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Seismic Reflection
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Definition: The process where energy waves bounce off a subsurface boundary separating rock layers of differing densities and return to the surface, allowing geologists to calculate boundary depths based on travel time.

Seismic Refraction
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Definition: The bending of energy waves as they cross a boundary between rock layers with differing wave velocities, densities, or mechanical strengths.

Refracted Wave Arrival Geometry
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Definition: An arrival pattern where recording stations near an epicenter receive direct waves first, while distant stations receive waves passing through a deeper, higher-velocity layer first.

Curved Seismic Paths
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Definition: Arched wave trajectories resulting from continuously increasing pressure with depth, which steadily elevates wave speeds through uniform rock.

P-Wave Shadow Zone
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Definition: A ring-shaped surface belt from 103° to 142° from an epicenter where direct primary waves are absent because they bend sharply downward upon entering the liquid outer core.

S-Wave Shadow Zone
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Definition: A broad region extending from 103° to 180° opposite an epicenter where secondary shear waves cannot pass, demonstrating that the outer core is liquid.

S-Wave Velocity at the Core-Mantle Boundary
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Definition: A complete drop in secondary wave speed to zero kilometers per second at ~2,900 km depth due to the inability of shear energy to travel through liquid metal.

P-Wave Velocity at the Core-Mantle Boundary
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Definition: A sharp reduction in primary wave speed from ~13 km/s down to ~8 km/s at ~2,900 km depth, followed by an increase at ~5,150 km depth upon encountering the solid inner core.

Density Jump at the Core-Mantle Boundary
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Definition: An abrupt rise in mass per unit volume from ~5.5 g/cm³ at the base of the lower mantle to 10-12 g/cm³ at the top of the outer core.

Blue Regions in Seismic Tomography
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Definition: Features on 3D subsurface maps representing faster-than-average wave speeds, corresponding to cooler, denser, or more rigid subducted material.

Red Regions in Seismic Tomography
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Definition: Features on 3D subsurface maps representing slower-than-average wave speeds, corresponding to warmer, softer, or less rigid upwelling material.

Isostatic Equilibrium
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Definition: The mechanical balance of lithospheric blocks floating on the ductile asthenosphere, where taller features require deep roots extending into the mantle.

Erosion
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Definition: The removal of mass from mountain peaks, which lightens the downward load on the crust, causing the lithosphere to rise vertically as mantle material flows inward underneath.

Deposition
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Definition: The accumulation of sediment in low-lying basins, which adds weight to the crust, forcing the lithosphere to sink downward and displacing mantle material outward.

Glacial Rebound
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Definition: The gradual upward vertical movement of the lithosphere following the melting of massive ice sheets, returning the crust toward its original buoyant balance as ductile mantle material flows back underneath.

Geodynamo
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Definition: Driven by convection and electric currents in the liquid outer core.

Curie Point
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Definition: 580°C for magnetite. Cooling below this locks in magnetic alignment (paleomagnetism/remanent magnetism).

Magnetic Reversals
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Definition: Polarity flips average once every 500,000 years and take ~10,000 years to complete.

Positive Magnetic Anomaly
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Definition: Caused by magnetite ore bodies, intrusive gabbro dikes in granite, or basement arches/anticlines.

Negative Magnetic Anomaly
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Definition: Caused by a downdropped fault block (graben) filled with non-magnetic sediment overlying magnetic basalt.

Geothermal Gradient
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Definition: Increases by 25°C per km near the surface (~75°F/mile), but tapers off rapidly in the mantle (~1°C/km).

Core-Mantle Boundary Temperature
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Definition: ~3,700°C ± 600°C

Center of Earth Temperature
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Definition: ~6,400°C ± 600°C

Heat Flow Equivalence
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Definition: Average heat flow from continents equals average heat flow from ocean basins. Continental heat originates from radioactive decay (U, Th, K) in the crust; oceanic heat originates from hot mantle convection below.

Newton’s Law
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Definition: Force decreases with the square of distance.

Positive Gravity Anomaly
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Definition: Regional gravity higher than normal; caused by dense metallic ore bodies or crust held up out of isostatic equilibrium by tectonic forces.

Negative Gravity Anomaly
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Definition: Regional gravity lower than normal; caused by thick low-density sediments, deep mountain roots, or crust held down / undergoing glacial rebound.

Geoid
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Definition: The hypothetical equipotential surface of Earth's gravity field at mean sea level
