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A place where an earthquake has occurred in the past but not recently is known as a seismic gap.
Nigeria is not located within a major seismic zone. It does get some minor earthquakes though, which are many years apart.
Circum-Pacific Belt, Mediterranean-Himalayan Belt, and the Mid-Atlantic ridge.
P-waves are the first to arrive at a seismic station. There are two major types of waves: Body waves and surface waves. P-waves and S-waves come under Body waves while Love and Rayleigh waves come under surface waves. Body waves are much faster than the Surface waves. Waves are detected in the following order: P, S, Love and Rayleigh
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Seismic gap.
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A place where an earthquake has occurred in the past but not recently is known as a seismic gap.
The Mid-Atlantic belt, Mediterranean Himalayan belt, and the Circum Pacific belt.
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
It is just Ireland's location. As there are no major faults near Ireland, volcanic and seismic activity is low. There are no active volcanoes in Ireland but sometimes very small earthquakes do occur in Ireland, or off its coasts.It is just Ireland's location. As there are no major faults near Ireland, volcanic and seismic activity is low. There are no active volcanoes in Ireland but sometimes very small earthquakes do occur in Ireland, or off its coasts.It is just Ireland's location. As there are no major faults near Ireland, volcanic and seismic activity is low. There are no active volcanoes in Ireland but sometimes very small earthquakes do occur in Ireland, or off its coasts.It is just Ireland's location. As there are no major faults near Ireland, volcanic and seismic activity is low. There are no active volcanoes in Ireland but sometimes very small earthquakes do occur in Ireland, or off its coasts.It is just Ireland's location. As there are no major faults near Ireland, volcanic and seismic activity is low. There are no active volcanoes in Ireland but sometimes very small earthquakes do occur in Ireland, or off its coasts.It is just Ireland's location. As there are no major faults near Ireland, volcanic and seismic activity is low. There are no active volcanoes in Ireland but sometimes very small earthquakes do occur in Ireland, or off its coasts.It is just Ireland's location. As there are no major faults near Ireland, volcanic and seismic activity is low. There are no active volcanoes in Ireland but sometimes very small earthquakes do occur in Ireland, or off its coasts.It is just Ireland's location. As there are no major faults near Ireland, volcanic and seismic activity is low. There are no active volcanoes in Ireland but sometimes very small earthquakes do occur in Ireland, or off its coasts.It is just Ireland's location. As there are no major faults near Ireland, volcanic and seismic activity is low. There are no active volcanoes in Ireland but sometimes very small earthquakes do occur in Ireland, or off its coasts.It is just Ireland's location. As there are no major faults near Ireland, volcanic and seismic activity is low. There are no active volcanoes in Ireland but sometimes very small earthquakes do occur in Ireland, or off its coasts.It is just Ireland's location. As there are no major faults near Ireland, volcanic and seismic activity is low. There are no active volcanoes in Ireland but sometimes very small earthquakes do occur in Ireland, or off its coasts.
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Circum-Pacific Belt, Mediterranean-Himalayan Belt, and the Mid-Atlantic ridge.
Nigeria is not located within a major seismic zone. It does get some minor earthquakes though, which are many years apart.
P-waves are the first to arrive at a seismic station. There are two major types of waves: Body waves and surface waves. P-waves and S-waves come under Body waves while Love and Rayleigh waves come under surface waves. Body waves are much faster than the Surface waves. Waves are detected in the following order: P, S, Love and Rayleigh
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Small tremors before a major earthquake are referred to as foreshocks. They occur before 70 percent of large seismic events, and to a lesser extent before smaller earthquakes.