Earth's Layers and Geological Processes

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These flashcards cover essential terms and concepts related to Earth's layers, geological processes, and dating methods that are crucial for understanding geology.

Last updated 11:07 PM on 2/3/26
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21 Terms

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Geology

The study of the Earth's rocks, minerals, and soils and how they have formed over time.

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Law of Superposition

States that in undisturbed rock layers, a rock layer is older than the layers above it and younger than the layers below it.

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Radioactive Dating

A process to determine the actual age of rocks by measuring the amount of radioactive elements they contain.

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Half-Life

The time it takes for half of a radioactive substance to decay.

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Erosion

The process by which materials are removed from the Earth's surface by natural forces such as water, wind, and ice.

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Intrusion

A layer of igneous rock that forms when magma from the Earth's mantle is injected into rock and cools and solidifies.

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Extrusion

Igneous rocks that form when magma seeps from the Earth and reaches the surface, cooling quickly.

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Fossils

Trace or remains of organisms that lived long ago, providing evidence of past life on Earth.

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Index Fossil

Fossils that are used to identify and date the rock layers in which they are found, specified by their wide distribution and short existence.

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Continental Drift

The gradual movement of continents across the Earth’s surface, as evidenced by matching fossils and geological features.

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Sedimentary Rock

Rock formed from the accumulation and compaction of mineral and organic particles.

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Unconformity

A gap in the geological record that shows where rock layers have been lost due to erosion.

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Differentiation

The process by which Earth separates into distinct layers based on density and material composition.

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Accretion

The process by which particles in space collide and come together due to gravitational pull, leading to the formation of planets.

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Pangaea

A supercontinent that existed during the late Paleozoic and early Mesozoic eras, before it split into the continents we know today.

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Absolute Age

The actual age of a rock or fossil, often determined using techniques such as radioactive dating.

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Relative Dating

A method of determining the age of rocks by comparing them to other rocks.

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Strata

Layers of rock that are deposited over time, which can be studied to understand geological history.

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Lateral Continuity

The principle that sediments are deposited in large, continuous sheets in all directions until they thin out or reach a barrier.

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Faulting

The fracturing of rock layers that occurs when stress is applied, causing the layers to displace.

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Folding

The bending of rock layers due to tectonic forces, which can result in complex structures.

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