Quartz
Quartz is a common, hard, glassy mineral with no cleavage and conchoidal fracture; its many colors make physical tests more reliable than appearance alone.
- Mohs hardness 7; scratches glass
- No cleavage
- Glassy luster on fresh surfaces
Physical-property field guide
Move beyond color. Compare hardness, streak, luster, cleavage, fracture, density, magnetism, and geologic setting to identify common minerals with greater confidence.
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Use converging evidence
Observe first, test gently, and verify with at least two independent properties. Mixed grains, coatings, alteration, and weathering can change the result.
Learn the field-test proceduresNeed help narrowing the possibilities? Use the interactive identifier. If the grains form a mixed material, begin with the rock identification guides.
Foundation collection
Quartz is a common, hard, glassy mineral with no cleavage and conchoidal fracture; its many colors make physical tests more reliable than appearance alone.
Calcite is a relatively soft carbonate mineral recognized by Mohs hardness 3, three-direction rhombohedral cleavage, and vigorous reaction with dilute acid on a fresh surface.
Gypsum is a very soft hydrous sulfate mineral that can be scratched by a fingernail and occurs as clear crystals, white fibrous masses, rosettes, or massive alabaster.
Halite is natural sodium chloride, typically recognized by cubic crystals or three perfect cleavage directions at right angles, softness, and ready solubility in water.
Fluorite is a colorful mineral defined by Mohs hardness 4, glassy luster, and four perfect cleavage directions that can produce octahedral fragments.
Feldspar is a family of abundant rock-forming silicates generally identified by hardness near 6, two cleavage directions, and blocky crystals; precise species identification may require optical or chemical work.
Muscovite is a pale mica that splits into thin, flexible, elastic sheets with a pearly to glassy luster and is commonly colorless, silvery, tan, or pale green.
Biotite is the common field name for dark iron- and magnesium-rich mica, recognized by perfect sheet cleavage, flexible elastic flakes, and brown to black color.
Pyrite is a brassy iron sulfide commonly called fool’s gold; it is harder and more brittle than gold, produces a dark streak, and often forms striated cubes.
Hematite is an iron oxide whose most reliable field clue is a red to reddish-brown streak, even when the specimen itself looks steel gray, black, earthy, or red.
Magnetite is a black iron oxide readily recognized by strong attraction to a magnet, black streak, relatively high density, and commonly octahedral or granular form.
Olivine is an olive-green to yellow-green rock-forming silicate, usually granular, hard, glassy, and lacking good cleavage; gem-quality material is called peridot.
Garnet is a group of hard silicate minerals that commonly forms equant, many-faced crystals with no cleavage; red is common, but garnet also occurs in orange, green, brown, black, and other colors.
Native gold is a dense, soft, malleable yellow metal that bends or flattens instead of shattering and leaves a yellow streak; those properties separate it from pyrite and most glittering minerals.
Chalcopyrite is a brass-yellow copper iron sulfide that is softer and usually deeper yellow than pyrite, commonly tarnishes purple or blue, and leaves a greenish-black streak.
Diamond is crystalline carbon defined by Mohs hardness 10, adamantine luster, high thermal conductivity, and perfect octahedral cleavage, but rough crystals and common imitations usually require professional testing.
Talc is the softest standard mineral at Mohs hardness 1, recognized by its very easy scratch, greasy or soapy feel, pale color, and platy to massive habit.
Dolomite is a calcium-magnesium carbonate with rhombohedral cleavage and hardness about 3.5 to 4; unlike calcite, an unpowdered fresh surface usually reacts weakly with cold dilute acid.
Native copper is a soft, malleable metallic mineral with a fresh copper-red color, high density, and no cleavage; exposed surfaces commonly tarnish brown, black, or green.
Native silver is a dense, soft, malleable metal with a bright silver-white fresh surface that commonly tarnishes gray, brown, or black; it occurs in wires, plates, grains, and irregular masses.
Galena is a dense, metallic lead-gray sulfide recognized by perfect cubic cleavage, a gray to black streak, and unusual heft; it is also a lead-bearing mineral that requires careful handling.
Sphalerite is the principal zinc sulfide, recognized by resinous to adamantine luster, pale yellow to dark brown or black color, perfect cleavage in six directions, and a light-colored streak that may smell sulfurous when freshly scratched.
Corundum is a very hard aluminum oxide mineral with Mohs hardness 9, no cleavage, and commonly barrel-shaped or tabular crystals; transparent red material is ruby and other gem colors are sapphire.
Graphite is a very soft, opaque form of carbon recognized by its dark gray color, greasy feel, perfect basal cleavage, low density, and black mark on paper or porcelain.
Molybdenite is a soft, dense, bluish-silver sulfide with a greasy feel and perfect basal cleavage; its flexible flakes resemble graphite but are substantially heavier and usually lighter in color.
Native sulfur is a very soft, lightweight, bright yellow nonmetallic mineral with a resinous luster, pale streak, and brittle fracture; it is commonly associated with volcanic gases, evaporites, and sulfide oxidation.
Malachite is a vivid green copper carbonate hydroxide commonly recognized by its green streak, banded or botryoidal forms, and occurrence in oxidized copper deposits.
Azurite is a deep blue copper carbonate hydroxide identified by its blue streak, glassy to earthy luster, softness, and occurrence with other oxidized copper minerals such as malachite.
Apatite is a calcium phosphate mineral group used as Mohs hardness 5, commonly recognized by hexagonal crystals, glassy luster, variable color, and hardness between fluorite and feldspar.
Topaz is a hard aluminum silicate mineral identified by Mohs hardness 8, perfect basal cleavage, glassy luster, and commonly prismatic orthorhombic crystals.
Beryl is a hard beryllium aluminum silicate commonly forming six-sided prisms; gem varieties include emerald and aquamarine, but most beryl is pale, cloudy, or opaque.
Tourmaline is a diverse borosilicate mineral group commonly recognized by hard, strongly lengthwise-striated prismatic crystals with triangular to rounded-triangular cross sections.
Kaolinite is a soft white to pale clay mineral commonly occurring as earthy, powdery, or compact masses; reliable identification often requires laboratory methods because individual crystals are microscopic.
Hornblende is a dark amphibole-group mineral commonly identified by elongate prismatic crystals, two good cleavage directions meeting near 56 and 124 degrees, and occurrence in igneous and metamorphic rocks.
Augite is a dark calcium-rich clinopyroxene commonly recognized by short blocky prisms, two cleavage directions close to 90 degrees, Mohs hardness near 5.5 to 6, and occurrence in mafic igneous rocks.
Serpentine is a group of soft green to yellowish hydrous magnesium silicate minerals with greasy, waxy, silky, or fibrous appearances; some fibrous varieties are regulated asbestos minerals.
Chlorite is a group of commonly green, soft sheet silicates recognized by perfect basal cleavage, flexible but generally nonelastic flakes, and widespread occurrence in low-grade metamorphic and altered rocks.
Epidote is commonly a pistachio-green to yellow-green mineral with prismatic habit, glassy luster, one perfect cleavage, and hardness near 6 to 7, widespread in metamorphic and altered rocks.
Barite is a notably heavy, relatively soft barium sulfate mineral commonly recognized by high density, white streak, tabular or bladed crystals, and hardness near 3 to 3.5.
Celestite is a strontium sulfate mineral commonly found as pale blue, white, or colorless tabular crystals with high density, white streak, good cleavage, and hardness near 3 to 3.5.
Kyanite is a bladed aluminum silicate mineral with strongly directional hardness, commonly blue to gray, that forms in aluminum-rich metamorphic rocks at elevated pressure.
Staurolite is a brown to reddish-brown metamorphic mineral known for prismatic crystals and distinctive cross-shaped twins, with hardness near 7 to 7.5 and a pale streak.
Goethite is a brown to yellow-brown iron oxide hydroxide identified by its yellowish-brown streak, earthy to submetallic luster, and common botryoidal, fibrous, stalactitic, or earthy habits.
Rutile is a dense titanium dioxide mineral commonly identified by reddish-brown to black prismatic crystals, strong lengthwise striations, high luster, hardness near 6 to 6.5, and a pale brown streak.
Ilmenite is a dense black to brownish-black iron titanium oxide recognized by its submetallic luster, black to brownish-red streak, weak or variable magnetism, and common occurrence in mafic rocks and heavy-mineral sands.
Zircon is a dense, hard zirconium silicate identified by tetragonal prismatic crystals, high luster, hardness near 7.5, and colors ranging from colorless to brown, red, yellow, green, or blue.
Cassiterite is a very dense tin oxide identified by hardness near 6 to 7, brown to black color, adamantine to submetallic luster, pale streak, and common short prismatic or bipyramidal crystals.
Monazite is a dense yellow-brown to reddish-brown rare-earth phosphate mineral, commonly occurring as resinous accessory crystals or heavy sand grains and often containing naturally occurring thorium and uranium.
Common lookalikes
Compare two possible minerals using the properties that actually separate them—hardness, streak, cleavage, magnetism, acid response, and crystal form.