The Mineral Identification Key |
Table IIC-1: Streak not colored, Cleavage prominent, Hardness 2½ to 3: (Can not be scratched by a fingernail, can be scratched by a copper penny, streak white or one.) [Previous Table] [Next Table]
Cleavage | Hardness | Color | Luster | Name | System | Habit | SG | Notes |
Perfect in one direction (basal) | 2½ to 4 | Lilac, Lavender, Greyish- to Greenish-white | Pearly on cleavage surfaces | LEPIDOLITE (Mica Group) |
Monoclinic, pseudo-hexagonal | Usually as aggregates of tiny flakes, also as "books" of larger sheets, rarely as diamond-shaped or distorted hexagonal shaped crystals, flakes or sheets | 2.8 to 3.0 |
Elastic, harder than other common micas – except for margarite (see below). |
Perfect in one direction (basal) | 3½ to 5 | Deep to pale Lilac, Grey to White | Pearly on cleavage surfaces | MARGARITE (Mica Group) CaAl2(Al2Si2)O10(OH)2 |
Monoclinic | Usually as flaky aggregates or cross-grain "books" sandwiched in a matrix of chlorite-rich amphibolite schist | 3.0 to 3.1 | Bends little and then breaks – "brittle mica." Hardest of the common micas. |
Cleavage | Hardness | Color | Luster | Name | System | Habit | SG | Notes |
Perfect in three directions (cubic) | 2 | Colorless to White (may be stained by impurities) | Vitreous to sub-vitreous | HALITE (Common Salt, Rock Salt) NaCl |
Isometric | Usually as granular crystalline masses or small cubic crystals | 2.17 | Has a salty taste. Halite and sylvite can be hard to tell apart, but sylvite has a more bitter taste |
Perfect in three directions (cubic) | 2 | Colorless to White (may be stained by impurities) | Vitreous to sub-vitreous | SYLVITE (Potassium Salt) KCl |
Isometric | Usually as granular crystalline masses or small cubic crystals | 1.97 to 1.99 | Has a salty taste. Sylvite and halite can be hard to tell apart, but sylvite has a more bitter taste |
Distinct in one direction (prismatic), good in a second
direction (basal) and fair to poor in a third direction (rhombic overall) |
2½ to 3 | Colorless or White to Greyish-white or Greyish-brown | Adamantine to sub-adamantine, may be vitreous to resinous on some surfaces | ANGLESITE PbSO4 |
Orthorhombic | Usually in crystalline masses, crystals usually small and tabular, rarely prismatic | 6.2 to 6.4 | Streak white; Massive material may be difficult to distinguish from cerussite without testing for SO4 vs. CO3 (See cerussite below). |
Cleavage | Hardness | Color | Luster | Name | System | Habit | SG | Notes |
Perfect in three directions, corners 120o or 60o (rhombic) | 3; but may be 2 across the top surface of prismatic crystals with a flat termination | Usually Clear or White to Tan or Grey, but may be tinted many colors | Vitreous to sub-vitreous | CALCITE CaCO3 |
Trigonal | May be in cleavable masses producing rhombs, granular masses (limestone and marble), scalenohedral ("dogtooth") crystals, rhombohedral crystals, flattened rhombohedral ("nailhead") crystals, or a wide variety of related shapes; The many varied habits of calcite crystals make this one of the species that can be tough to identify by crystal form alone. Few people, if any, are familiar with all the forms it takes. (there are over 800 crystals forms known for this species to date…) | 2.71 | White streak; clear rhombs show a doubled image of print viewed through them, effervesces in cold, dilute acid – even in vinegar or Coke to a small degree. |
Cleavage | Hardness | Color | Luster | Name | System | Habit | SG | Notes |
Perfect in two directions (prismatic) and fair in a third | 3 | Colorless, White, or Grey (may be stained other colors) | Vitreous to sub-vitreous | KERNITE Na2B4O6(OH)2.3H2O |
Monoclinic | Usually in cleavable crystalline masses | 1.95 | Splintery cleavage fragments |
Imperfect in one direction (basal), distinct in another
direction (rhombic), may not be seen |
3 to 3½ | Colorless to White or Greyish-white, may be tinted other colors | Vitreous to sub-vitreous | WITHERITE (Aragonite Group) BaCO3 |
Orthorhombic, pseudo-hexagonal | Usually as stout prismatic twinned crystals with a hexagonal cross section, often with pyramidal terminations on both ends, more rarely as globular to botryoidal clusters, coarse fibrous aggregates, and granular | 4.29 | Often hazed, will effervesce in cold acid. |
Perfect in two directions, imperfect to good in a third | 3 to 3½ | Colorless to White or Greyish-white, may be tinted other colors | Vitreous and/or pearly | ANHYDRITE CaSO4 |
Orthorhombic | Usually in coarsely crystalline masses exhibiting a pseudo-cubic cleavage, or in granular masses with no cleavage apparent, crystals rare and usually equant or thick tabular | 2.9 to 2.98 |
Pseudo-cubic cleavage |
Cleavage | Hardness | Color | Luster | Name | System | Habit | SG | Notes |
Distinct in one direction (prismatic), good in a second
direction (basal) and fair to poor in a third direction (rhombic overall) |
3 to 3½ | Colorless to White or Greyish-white, may be tinted other colors | Vitreous, pearly on basal cleavage surfaces |
BARITE BaSO4 |
Orthorhombic | Usually in clusters or aggregates of platy to tabular crystals | 4.5 | Distinguish from Celestine by SG or a flame test (lime green) |
Distinct in one direction (prismatic), good in a second
direction (basal) and fair to poor in a third direction (rhombic overall) |
3 to 3½ | Colorless to White or Greyish-white, Blue, may be tinted other colors | Vitreous, pearly on basal cleavage surfaces | CELESTITE (Celestine) SrSO4 |
Orthorhombic | Usually in clusters or aggregates of platy to tabular crystals | 3.95 to 3.97 | Distinguish from Barite by SG or a flame test (bright red) |
Note: The above three members of the Barite Group are most easily told apart by their S.G.s Anglesite is noticeably heavier than the other two, barite may feel heavier than celestite.
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