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A vocabulary set covering earthquakes, plate tectonics, weathering/erosion, and related features.
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Focus (hypocenter)
The location within the Earth’s crust where an earthquake originates.
Epicenter
The point on the Earth's surface directly above the focus.
Seismic Waves
Energy waves produced by earthquakes that travel through the Earth’s layers.
P Waves (Primary Waves)
Fastest seismic waves; travel through both fluids and solids; push–pull motion; arrive first.
S Waves (Secondary Waves)
Slower seismic waves; travel only through solids; move rock particles up and down or side to side, perpendicular to the direction of travel.
Surface Waves
Seismic waves that travel near the surface; lower frequency; arrive after body waves and cause most earthquake damage.
Magnitude
Energy released at the earthquake’s source; measured from seismograph readings.
Intensity
Strength of shaking at a location, estimated from eyewitness accounts and damage.
Seismograph
Instrument used to measure and record seismic waves and magnitude.
Plate Tectonics
Theory that Earth’s lithosphere is divided into moving plates whose interactions cause geologic activity.
Mantle
Layer beneath the crust where convection currents drive plate movement.
Convection Currents
Cyclic movement of mantle rock caused by temperature differences, powering plate motion.
Lithosphere
Rigid outer layer of Earth, including the crust and upper mantle.
Plate Boundary
Edge where two tectonic plates meet; boundaries can be divergent, convergent, or transform.
Divergent Boundary
Plates move apart, creating new crust at mid-ocean ridges or rift valleys.
Convergent Boundary
Plates move toward each other; may involve subduction and/or mountain building.
Transform Boundary
Plates slide past one another horizontally, often causing earthquakes.
Subduction
One plate moves beneath another at a convergent boundary, producing earthquakes and volcanoes.
Trenches
Deep oceanic troughs formed at subduction zones.
Island Arc
Chain of volcanic islands formed by subduction of oceanic crust beneath another plate.
Hot Spot
Localized plume of hot mantle that rises toward the surface, causing volcanic activity away from plate boundaries.
Oceanic Crust
Thin, dense crust made mostly of basalt; sinks beneath continental or other oceanic crust at subduction zones.
Continental Crust
Thicker, less dense crust that forms continents and mountains when collision occurs.
Fault
A fracture in rocks where movement has occurred.
Strike‑Slip Fault
Horizontal movement of rocks along a fault, typically at transform boundaries.
Normal Fault
Dip-slip fault where the block above moves downward relative to the block below; common at divergent boundaries.
Reverse Fault
Dip-slip fault where the block above moves upward relative to the block below; common at subduction/convergent boundaries.
Rock Cycle
Processes by which rocks change between igneous, sedimentary, and metamorphic forms.
Igneous
Rock formed when magma cools and crystallizes.
Sedimentary
Rock formed from weathering, erosion, compaction, and cementation of sediments.
Metamorphic
Rock formed from existing rocks transformed by heat and pressure.
Weathering
Chemical and physical breakdown of rocks into sediment.
Chemical Weathering
Chemical changes in minerals, such as oxidation, hydrolysis, and carbonation.
Oxidation
Chemical reaction of minerals with oxygen (e.g., rust formation).
Hydrolysis
Water reacting with minerals to weaken rock structures.
Carbonation
Carbon dioxide in rain forms carbonic acid, contributing to weathering.
Physical (Mechanical) Weathering
Breaking rocks without changing their chemical composition (e.g., frost wedging, abrasion, plant growth).
Erosion
Movement of sediment by wind, water, ice, or gravity.
Deposition
Sediments deposited to form landforms such as deltas, flood plains, dunes, estuaries, and beaches.
Volcano
A vent in the crust through which magma erupts; part of volcanism.
Volcanism
The process of volcanic eruption and related activity, often linked to plate tectonics and hot spots.
Density
Mass per unit volume (commonly expressed in g/cm^3).