GEOL 4

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Last updated 12:07 AM on 2/13/25
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43 Terms

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Aftershock

A smaller earthquake that follows the mainshock, occurring in the same region as the initial quake.

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Amplification

The increase in seismic wave amplitude as they pass through softer ground, leading to stronger shaking.

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Anticline

An upward-arching fold in rock layers, typically formed by compressional forces.

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Attenuation

The decrease in seismic wave energy as it travels through the Earth’s materials.

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Body Waves

Seismic waves that travel through the Earth's interior, including P-waves and S-waves.

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Compression

A type of stress that squeezes rocks together, often leading to faulting or folding.

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Dip-Slip Fault

A fault where movement occurs along the dip of the fault plane, either upward (reverse fault) or downward (normal fault).

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Earthquake

The shaking of the Earth's surface caused by the sudden release of energy along a fault.

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Elastic Rebound

The process where rocks deform under stress and then snap back to their original shape, releasing energy and causing an earthquake.

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Epicenter

The point on the Earth's surface directly above the earthquake's focus.

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Fault

A fracture in the Earth's crust along which movement has occurred.

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Focus

The point within the Earth where an earthquake originates.

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Folds

Bends in rock layers caused by compressional forces.

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Footwall

The block of rock below a fault plane.

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Foreshock

A smaller earthquake that precedes the mainshock.

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Hanging Wall

The block of rock above a fault plane.

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Intensity

A measure of the effects of an earthquake at different locations, often determined using the Modified Mercalli Intensity scale.

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Intraplate

Earthquakes that occur within a tectonic plate, rather than at plate boundaries.

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Liquefaction

The process where saturated soil temporarily loses strength due to shaking, behaving like a liquid.

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Magnitude

A numerical measure of an earthquake’s size based on energy release.

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Mainshock

The largest earthquake in a sequence, often followed by aftershocks.

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Modified Mercalli Intensity (MMI)

A scale that measures earthquake intensity based on observed effects and damage.

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Moment Magnitude

A modern scale used to measure earthquake size, based on seismic moment (fault slip, area, and rock rigidity).

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Normal Fault

A dip-slip fault where the hanging wall moves downward relative to the footwall, caused by tension.

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P-Waves (Primary Waves)

The fastest seismic waves that travel through solids, liquids, and gases by compressing and expanding the material.

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Resonance

The amplification of shaking when the frequency of seismic waves matches the natural frequency of a structure.

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Reverse Fault

A dip-slip fault where the hanging wall moves upward relative to the footwall, caused by compression.

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Richter Scale

An older logarithmic scale that measures earthquake magnitude based on seismic wave amplitude.

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Rupture

The breaking and displacement of rock along a fault during an earthquake.

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S-Waves (Secondary Waves)

Seismic waves that move perpendicular to their direction of travel; they only move through solids.

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Scarp

A steep slope or cliff formed by fault movement or erosion.

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Seismometer

An instrument that detects and records seismic waves.

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Shear

A type of stress that causes parts of a material to slide past each other in opposite directions.

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Strain

The deformation of rocks due to stress.

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Stress

The force applied to a material, which can cause deformation and lead to earthquakes.

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Strike-Slip Fault

A fault where horizontal motion occurs due to shear stress, such as the San Andreas Fault.

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Subsidence

The sinking or downward settling of the Earth’s surface.

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Surface Waves

Seismic waves that travel along the Earth's surface, causing most earthquake damage.

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Syncline

A downward-curving fold in rock layers.

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Tectonic Creep

The slow, continuous movement along a fault without noticeable earthquakes.

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Tension

A type of stress that pulls rocks apart, leading to normal faulting.

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Tsunami

A large ocean wave generated by underwater earthquakes, landslides, or volcanic eruptions.

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Warning

A system that detects early seismic waves and alerts people before strong shaking arrives.