Epizentrum vs. Hypozentrum: Was ist der Unterschied?

Epicenter: The Point on the Surface

The EpicenterThe point on the Earth's surface directly above the hypocenter (focus) where an earthquake originates underground. Often reported as the earthquake's location in news reports. is the point on the Earth's surface directly above where an earthquake begins. It is the location reported in news headlines — "earthquake strikes 30 km south of city X" — because it tells you where on the map the seismic energy originated most directly above ground. The epicenter is the geographically relevant location for emergency responders, residents, and infrastructure managers trying to understand where they should focus their attention.

However, it is crucial to understand that the epicenter is a projected point on the surface, not where the rupture actually started. The actual rupture initiation point is always somewhere below the surface. For a shallow earthquake 10 km deep, the epicenter is a reasonable proxy for the source location. For a deep earthquake 200 km below the surface, the epicenter might be more than 100 km away from the closest surface expression of the fault system, and the area of maximum surface shaking may not even be centred on the epicenter.

Hypocenter: Where the Rupture Begins

The Hypocenter (Focus)The actual point within the Earth where an earthquake rupture initiates. Also called the focus. Depth of the hypocenter significantly affects how an earthquake is felt at the surface. (also called the focus) is the three-dimensional point within the Earth where the earthquake rupture initiates. It is defined by three coordinates: latitude, longitude, and depth. The depth is often the most uncertain of the three, because determining depth requires particularly good data coverage — ideally stations both near the epicenter and at varying distances.

Understanding the hypocenter depth is essential for hazard assessment. Shallow earthquakes (less than 70 km deep) release their energy closer to the surface and generally cause more intense surface shaking for a given magnitude than deep earthquakes. The 2015 Nepal earthquake (Mw 7.8) had a hypocenter approximately 15 km deep, which contributed to its devastating surface shaking. By contrast, deep focus earthquakes in the Subduction ZoneA region where one tectonic plate dives beneath another into the mantle. Subduction zones produce the world's largest earthquakes (M8.5+) and are associated with deep ocean trenches and volcanic arcs.s beneath South America and the Kuril Islands occur at depths exceeding 500–600 km; although some of these events have very large magnitudes, their great depth means the shaking at the surface is spread over a much larger area and is less intense locally.

How Scientists Triangulate Earthquake Locations

Locating an earthquake requires solving for four unknowns: latitude, longitude, depth, and time of origin. The data used are the arrival times of P-Wave (Primary Wave)The fastest seismic wave, traveling through both solid rock and liquid at 5-8 km/s. P-waves compress and expand material in the direction of travel, like a slinky. They arrive first at seismograph stations.s and S-Wave (Secondary Wave)Seismic waves that move rock perpendicular to the direction of travel, arriving after P-waves. S-waves cannot travel through liquids, which proved the Earth's outer core is liquid.s at SeismographAn instrument that detects and records ground motion caused by seismic waves. Modern digital seismographs can detect movements smaller than a nanometer. stations of known location. With the travel time from a station and knowledge of wave velocities in the Earth, a circle of possible hypocenter locations can be drawn around each station. With three stations, the three circles intersect at (ideally) one point that gives the epicenter. With four or more stations, over-determined systems allow both epicenter and depth to be estimated simultaneously.

In practice, Earth's velocity structure is not perfectly known, stations have timing uncertainties, and seismic waves are affected by complex three-dimensional geology. Modern earthquake location algorithms use iterative least-squares fitting to minimise the mismatch between observed and predicted arrival times, often incorporating three-dimensional velocity models and waveform cross-correlation to achieve sub-kilometre location accuracy for well-recorded events. The Global Seismographic Network (GSN)A worldwide network of 150+ broadband seismograph stations that provides comprehensive monitoring of global earthquake activity. Jointly operated by USGS, NSF, and IRIS.'s global station coverage has made it possible to reliably locate earthquakes anywhere on Earth to within a few tens of kilometres under routine operating conditions.

Why Depth Matters: Shallow vs Deep Earthquakes

Earthquake depth profoundly influences the distribution and character of surface shaking. Consider two earthquakes, both of magnitude 7.0: one at 10 km depth and one at 200 km depth. The shallow earthquake concentrates its energy in a small area directly above the hypocenter, producing intense, potentially devastating shaking in a limited region. The deep earthquake spreads its energy over a much larger footprint at the surface, producing moderate shaking over a wide area — potentially felt across an entire country — but with less intensity at any individual location.

Depth also affects what types of secondary hazards are produced. Shallow earthquakes are more likely to generate TsunamiA series of ocean waves generated by sudden displacement of the seafloor during an underwater earthquake. Tsunamis can travel across entire ocean basins at jet speed (700+ km/h).s (if they occur under the ocean and involve significant vertical displacement of the seafloor), LiquefactionA phenomenon where saturated, loose soil temporarily loses strength and behaves like a liquid during strong shaking. Can cause buildings to sink, tilt, or collapse into the ground. of saturated soils, and permanent Ground Rupture (Surface Faulting)Visible displacement of the ground surface along a fault during an earthquake. Structures built across a surface rupture zone can be torn apart regardless of their structural strength. visible at the surface. Very deep earthquakes rarely generate tsunamis because the seafloor deformation, transmitted through hundreds of kilometres of rock, is diffuse rather than concentrated. The geographic footprint of a deep earthquake is so large that even with a high MagnitudeA single number that quantifies the total energy released by an earthquake. Each whole number increase represents roughly 31.6 times more energy released., the local Seismic IntensityA measure of the strength of shaking at a particular location, determined by observed effects on people, structures, and the natural environment. Decreases with distance from the epicenter. at the EpicenterThe point on the Earth's surface directly above the hypocenter (focus) where an earthquake originates underground. Often reported as the earthquake's location in news reports. may be surprisingly modest.

The Role of Seismic Networks in Location Accuracy

The accuracy of hypocenter and epicenter determinations has improved dramatically over the past century, driven by the growth of Seismic NetworkA coordinated group of seismograph stations that continuously monitor earthquake activity. The Global Seismographic Network (GSN) includes 150+ stations providing worldwide coverage.s from a handful of stations to global networks of thousands. The Global Seismographic Network (GSN)A worldwide network of 150+ broadband seismograph stations that provides comprehensive monitoring of global earthquake activity. Jointly operated by USGS, NSF, and IRIS., operated by the USGS (United States Geological Survey)The primary US government agency responsible for monitoring earthquakes, operating the National Earthquake Information Center, and publishing real-time earthquake data worldwide. and partner institutions, provides high-quality broadband data from more than 150 stations worldwide, enabling reliable location of earthquakes above about magnitude 4.0 anywhere on Earth.

Regional dense networks — like those operated by CalTech in Southern California, the Japan Meteorological Agency, and seismological institutes in New Zealand and Switzerland — provide vastly denser station coverage within their regions, enabling location accuracies of a kilometre or less for local events. This precision is essential for aftershock studies, fault mapping, and verifying compliance with nuclear test ban treaties. Use the Distance from Epicenter tool to estimate how far you are from an earthquake's epicentre and how that distance affects the shaking you might experience.