Midterm 1 - Important terms and concepts GEOL-1100: Dynamic Earth

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Vocabulary flashcards covering key terms, definitions, and concepts from GEOL-1100 lectures 1–7.

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79 Terms

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Uniformitarianism

Geologic processes today also shaped Earth in the past.

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Atom

Basic unit of matter: protons, neutrons, electrons.

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Proton

Positive particle in nucleus; defines element.

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Neutron

Neutral particle in nucleus; adds to mass.

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Electron

Negative particle orbiting nucleus; controls chemical bonds.

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Element

Substance defined by proton count; can't be broken down chemically.

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Ion

Atom/molecule with charge (lost or gained electrons).

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Anion

Negative ion (gained electrons).

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Cation

Positive ion (lost electrons).

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Isotope

Same protons, different neutrons (variants of an element).

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Nucleosynthesis

Formation of atomic nuclei in stars and early universe.

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Big Bang nucleosynthesis

Light element formation in early universe.

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Stellar nucleosynthesis

Element formation inside stars via fusion.

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Inner planets

Rocky planets: Mercury, Venus, Earth, Mars.

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Outer planets

Gas/ice giants: Jupiter, Saturn, Uranus, Neptune.

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Orbital eccentricity

How elliptical (non-circular) an orbit is.

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Sun composition

Mostly hydrogen and helium (98\%).

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Hydrogen

Lightest element; major part of Sun and gas giants.

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Helium

Second most abundant in Sun; from hydrogen fusion.

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Nuclear fusion in the Sun

Hydrogen to helium conversion, releasing energy.

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Proton-proton chain

Dominant fusion reaction in the Sun.

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Earth’s composition

Rich in iron, oxygen, silicon.

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Planetary differentiation

Earth's materials sorted by density (core, mantle, crust).

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Giant-impact hypothesis

Moon formed from Earth-Mars sized body collision.

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Tidal force

Gravitational forces that deform bodies, creating tides.

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Composition

Types of materials making up a body.

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Temperature

Average kinetic energy of particles.

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Pressure

Force per unit area by particles.

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Volume

Amount of 3D space occupied.

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Density

Mass per unit volume; key for Earth's layering.

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Depth variation (geology)

How properties (T, P, D, C) change with Earth's depth.

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Brittle

Rock fractures readily with little deformation.

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Ductile

Rock deforms plastically without breaking.

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Lithosphere

Rigid outer shell: crust and upper mantle.

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Asthenosphere

Weak, flowing layer beneath lithosphere.

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Mesosphere

Lower mantle region (solid).

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Outer core

Liquid iron-nickel; generates magnetic field.

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Inner core

Solid iron-nickel sphere at Earth's center.

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Crust

Outermost solid shell (continental/oceanic).

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Mantle

Layer between crust and core.

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Core

Earth’s central metallic region.

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Continental crust

Thicker, less dense, granitic rocks.

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Oceanic crust

Thinner, denser, basaltic rocks.

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Density sorting

Materials separate by density during differentiation.

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Convection currents (Earth’s mantle)

Mantle movement by heat, drives plate tectonics.

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Modern atmosphere composition

Mostly nitrogen (N2), oxygen (O2), argon (Ar).

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Ozone (O3)

Trioxygen in stratosphere; absorbs UV.

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Greenhouse gases

Gases (CO2, CH4, H2O) that trap heat.

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Albedo

Reflectivity of Earth’s surface.

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Solar luminosity

Total energy emitted by the Sun.

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Earth’s magnetic field

From outer core liquid iron; shields from solar wind.

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Biosphere

Zone of life; interacts with atmosphere/geosphere.

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Oxygenic photosynthesis

Photosynthesis that releases oxygen.

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Cellular respiration

Metabolic process releasing energy from molecules.

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Nitrogen fixation

Converting N2 to usable forms (ammonia).

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Carbon cycle

Carbon movement: atmosphere, biosphere, oceans, rocks.

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Rocks vs minerals

Minerals are crystalline compounds; rocks are mineral aggregates.

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Crystal structures

Ordered atom arrangement in a mineral.

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Ionic bond

Electrons transferred between atoms.

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Covalent bond

Electrons shared between atoms.

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Metallic bond

Electrons shared collectively in metals.

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Crystal formation

Growth from melt/solution into ordered lattices.

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Mineral diagnostic properties

Features to identify minerals (color, luster, hardness, etc.).

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Mohs hardness scale

Scale (1-10) for scratch resistance.

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Conchoidal fracture

Curved, shell-like fracture (e.g., quartz).

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Atomic substitution

One ion replaces another of similar size in a lattice.

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Polymorph

Same formula, different crystal structure (e.g., diamond/graphite).

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Native element

Mineral of a pure element (e.g., gold).

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Mineral classes

Categories by chemistry: Silicates, Oxides, Sulfides, etc.

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Silicate minerals

Most abundant crustal minerals (feldspar, quartz).

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Silica tetrahedron

SiO_4^{4-} unit; basic silicate building block.

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Important silicates

Quartz, Feldspar, Muscovite, Biotite, Amphibole, Pyroxene, Olivine, Garnet, Staurolite, Kaolinite, Chalcedony.

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Non-silicate minerals

Minerals without silicate structures.

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Major anions (non-silicates)

Key negative groups for mineral classes (O^{2-}, S^{2-}, SO4^{2-}, CO3^{2-}, F^{-}, Cl^{-}, Br^{-}, I^{-}).

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Hematite

Iron oxide mineral (Fe2O3).

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Pyrite

Iron sulfide (FeS_2); 'fool’s gold.'

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Halite

Sodium chloride (NaCl); common halide.

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Calcite

Calcium carbonate (CaCO_3); reacts with acid.

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Evaporitic minerals

Minerals from water evaporation (sulfates, halides).