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47 Terms

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Hypothesis

A proposed explanation or prediction that can be tested through experimentation or observation.

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Isotope

Atoms of the same element that have different numbers of neutrons, resulting in different atomic masses.

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Geothermal gradient

The rate at which temperature increases with depth in the Earth's crust.

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Scientific law

A statement that describes a natural phenomenon and is supported by extensive experimental evidence.

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Covalent bond

A chemical bond formed when two atoms share electrons.

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Silicate tetrahedron

A fundamental building block of silicate minerals, consisting of one silicon atom bonded to four oxygen atoms.

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Scientific theory

A well-substantiated explanation of some aspect of the natural world that is based on a body of evidence.

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Ionic bond

A chemical bond formed between two ions of opposite charges.

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Igneous rock

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

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Catastrophism

The belief that Earth's geological features are primarily the result of sudden, violent events.

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Metallic bond

A chemical bond formed by the attraction between metal atoms and the delocalized electrons.

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Metamorphic rock

Rock that has undergone changes in texture, mineralogy, or chemical composition due to high temperature and pressure.

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Principle of Uniformitarianism

the same natural laws and processes that operate in our present-day scientific observations have always operated in the universe in the past and apply everywhere in the universe

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Sedimentary rock

Rock formed from the accumulation and lithification of sediments.

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Atom

The basic unit of matter, consisting of a nucleus (containing protons and neutrons) and electrons orbiting around it.

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Rock cycle

The continuous process of formation, destruction, and reformation of rocks on Earth's surface.

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Lithosphere

The rigid outer layer of the Earth, consisting of the crust and uppermost part of the mantle.

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Valence electron

An electron in the outermost shell of an atom that is involved in chemical bonding.

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Lava

Molten rock that reaches the Earth's surface during a volcanic eruption.

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Asthenosphere

The partially molten, ductile layer of the Earth's mantle beneath the lithosphere.

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Cation

A positively charged ion.

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Magma

Molten rock beneath the Earth's surface.

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Geochronology

The study of the age of rocks and geological events.

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Anion

A negatively charged ion.

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Intrusive igneous rock

Igneous rock that forms from the solidification of magma beneath the Earth's surface.

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Seismology

The study of earthquakes and seismic waves.

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Radius ratio

The ratio of the radii of two ions in an ionic compound, which determines the coordination number and crystal structure.

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Extrusive igneous rock

Igneous rock that forms from the solidification of lava on the Earth's surface.

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Topography

The arrangement of the natural and artificial physical features of an area.

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Bravais lattices

The 14 possible three-dimensional arrangements of points in a crystal lattice.

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Plutonic rock

Another term for intrusive igneous rock, referring to its association with plutons.

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Mid-ocean ridge

Underwater mountain range formed by plate tectonics where new oceanic crust is created.

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Unit cell

The smallest repeating unit of a crystal lattice.

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Volcanic rock

Rock formed from the solidification of lava on the Earth's surface.

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Deep-ocean trench

A long, narrow, and steep depression in the ocean floor, usually associated with subduction zones.

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Crystal lattice

The regular arrangement of atoms, ions, or molecules in a crystalline solid.

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Decompression melting

The melting of rock due to a decrease in pressure as it rises towards the Earth's surface.

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Subduction zone

A region where one tectonic plate is forced beneath another plate into the Earth's mantle.

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Polymorph

Different forms of the same substance with different crystal structures.

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Heat transfer

The movement of thermal energy from one object or substance to another.

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Geotherm

The temperature distribution within the Earth.

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Nucleation

The initial formation of a solid phase from a liquid or gas phase.

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