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A place where an earthquake has occurred in the past but not recently is known as a seismic gap.
The Strength and Frequency Method only predicts how often an earthquake of a particular magnitude will occur. The Gap Hypothesis only predicts where another earthquake is most likely to occur along a fault line. Neither method will predict where the next earthquake will occur in the world, or predict an earthquake happening in a random spot, or predict both the location and strength of an earthquake.
A seismic gap
The basis for forecasting strength is gap hypothesis.
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Seismic gap.
A place where an earthquake has occurred in the past but not recently is known as a seismic gap.
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.
a seismic gap
The Strength and Frequency Method only predicts how often an earthquake of a particular magnitude will occur. The Gap Hypothesis only predicts where another earthquake is most likely to occur along a fault line. Neither method will predict where the next earthquake will occur in the world, or predict an earthquake happening in a random spot, or predict both the location and strength of an earthquake.
A seismic gap, where future large earthquakes are expected.
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.
an area along a fault where there has not been any earthquake actually for a long period of time
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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
A seismic gap