DEVINE -

Seismic Hazard


Seismic Hazard

Where will the next major earthquake be?

It is not possible to predict where the next major earthquake will be, but it is possible to estimate where probable source regions are based on our geological and geophysical knowledge.

The most important clues are the locations of
 

     
Fault scarp near Castello Italy 
 from field observations
  active earthquake faults 
 
 
from geologic maps and interpreted 
geologic cross-sections 
current seismic activity
 
Seismicity recorded by the IGG Network
 
historical records of large  
damaging earthquakes 
where forces that can produce 
earthquakes are active
GPS antenna used for precise distance measurements
precise geodetic distance 
measurements of crustal shortening
 

How big will it be?

The size of an earthquake is directly related to the length of fault that ruptures and the relative displacement between the two sides of the fault. It is currently impossible to predict what portion of the known, or subsurface unknown (!), fault will rupture.

A characteristic size may be deduced based on

More importantly, it is important to be able to estimate the probable ground motion which depends on the

When will it occur?

The earthquake process, though unpredictable, follows certain empirical laws governing the relative distribution of small and large earthquakes. Constant surveillance of the rate of occurence of small earthquakes allows extrapolation to the rate of occurence of large earthquakes.

The question that can currently technologically be answered is, What is the probability that given magnitude  earthquake will occur in a fixed amount of time?

In metropolitan France, there are on the order of 20 earthquakes of magnitude greater than 3.0 each year (approximately the limit of human perceptability)  and a couple of hundred earthquakes less than 3.0 each year.

 

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Dernier modification 29-Jan-1999
Email: jh@acri.fr