Independent seismic context • Updated 28 August 2026Verify urgent alerts with local emergency authorities
Understanding earthquakes

Glossary of earthquake terms

A practical A–Z reference to the language used in seismic reports, from acceleration and aftershocks to subduction, surface waves and tsunami.

Layered geological terrain illustrating earthquake science for Earthquake Report

Earthquake reports combine measurements, geological concepts and descriptions of observed effects. This shortened glossary explains commonly encountered terms in plain language.

Reading note: Magnitude describes an earthquake’s size, while intensity describes shaking and effects at a particular place. Early event values may be revised as more seismic stations report.

A

Acceleration
The rate at which velocity changes. Ground acceleration is commonly expressed in metres per second squared or as a fraction of standard gravity, g.
Active fault
A fault considered capable of renewed movement within the period relevant to a hazard assessment. The time criteria vary by region and application.
Aftershock
An earthquake occurring after the largest event in a sequence and within the same general source area. Aftershocks can continue for weeks, months or longer.
Asthenosphere
A mechanically weak and slowly deforming region of the upper mantle beneath the lithosphere. Tectonic plates move above it.

B

Blind fault
A fault that does not reach the ground surface. Movement on a blind fault can still produce strong shaking and folding above the rupture.
Body waves
Seismic waves that travel through Earth’s interior. P waves and S waves are the principal types.
Building code
Rules establishing minimum requirements for the design, construction and occupancy of structures. Seismic provisions seek to reduce collapse and protect life during shaking.

C

Continental crust
The outer solid layer forming the continents. It is generally thicker and less dense than oceanic crust.
Critical structures
Facilities whose continued operation is important during an emergency, or whose failure could have severe consequences, such as hospitals, major utilities, bridges and emergency-response facilities.
Crust
Earth’s outermost major solid layer. Its thickness varies beneath continents and oceans, and its brittle portions host many earthquakes.

D

Deep earthquake
An earthquake with a hypocentre deeper than 300 kilometres under a widely used scientific classification. Deep events occur mainly within descending tectonic plates.
Depth
The distance below Earth’s surface to an earthquake’s hypocentre. Depth is often less certain than horizontal location in an initial report.
Duration
The interval during which measurable or strong ground motion persists. Perceived duration varies with distance, geology and building response.

E

Earthquake
Ground motion and radiated seismic energy produced most commonly by sudden slip on a fault, and sometimes by volcanic activity or other abrupt stress changes.
Earthquake risk
The potential for harm or loss when earthquake hazards interact with exposed people, buildings, infrastructure and their vulnerability.
Epicentre
The point on Earth’s surface directly above the hypocentre where rupture begins. It is not necessarily the location of the strongest shaking or greatest effects.

F

Fault
A fracture or zone of fractures across which blocks of rock have moved relative to one another.
Fault plane
The surface along which fault movement occurs.
Fault scarp
A step-like landform produced where displacement on a fault reaches or deforms the surface.
Fault trace
The line where a fault intersects the ground surface, or its representation on a geological map.
Focal depth
Another term for the depth of an earthquake’s hypocentre.
Focus
Another name for the hypocentre: the point within Earth where rupture starts.

G

Ground motion
Movement of the ground caused by seismic waves. It may be described using displacement, velocity, acceleration, frequency and duration.
Gutenberg–Richter relationship
An empirical relationship showing that smaller earthquakes generally occur much more often than larger ones in a defined region and period.

H

Hazard
A potentially damaging earthquake-related phenomenon, including shaking, surface rupture, liquefaction, landslides, deformation and tsunami. Hazard is not the same as risk.
Hypocentre
The point within Earth where an earthquake rupture initiates. It is also called the focus.

I

Intensity
A description of shaking severity and observed effects at a particular location. Intensity can vary widely across the area affected by one earthquake.
Intermediate-depth earthquake
An earthquake whose hypocentre is approximately 70 to 300 kilometres below the surface.

J

JMA seismic intensity
A scale used by the Japan Meteorological Agency to describe local shaking intensity. It is distinct from earthquake magnitude.

L

Landslide
Downslope movement of rock, soil or debris under gravity. Earthquake shaking can trigger landslides on susceptible slopes.
Latitude
Angular distance north or south of the equator, expressed in degrees.
Liquefaction
A loss of strength in water-saturated granular soil when shaking raises pore-water pressure. The affected ground can deform and lose its ability to support structures.
Lithosphere
Earth’s rigid outer shell, comprising the crust and uppermost mantle and divided into tectonic plates.
Local site conditions
The soil, rock, groundwater and topographic characteristics that influence shaking at a location.
Locked fault
A fault segment where friction prevents steady slip while tectonic strain may continue to accumulate.
Longitude
Angular distance east or west of the prime meridian, expressed in degrees.

M

Magnitude
A logarithmic measure of an earthquake’s size derived from seismic recordings. A one-unit increase represents ten times the recorded wave amplitude and roughly 32 times the energy release, although the precise relationship depends on the measure used.
Mainshock
The largest earthquake in a recognised sequence. An event can be reclassified if a larger earthquake follows.
Mantle
The major rocky layer between Earth’s crust and core, extending to a depth of about 2,900 kilometres.
Modified Mercalli intensity
A twelve-level scale, written with Roman numerals, describing observed shaking and effects from not felt to extreme.
Moment magnitude (Mw)
A magnitude scale based on seismic moment, which reflects fault area, slip and rock rigidity. It performs well across a broad range of earthquake sizes.

O

Oceanic crust
The relatively thin, dense crust beneath the oceans, composed mainly of basaltic rock.
Oceanic trench
A long, deep depression in the seafloor commonly associated with a subduction zone.
Oscillator
A system that moves back and forth around an equilibrium position. Simplified oscillators are used to model how structures respond to shaking.

P

P wave
The fastest seismic body wave. It alternately compresses and expands material in the direction the wave travels and can pass through solids and fluids.
Peak ground acceleration (PGA)
The largest ground acceleration measured or estimated during an earthquake. PGA is one useful engineering measure but does not describe every aspect of damaging motion.
Plate
A large, comparatively rigid section of the lithosphere that moves relative to neighbouring plates.
Plate tectonics
The framework explaining the motion and interaction of lithospheric plates. Many earthquakes occur at subduction zones, spreading ridges and transform boundaries.
Preparedness
Planning, knowledge, supplies, training and coordination developed before an emergency to support an effective response and recovery.

R

Resilience
The capacity of people, communities and systems to withstand disruption, maintain essential functions and recover.
Reverse fault
An inclined fault on which the block above the fault plane moves upward relative to the block below.
Risk
The probability and consequences of loss arising from the interaction of a hazard with exposure and vulnerability.
Risk assessment
A structured analysis of hazards, exposed assets, vulnerability and capacity used to understand potential consequences and support decisions.
Rupture
The process by which slip spreads across a fault during an earthquake. Rupture may propagate mainly in one direction or in several directions.

S

S wave
A shear body wave whose particle motion is perpendicular to its direction of travel. S waves pass through solids but not fluids.
Seismic hazard
The probability that specified earthquake effects, such as a level of ground motion, will occur at a location during a stated period.
Seismic station
A site where instruments record ground motion or other geophysical observations.
Seismic waves
Elastic waves generated by an earthquake or another sudden energy source. Body waves travel through Earth, while surface waves travel near its exterior.
Seismicity
The distribution of earthquakes in space, time and magnitude within a region.
Seismogram
The recorded signal produced by a seismic instrument.
Seismometer
An instrument that detects and measures ground motion. A recording system paired with the sensor is often called a seismograph.
ShakeMap
A map estimating the distribution of ground motion and shaking intensity after an earthquake using instrument readings, observations and models.
Shallow earthquake
An earthquake with a hypocentre less than about 70 kilometres deep. Shallow events can produce strong local shaking, though damage cannot be inferred from depth alone.
Strike-slip fault
A usually steep fault on which blocks move primarily horizontally past one another.
Subduction
The process in which one tectonic plate descends beneath another into the mantle.
Surface faulting
Permanent displacement or deformation that reaches the ground surface during fault movement.
Surface wave
A seismic wave that travels along or near Earth’s surface. Love and Rayleigh waves are common types.

T

Thrust fault
A low-angle reverse fault on which the upper block moves up and over the lower block.
Tsunami
A series of long ocean waves caused by substantial displacement of water, most commonly from seafloor movement during a large earthquake and sometimes from landslides or volcanic activity.

V

Velocity
The rate and direction of ground displacement over time. Ground velocity is often reported in centimetres per second.
Common distinctions

Glossary FAQ

Are magnitude and intensity the same?

No. Magnitude is an estimate of the earthquake’s overall size. Intensity describes shaking and effects at a specific place.

Why can earthquake depth change?

Initial locations use limited data. As more station readings are analysed, agencies may refine the hypocentre and reported depth.

Is the epicentre always the worst-hit place?

No. Effects also depend on rupture direction, depth, distance, local geology, buildings and other conditions.

What is the difference between hazard and risk?

Hazard concerns the chance and severity of earthquake effects. Risk also considers who and what is exposed and how vulnerable they are.

Can an aftershock be larger than the mainshock?

If a later event is larger, it becomes the mainshock and the earlier event may be classified as a foreshock.

Does a shallow earthquake always cause damage?

No. Depth matters, but magnitude, location, ground conditions, construction and exposure also influence outcomes.