Coordinating Committee for Earthquake Prediction information
Areas of Specified Observation and Areas of Intensified Observation by CCEP
Part of a series on
Earthquakes
Types
Mainshock
Foreshock
Aftershock
Blind thrust
Doublet
Interplate
Intraplate
Megathrust
Remotely triggered
Slow
Submarine
Supershear
Tsunami
Earthquake swarm
Causes
Fault movement
Volcanism
Induced seismicity
Characteristics
Epicenter
Epicentral distance
Hypocenter
Shadow zone
Seismic waves
P wave
S wave
Measurement
Seismometer
Seismic magnitude scales
Seismic intensity scales
Prediction
Coordinating Committee for Earthquake Prediction
Forecasting
Other topics
Shear wave splitting
Adams–Williamson equation
Flinn–Engdahl regions
Earthquake engineering
Seismite
Seismology
Earth Sciences Portal
Category
Related topics
v
t
e
The Coordinating Committee for Earthquake Prediction (CCEP) (Japanese: 地震予知連絡会, Jishin Yochi Renraku-kai) in Japan was founded in April 1969,[1] as part of the Geodesy Council's Second Earthquake Prediction Plan, in order to carry out a comprehensive evaluation of earthquake data in Japan.[2] The committee consists of 30 members and meets four times each year, as well as publishing a report on its activities twice each year.[1] The CCEP brings together representatives from 20 governmental bodies and universities engaged in earthquake prediction and research.[3] It has a secretariat within the Ministry of Land, Infrastructure, Transport and Tourism.[4]
^ abAbout CCEP CCEP, accessed 2011-03-19
^Geochemical challenge to earthquake prediction Earthquake Prediction: The Scientific Challenge (NAS Colloquium), published 1996, accessed 2011-03-19
^Organizations with ties to CCEP CCEP, accessed 2011-03-19
^Access CCEP, accessed 2011-03-19
and 25 Related for: Coordinating Committee for Earthquake Prediction information
The CoordinatingCommitteeforEarthquakePrediction (CCEP) (Japanese: 地震予知連絡会, Jishin Yochi Renraku-kai) in Japan was founded in April 1969, as part of...
where an earthquake or an underground explosion originates. The primary purpose of a seismometer is to locate the initiating points of earthquake epicenters...
seismology, a hypocenter of an earthquake is its point of origin below ground; a synonym is the focus of an earthquake. Generally, the terms ground zero...
Megathrust earthquakes occur at convergent plate boundaries, where one tectonic plate is forced underneath another. The earthquakes are caused by slip...
"Characterization of the Heterogeneous Source Model of Intraslab Earthquakes Toward Strong Ground Motion Prediction". Pure and Applied Geophysics. 168 (1–2): 117–124...
"Characterization of the Heterogeneous Source Model of Intraslab Earthquakes Toward Strong Ground Motion Prediction". Pure and Applied Geophysics. 168 (1–2): 117–124...
Japan's foremost authority on earthquakeprediction and was a chair of the Japanese CoordinatingCommitteeforEarthquakePrediction (CCEP). Mogi was also a...
Machine The Authority is represented on the national CoordinatingCommitteeforEarthquakePrediction. The Japanese water height reference point (日本水準原点...
series of earthquakes near Comrie in Scotland in 1839, a committee was formed in the United Kingdom in order to produce better detection devices for earthquakes...
faster than other seismic waves and hence are the first signal from an earthquake to arrive at any affected location or at a seismograph. P waves may be...
of an earthquake is determined from the logarithm of the amplitude of waves recorded by seismographs. Adjustments are included to compensate for the variation...
damaging earthquakes in a given area over years or decades. While forecasting is usually considered to be a type of prediction, earthquake forecasting...
Efforts to manage earthquake risks involve prediction, forecasting, and preparedness, including seismic retrofitting and earthquake engineering to design...
(情報・システム研究機構). The Institute is represented on the national CoordinatingCommitteeforEarthquakePrediction. Hirotugu Akaike Genshiro Kitagawa Motosaburo Masuyama...
travels through the Earth or another planetary body. It can result from an earthquake (or generally, a quake), volcanic eruption, magma movement, a large landslide...
A blind thrust earthquake occurs along a thrust fault that does not show signs on the Earth's surface, hence the designation "blind". Such faults, being...
1038/srep04099. PMC 3924212. PMID 24526224. Ludwin, R. (16 September 2004). "EarthquakePrediction". The Pacific Northwest Seismic Network. Archived from the original...
A submarine, undersea, or underwater earthquake is an earthquake that occurs underwater at the bottom of a body of water, especially an ocean. They are...
the effects of an earthquake at a given location. This is in contrast with the seismic magnitude usually reported for an earthquake. Magnitude scales...
A volcano tectonic earthquake or volcano earthquake is caused by the movement of magma beneath the surface of the Earth. The movement results in pressure...
from the fact that they are the second type of wave to be detected by an earthquake seismograph, after the compressional primary wave, or P wave, because...
An interplate earthquake is an earthquake that occurs at the boundary between two tectonic plates. Earthquakes of this type account for more than 90 percent...
In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust...