Epicenter, the Glossary
The epicenter, epicentre, or epicentrum in seismology is the point on the Earth's surface directly above a hypocenter or focus, the point where an earthquake or an underground explosion originates.[1]
Table of Contents
39 relations: Alaska, Ancient Greek, Bryan A. Garner, Bulk density, Clock, Degree (angle), Displacement (geometry), Earth, Earth's outer core, Earthquake, Fault mechanics, Focal mechanism, Gardner's relation, Garner's Modern English Usage, Ground motion, Hypocenter, Latinisation of names, Longitudinal wave, Moment magnitude scale, Neo-Latin, Oxford University Press, P wave, Pendulum, Refraction, Robert Mallet, S wave, Seismic hazard, Seismic wave, Seismogram, Seismology, Seismometer, Shadow zone, Subduction, Time, Transverse wave, Trilateration, Václav Láska (mathematician), William Safire, 2002 Denali earthquake.
- Geographic position
- Geometric centers
Alaska
Alaska is a non-contiguous U.S. state on the northwest extremity of North America.
Ancient Greek
Ancient Greek (Ἑλληνῐκή) includes the forms of the Greek language used in ancient Greece and the ancient world from around 1500 BC to 300 BC.
See Epicenter and Ancient Greek
Bryan A. Garner
Bryan Andrew Garner (born November 17, 1958) is an American legal scholar and lexicographer.
See Epicenter and Bryan A. Garner
Bulk density
In materials science, bulk density, also called apparent density, is a material property defined as the mass of the many particles of the material divided by the bulk volume.
See Epicenter and Bulk density
Clock
A clock or chronometer is a device that measures and displays time.
Degree (angle)
A degree (in full, a degree of arc, arc degree, or arcdegree), usually denoted by ° (the degree symbol), is a measurement of a plane angle in which one full rotation is 360 degrees.
See Epicenter and Degree (angle)
Displacement (geometry)
In geometry and mechanics, a displacement is a vector whose length is the shortest distance from the initial to the final position of a point P undergoing motion.
See Epicenter and Displacement (geometry)
Earth
Earth is the third planet from the Sun and the only astronomical object known to harbor life.
Earth's outer core
Earth's outer core is a fluid layer about thick, composed of mostly iron and nickel that lies above Earth's solid inner core and below its mantle.
See Epicenter and Earth's outer core
Earthquake
An earthquakealso called a quake, tremor, or tembloris the shaking of the Earth's surface resulting from a sudden release of energy in the lithosphere that creates seismic waves. Epicenter and earthquake are seismology.
Fault mechanics
Fault mechanics is a field of study that investigates the behavior of geologic faults.
See Epicenter and Fault mechanics
Focal mechanism
The focal mechanism of an earthquake describes the deformation in the source region that generates the seismic waves. Epicenter and focal mechanism are seismology.
See Epicenter and Focal mechanism
Gardner's relation
Gardner's relation, or Gardner's equation, named after G. H. F. Gardner and L. W. Gardner, is an empirically derived equation that relates seismic P-wave velocity to the bulk density of the lithology in which the wave travels. Epicenter and Gardner's relation are seismology.
See Epicenter and Gardner's relation
Garner's Modern English Usage
Garner's Modern English Usage (GMEU), written by Bryan A. Garner and published by Oxford University Press, is a usage dictionary and style guide (or 'prescriptive dictionary') for contemporary Modern English.
See Epicenter and Garner's Modern English Usage
Ground motion
Ground motion is the movement of the Earth’s surface from earthquakes or explosions. Epicenter and Ground motion are seismology.
See Epicenter and Ground motion
Hypocenter
A hypocenter or hypocentre, also called ground zero or surface zero, is the point on the Earth's surface directly below a nuclear explosion, meteor air burst, or other mid-air explosion. Epicenter and hypocenter are Geometric centers and seismology.
Latinisation of names
Latinisation (or Latinization) of names, also known as onomastic Latinisation, is the practice of rendering a non-Latin name in a modern Latin style.
See Epicenter and Latinisation of names
Longitudinal wave
Longitudinal waves are waves in which the vibration of the medium is parallel to the direction the wave travels and displacement of the medium is in the same (or opposite) direction of the wave propagation.
See Epicenter and Longitudinal wave
Moment magnitude scale
The moment magnitude scale (MMS; denoted explicitly with M or or Mwg, and generally implied with use of a single M for magnitude) is a measure of an earthquake's magnitude ("size" or strength) based on its seismic moment.
See Epicenter and Moment magnitude scale
Neo-Latin
Neo-LatinSidwell, Keith Classical Latin-Medieval Latin-Neo Latin in; others, throughout.
Oxford University Press
Oxford University Press (OUP) is the publishing house of the University of Oxford.
See Epicenter and Oxford University Press
P wave
A P wave (primary wave or pressure wave) is one of the two main types of elastic body waves, called seismic waves in seismology. Epicenter and p wave are seismology.
Pendulum
A pendulum is a device made of a weight suspended from a pivot so that it can swing freely.
Refraction
In physics, refraction is the redirection of a wave as it passes from one medium to another.
Robert Mallet
Robert Mallet (3 June 1810 – 5 November 1881) was an Irish geophysicist, civil engineer, and inventor who distinguished himself by research concerning earthquakes (and is sometimes known as the father of seismology).
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S wave
In seismology and other areas involving elastic waves, S waves, secondary waves, or shear waves (sometimes called elastic S waves) are a type of elastic wave and are one of the two main types of elastic body waves, so named because they move through the body of an object, unlike surface waves. Epicenter and s wave are seismology.
Seismic hazard
A seismic hazard is the probability that an earthquake will occur in a given geographic area, within a given window of time, and with ground motion intensity exceeding a given threshold.
See Epicenter and Seismic hazard
Seismic wave
A seismic wave is a mechanical wave of acoustic energy that travels through the Earth or another planetary body. Epicenter and seismic wave are seismology.
See Epicenter and Seismic wave
Seismogram
A seismogram is a graph output by a seismograph.
Seismology
Seismology (from Ancient Greek σεισμός (seismós) meaning "earthquake" and -λογία (-logía) meaning "study of") is the scientific study of earthquakes (or generally, quakes) and the generation and propagation of elastic waves through the Earth or other planetary bodies.
Seismometer
A seismometer is an instrument that responds to ground displacement and shaking such as caused by quakes, volcanic eruptions, and explosions.
Shadow zone
A seismic shadow zone is an area of the Earth's surface where seismographs cannot detect direct P waves and/or S waves from an earthquake. Epicenter and shadow zone are seismology.
Subduction
Subduction is a geological process in which the oceanic lithosphere and some continental lithosphere is recycled into the Earth's mantle at convergent boundaries.
Time
Time is the continued sequence of existence and events that occurs in an apparently irreversible succession from the past, through the present, and into the future.
Transverse wave
In physics, a transverse wave is a wave that oscillates perpendicularly to the direction of the wave's advance.
See Epicenter and Transverse wave
Trilateration
Trilateration is the use of distances (or "ranges") for determining the unknown position coordinates of a point of interest, often around Earth (geopositioning).
See Epicenter and Trilateration
Václav Láska (mathematician)
Václav Jan Láska (1862–1943) was a Czech surveyor, astronomer, geophysicist, and mathematician.
See Epicenter and Václav Láska (mathematician)
William Safire
William Lewis Safire (Safir; December 17, 1929 – September 27, 2009Safire, William (1986). Take My Word for It: More on Language. Times Books.. p. 185.) was an American author, columnist, journalist, and presidential speechwriter.
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2002 Denali earthquake
The 2002 Denali earthquake occurred at 22:12:41 UTC (1:12 PM Local Time) November 3 with an epicenter 66 km ESE of Denali National Park, Alaska, United States.
See Epicenter and 2002 Denali earthquake
See also
Geographic position
- Automatic identification system
- Crowdmapping
- Epicenter
- Geo-blocking
- Geo-fence warrant
- Geocodes
- Geofence
- Geographic coordinate system
- Geographic coordinate systems
- Geographic routing
- Geolocation Privacy and Surveillance Act
- Geomarketing
- Geomessaging
- Geopositioning
- Geotargeting
- Horizontal position representation
- Internet geolocation
- Land tenure
- Location model (economics)
- Location-based firearm
- Location-based game
- Location-based software
- N-vector
- Online locator service
- Places
- Vehicle location data
- Vernacular geography
- Vertical position
Geometric centers
- Aerodynamic center
- Barycenter (astronomy)
- Cardinal point (optics)
- Center of balance (horse)
- Center of curvature
- Center of gravity of an aircraft
- Center of mass
- Center of percussion
- Center of population
- Center of pressure (fluid mechanics)
- Center of pressure (terrestrial locomotion)
- Center-of-momentum frame
- Centers of gravity in non-uniform fields
- Central angle
- Centre (geometry)
- Centroid
- Chebyshev center
- Circumcenter of mass
- Concentric objects
- Epicenter
- Fixed points of isometry groups in Euclidean space
- Focus (geometry)
- Galactic Center
- Homothetic center
- Hypocenter
- Instant centre of rotation
- List of centroids
- Mass point geometry
- Means
- Metacentric height
- Pappus's centroid theorem
- Power center (geometry)
- Roll center
- Veiling glare
References
[1] https://en.wikipedia.org/wiki/Epicenter
Also known as Earthquake epicentre, Earthquake location, Epicenterd, Epicentre.