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TitleEarthquake magnitude
AuthorCassidy, J F
SourceEncyclopedia of engineering geology; by Bobrowsky, P (ed.); Marker, B (ed.); Encyclopedia of Earth Sciences Series 2018., https://doi.org/10.1007/978-3-319-12127-7 102-1
Year2018
Alt SeriesNatural Resources Canada, Contribution Series 20170324
PublisherSpringer
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
SubjectsTransport; earthquakes; earthquake magnitudes
Illustrationsgraphs
ProgramAssessing Earthquake Geohazards, Public Safety Geoscience
AbstractDefinition: Earthquake magnitude (M) describes the energy release (or size) of an earthquake.
There are many types of magnitude scales, with the vast majority based on recorded seismic waveforms. Magnitude scales are logarithmic, correct for distance from the earthquake, and are unbounded (the smallest earthquakes are less than zero, and the largest recorded event to date is the 1960 M9.5, Chile earthquake). Some magnitude scales are based on measurements of shorter-period body waves (primary (P) or secondary (S)-waves) and some are based on longer-period surface waves. The original (and most famous) magnitude scale, the 'Richter scale' was developed in the 1930's for California earthquakes (Richter, 1935). The modern, and most commonly-used magnitude scale is moment magnitude, Mw (Hanks and Kanamori, 1979). It is based on seismic moment (Mo) release, which directly relates to the fault rupture area and amount of slip. It is important to note that each unit increase in magnitude represents a 10-fold increase in amplitude of shaking, and a 33-fold increase in energy release. For example, a M7 earthquake releases 1000 times as much energy as a M5 earthquake, and has shaking that is 100 times stronger. Earthquakes can generally be felt starting at M 2-3. Earthquakes may cause minor damage starting at M ~4-5, and earthquakes of M7 or larger are considered major and can be felt (and have the potential to cause damage) up to 100s of km away. Small earthquakes are much more frequent than large earthquakes ' for example, there are, on average, about 1.3 million M2-2.9 earthquakes around the world each year, compared to 15-20 M 7-7.9 events. Scientists are limited to the instrumental recording period (since the late 1800s) for the accurate estimation of earthquake magnitude. Prior to that time, they rely on written and oral reports that describe the earthquake's 'intensity'. Intensity describes the effects of an earthquake on humans or the environment, and requires no instrumental records. Earthquake magnitude has important applications for engineering geology, including numerous empirical relationships developed between magnitude and potential for triggering of landslides and liquefaction. Specifically, a historical (and global) review of earthquake-triggered landslides (including rockfalls, delayed-initiation landslides, lateral spreads and flows) as a function of earthquake magnitude is provided by Keefer (2002). For example, a M 7 earthquake can be expected to generate lateral flows to distances of ~80 km and landslides to distances of ~170 km. A relationship between areas of potential liquefaction and earthquake magnitude is provided by Wang et al. (2006). Based on their work (and references therein) a M 7 earthquake may cause liquefaction to hypocentral distances of ~160 km.
Summary(Plain Language Summary, not published)
This book chapter provides a very short (<500 words) summary of 'earthquake magnitude' for an engineering geology audience. This document summarises the key earthquake magnitude scales and how they work, and provides a few engineering geology applications.
GEOSCAN ID306419