Minerals and Rocks – Core Vocabulary

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A comprehensive set of vocabulary flashcards covering minerals, igneous, sedimentary, and metamorphic rocks, their properties, formation processes, and the overarching rock cycle.

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65 Terms

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Mineral

A naturally occurring, inorganic solid with a definable chemical composition and an ordered crystalline structure.

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Naturally Occurring Solid

A substance formed by geologic processes that is solid at Earth-surface temperatures; excludes synthetics, liquids, and gases.

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Definable Chemical Composition

A fixed or narrowly ranged chemical formula that characterizes every specimen of a mineral, e.g., SiO₂ for quartz.

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Crystalline Structure

An internal atomic arrangement that repeats in an orderly pattern, giving a mineral its crystal form and symmetry.

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Typically Inorganic

Describes most minerals, which form from geologic—not biological—processes; biogenic minerals are noted exceptions.

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Biogenic Mineral

A mineral precipitated by living organisms, such as calcite in shells or speleothems.

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Calcite

A carbonate mineral (CaCO₃) common in limestone, marble, and cave formations.

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Physical Properties (Minerals)

Observable traits—color, streak, luster, crystal habit, cleavage, hardness, etc.—used to identify minerals.

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Color

The visible hue of a mineral in hand sample; often unreliable alone for identification.

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Streak

The color of a mineral’s powdered form, tested by scraping on porcelain.

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Luster

The way a mineral reflects light; categories include metallic, glassy, and earthy.

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Crystal Habit

The typical external shape that crystals of a mineral display as they grow.

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Cleavage

The tendency of a mineral to break along planes of weakness related to atomic structure.

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Mohs Hardness Scale

Relative scale (1–10) ranking mineral resistance to scratching, with talc at 1 and diamond at 10.

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Ionic Bond

Chemical bond produced by electron transfer between ions, common in salts like NaCl.

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Covalent Bond

Strong bond formed by electron sharing between atoms, as in diamond.

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Van der Waals Force

Weak electrostatic attraction between molecules; responsible for easy cleavage in graphite.

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Silicate

Mineral group built from silica tetrahedra (SiO₄⁴⁻); composes >95 % of Earth’s crust.

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Silica Tetrahedron

The four-oxygen, one-silicon pyramid that is the structural building block of all silicate minerals.

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Oxide

Non-silicate mineral group with O²⁻ anion; e.g., hematite (Fe₂O₃).

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Sulfide

Mineral group with S²⁻ anion; includes ore minerals like pyrite (FeS₂).

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Sulfate

Mineral group containing SO₄²⁻; gypsum (CaSO₄·2H₂O) is typical.

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Phosphate

Mineral group with PO₄²⁻ anion; fluorapatite (Ca₅(PO₄)₃F) is common in bones and teeth.

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Carbonate

Minerals with CO₃²⁻, notably calcite (CaCO₃) and dolomite [CaMg(CO₃)₂].

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Halide

Mineral group containing halogen ions (Cl⁻, F⁻); examples are halite (NaCl) and fluorite (CaF₂).

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Igneous Rock

Rock formed by solidification of molten material (magma or lava).

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Magma

Molten rock beneath Earth’s surface; may cool to form intrusive rocks.

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Lava

Magma erupted onto Earth’s surface; cools to form extrusive rocks.

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Geothermal Gradient

The rate of temperature increase with depth in Earth, influencing melting.

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Decompression Melting

Partial melting triggered when hot mantle rock rises and pressure drops.

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Addition of Volatiles

Process where water or CO₂ lowers a rock’s melting temperature, aiding magma generation.

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Heat Transfer Melting

Generation of melt when rising magma heats and partially melts surrounding rock.

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Viscosity

A magma’s resistance to flow; controlled by temperature, volatile content, and silica content.

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Magmatic Differentiation

Processes (partial melting, assimilation, fractional crystallization) that create diverse igneous rocks from one magma source.

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Partial Melting

Incomplete melting of a rock, producing silica-rich magma and mafic residue.

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Assimilation

Incorporation of wall-rock pieces into magma, altering its composition.

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Fractional Crystallization

Sequential removal of early-formed minerals from magma, changing remaining melt chemistry.

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Volcanic (Extrusive) Rock

Igneous rock that crystallizes at or near the surface; generally fine-grained.

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Plutonic (Intrusive) Rock

Igneous rock that cools slowly below ground; typically coarse-grained.

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Composition (Igneous)

Overall chemical makeup of an igneous rock, linked to mineral content (felsic, intermediate, mafic, ultramafic).

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Texture (Igneous)

Size, shape, and arrangement of crystals or glass in an igneous rock.

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Bowen’s Reaction Series

Model describing the order of mineral crystallization from cooling magma.

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Aphanitic Texture

Fine-grained igneous texture with crystals too small to see unaided; indicates rapid cooling.

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Phaneritic Texture

Coarse-grained igneous texture with visible crystals; indicates slow cooling.

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Sedimentary Rock

Rock formed by lithification of sediment or precipitation from solution.

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Lithification

Compaction and cementation that transform loose sediment into solid rock.

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Weathering

Physical, chemical, or biological breakdown of pre-existing rock at Earth’s surface.

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Erosion and Transportation

Removal and movement of weathered material by wind, water, ice, or gravity.

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Strata

Horizontal layers of sedimentary rock representing depositional episodes.

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Clastic (Detrital) Rock

Sedimentary rock composed of fragments of pre-existing minerals/rocks, e.g., sandstone.

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Carbonate Rock

Sedimentary rock formed by chemical or biological precipitation of carbonates; e.g., limestone.

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Chert

Hard, microcrystalline quartz sedimentary rock often formed from silica-rich ooze.

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Evaporite

Sedimentary rock (e.g., halite, gypsum) crystallized from evaporating water bodies.

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Coal

Organic sedimentary rock formed from compressed plant material rich in carbon.

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Metamorphic Rock

Rock altered in the solid state by heat, pressure, and chemically active fluids.

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Protolith

The original, unmetamorphosed rock from which a metamorphic rock forms.

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Metamorphic Grade

Intensity of metamorphism, increasing with temperature and pressure; indicated by index minerals.

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Foliation

Planar alignment of platy minerals produced by differential stress during metamorphism.

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Slate

Low-grade foliated metamorphic rock derived from shale; exhibits slaty cleavage.

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Schist

Medium-grade foliated metamorphic rock rich in visible mica flakes.

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Gneiss

High-grade foliated metamorphic rock with compositional banding of light and dark minerals.

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Marble

Nonfoliated metamorphic rock formed from limestone; composed mainly of calcite.

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Quartzite

Nonfoliated metamorphic rock formed from quartz-rich sandstone; extremely hard.

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Rock Cycle

Continuous set of processes that transform rocks among igneous, sedimentary, and metamorphic types.

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Plate Tectonics (and Rock Cycle)

Global mechanism driving rock-forming processes—melting, uplift, burial—through interactions at plate boundaries.