually massive or granular, crystals uncommon and usually pseudo-tetrahedral | 4.6 to 5.1 | End members difficult to distinguish without subtle tests – an S.G. above 4.7 is conclusive for tetrahedrite. | |
3½ | Tin-white, tarnishing to Dark-grey | Grey-black | One perfect (basal) | ARSENIC As |
Trigonal | Usually found in botryoidal fibrous masses | 5.7 | Heated in candle flame it gives off white fumes that have a strong garlic odor (poisonous!) Rare |
3½ to 4 | Brownish-bronze to Bronze-yellow | Black | No cleavage but large grains exhibit an octahedral parting | PENTLANDITE (Fe,Ni)9S8 |
Isometric | Usually massive in granular aggregates | 4.6 to 5.0 | Resembles pyrrhotite but is not magnetic, often mixed with pyrrhotite |
3½ to 4 | Brass-yellow, often iridescent | Black | CHALCOPYRITE CuFeS2 |
Tetragonal | Usually massive, crystals blocky tetrahedrons or wedge-shaped. | 4.1 to 4.3 | Often mixed with pyrite, making a hardness test inconclusive; distinguished from pyrite by softness and shape of crystals. | |
3½ to 4 | Brown to Black | Brown | Good in one direction, poor in another direction | WURTZITE ZnS |
Hexagonal | Usually massive and as banded botryoidal crusts, more rarely as pyramidal hemimorphic crystals | 4.0 to 4.1 | Rare |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
3½ to 4 | Dark-brown to black, sometimes Olive-yellow or Red ("Ruby Jack") to Reddish-black | Dark to Light-brown: streak usually lighter than the color of the sample | Perfect in six directions, three directions usually prominent | SPHALERITE ZnS |
Isometric | Usually in compact crystalline masses, crystals usually blocky pyramidal, appearing tetrahedral | 3.9 to 4.1 | Luster actually resinous, appearing metallic or submetallic |
3½ to 4 | Ruby-red to Reddish-brown | Brownish-red | CUPRITE Cu2O |
Isometric | Usually massive, crystals usually cubes or octahedrons | 6.0 | Luster may be adamantine rather than metallic in crystals | |
3½ to 4 | Black | Green | One perfect direction | ALABANDITE MnS |
Isometric | Usually massive or granular. | 4.0 to 4.1 | Rare |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
4 | Brownish-bronze to Bronze-yellow | Grey-black | PYRRHOTITE Fe1-xS |
Monoclinic pseudo- hexagonal |
Usually massive, crystals as pseudo-hexagonal plates | 4.6 to 4.7 | Magnetic, though may be weak | |
4 | Steel-grey to Iron-black | Black | Indistinct in two directions | STANNITE Cu2FeSnS4 |
Tetragonal | Usually massive, rarely as pseudo-octahedral crystals | 4.3 to 4.5 | Rare |
4 | Steel-grey to Iron-black | Dark reddish-brown to Black | One perfect, two good directions | MANGANITE MnO(OH) |
Monoclinic, pseudo- orthorhombic |
Usually in radiating fibrous masses, crystals often grouped in bundles. | 4.3 | Often associated with pyrolusite; distinguished from that species by its significantly greater hardness |
4 to 4½ | White to Steel-grey | Grey, shiny | PLATINUM Pt |
Isometric | Usually massive in irregular grains or nuggets, crystals rare and usually malformed cubes | 14 to 19 | Malleable, very heavy! Very rare. Distinguished from gold by its color. | |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
5 | Steel-grey | Black | One perfect direction | GLAUCODOT (Co,Fe)AsS |
Orthorhombic | Usually massive, more rarely as prismatic crystals in cruciform penetration twins | 5.9 to 6.1 | Rare; alloclasite, monoclinic, is dimorphous with glaucodot and difficult to distinguish from it, but is probably even rarer |
5 | Yellowish or reddish-brown | Pale-brown to white | Variable: may be good in one direction and poor to good in another direction | MONAZITE (Ce,La,Nd)PO4 |
Monoclinic | Usually massive, granular, may be in crude large crystals | 4.6 to 5.3 (approx.) | Luster usually resinous to waxy, but may be adamantine and may appear sub-metallic |
5 to 5½ | Dark-brown to Black: color black in ferberite brown in hübnerite | Dark-brown to Black: streak darkens with increasing Fe content | 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 | S.G. above about 7.3 indicates ferberite, lower indicates hübnerite |
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 | 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 | |
Hardness | Color | Streak | Cleavage | Name | System | Habit | SG | Notes |
5½ | Dark-brown to Black | Iron-black to Brownish-black | CHROMITE FeCr2O4 (Magnesiochromite is closely related, S.G. 4.2,
Rare. |
Isometric | Usually massive, rarely as octahedral crystals | 4.6 | Luster usually pitchy, submetallic, usually associated with peridotite rocks and accompanied by green or yellow alteration products. | |
5½ to 6½ | Dark-brown to Steel-grey to Black | Rust-red or Indian-red | HEMATITE Fe2O3 |
Trigonal | Usually massive in radiating, reniform, or micaceous aggregates | 4.8 to 5.3 | Usually harder than a knife, but some forms can be softer. (See under Tables IA & IC.) |
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