Linked from

The 47 pages that link to Seismology, each with the reason it gives.

• Plate tectonicsRelated: Global earthquake distribution mapped the plate boundaries before plates were named.

• Seismic waveNarrower topic: Seismology uses wave observations to infer earthquakes and Earth's internal structure.

• Earthquake engineeringNarrower topic: Earthquake engineering draws on seismology to characterize sources and shaking.

• AcousticsRelated: Seismic waves share mechanical-wave principles with sound but travel through geological structures.

• SeismometerNarrower topic: Seismometers provide the observations on which much of the field relies.

• San Andreas FaultRelated: The 1906 rupture created the field's founding dataset and its first fault-rupture measurements.

• Moment magnitude scaleNarrower topic: The scale emerged from seismology’s effort to measure earthquake sources consistently.

• P wavesNarrower topic: P-wave observations are foundational evidence in this field.

• Volcano monitoringRelated: Earthquake patterns can reveal magma movement and changes in volcanic conduits.

• GeophysicsNarrower topic: It is a major branch of geophysics centered on elastic waves.

• OscillationNarrower topic: Ground motion records oscillations generated by earthquakes and their waves.

• S-waveNarrower topic: S-waves are a principal signal studied in seismology.

• United States Geological SurveyRelated: USGS uses seismic observations to locate earthquakes and characterize their sources and impacts.

• Poisson's ratioRelated: Elastic-wave speeds can be related to Poisson's ratio in models of subsurface materials.

• VolcanologyRelated: Seismic signals help locate moving magma and characterize volcanic interiors.

• Dispersion relationRelated: Seismic dispersion reveals how wave speed varies with frequency and subsurface structure.

• AsthenosphereRelated: Seismic velocities, not drilling, revealed the asthenosphere's existence.

• Tsunami warning systemRelated: Earthquake location, depth, and magnitude provide the first clues to tsunami potential.

• Comprehensive Nuclear-Test-Ban TreatyNarrower topic: The treaty’s underground-explosion detection depends on seismological methods.

• Strike-slip faultNarrower topic: Seismic observations constrain rupture, depth, and slip on strike-slip faults.

• Beno GutenbergNarrower topic: Gutenberg’s work helped make seismic waves a tool for probing deep planetary structure.

• Inge LehmannNarrower topic: Lehmann’s discovery showed how seismic observations can reveal inaccessible planetary structure.

• Longitudinal waveNarrower topic: Seismologists infer underground structure from longitudinal P-wave arrivals.

• 1755 Lisbon earthquakeNarrower topic: The catastrophe encouraged systematic observation and natural explanations of earthquakes.

• Surface waveNarrower topic: Surface waves are analyzed to measure earthquakes and probe Earth's interior.

• Earth's massRelated: Wave speeds and paths help test models of the interior that must fit Earth's measured mass.

• Earth's outer coreNarrower topic: Seismic observations establish the outer core's boundaries and liquid state.

• High-pressure mineral physicsRelated: It supplies interior observations that high-pressure mineral measurements help interpret.

• Earth's inner coreNarrower topic: Seismology supplies the indirect measurements used to investigate Earth’s inaccessible center.

• Mantle transition zoneRelated: Seismic imaging provides most evidence for the zone’s boundaries and structure.

• Andrija MohorovičićNarrower topic: His research helped make seismic-wave analysis a method for probing Earth’s interior.

• Earthquake catalogNarrower topic: It supplies the methods used to detect and describe cataloged earthquakes.

• Harold JeffreysNarrower topic: Jeffreys used seismic-wave travel times to investigate Earth’s internal structure.

• Gutenberg–Richter lawNarrower topic: The relationship became a foundational statistical regularity within this field.

• Love waveNarrower topic: Love waves entered seismology as both a predicted mode and an observable earthquake phase.

• Mineral physicsNarrower topic: Mineral elastic properties let seismologists interpret wave speeds in terms of interior materials.

• Planetary coreRelated: Seismic waves provide the main direct evidence about Earth’s deep core structure.

• Internal structure of EarthNarrower topic: Seismology supplies the principal observational evidence for the planet’s layered interior.

• Chersky RangeNarrower topic: It helps investigate earthquakes in the active Chersky seismic region.

• Birch's lawNarrower topic: Birch's law provides a bridge between measured wave speeds and material properties.

• GeologistRelated: Seismic waves reveal structures deep below exposures and drill sites.

• Maurice EwingNarrower topic: Ewing applied seismic methods to the ocean floor as well as earthquakes and Earth's interior.

• Old FaithfulRelated: Seismic instruments can detect signals associated with geyser activity and underground fluid movement.

• Seismic magnitude scalesNarrower topic: Magnitude scales are one set of tools within this broader study.

• Charles RichterNarrower topic: Richter’s career helped shape modern quantitative seismology.

• Composition of astronomical objectsRelated: Seismic measurements constrain interior layers and density profiles that help identify bulk composition.

• History of geophysicsBroader topic: Earthquake waves revealed deep structure that direct observation could not reach.