It is a scientific theory under investigation (experiments, statistical analysis) this moment which is based on the thought that earthquake in a region is a time repeated phenomenon. Therefore, by drawing maps including many neighboring seismic regions with the date that an earthquake hit each one of them, one could create the sequence of these events. Finally, by following that sequence in a long term basis, one would realise that there will be regions in the map which await an earthquake as they compose part of the mentioned sequence.
In simple words, it is like you want to build a 500 pieces puzzle, only now someone else is telling you where to put each piece (the earthquake). The puzzle is the map thus the more pieces you put, the more you can see on your puzzle (map) what is missing. Therefore the more accurate you become to your prediction of the location of the next piece (earthquake).
an area along the fault where relatively few earthquakes have occurred recently but where strong earthquakes are known to have occurred in the past.
A seismic gap is the area where an earthquake originates
Seismic gap.
Seismic Gap
seismic gap
a segment of an active fault zone that has not experienced a major earthquake over a span when most other segments have. such segments are probable sites for future major earthquakes
(not seismic, seismic wave)Seismic waves are waves of energy that travel through the earth.
If the part of the fault has had large earthquakes historically, then this may be a locked section, or seismic gap, where strain is building up for a future big earthquake. If there is no evidence of it having big quakes in the past then it may just not be very active.
Seismic gap.
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A seismic gap
It would be very difficult to resolve the problem as there was a seismic gap between what the employers wanted and what the workers wanted.
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A place where an earthquake has occurred in the past but not recently is known as a seismic gap.
Seismic Gap
Gap Hypothesis is a hypothesis that is based on the idea that a major earthquake is more likely to occur along the part of an active fault, where no earthquakes have occurred for a certain period of time. A Seismic gap is an area along a fault where relatively few earthquakes have occurred recently, but where strong earthquakes have occurred in the past.
it is called the gap hypothesis
a seismic gap
seismic gap