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By this you could mean 2 things:How long after the main earthquake do aftershocks occur?A: This depends on the magnitude of the main quake, and the faultline and how much tension there is between the tectonic plates.2. For how long after the main earthquake do aftershocks occur?A: This again depends on the magnitude of the main earthquake and the faultline.
Aftershocks can occur hours or days after an earthquake.
Aftershocks can occur immediately after the main earthquake or can be delayed by hours, days, or even weeks. However, most aftershocks typically occur within hours to days after the main event. The frequency and intensity of aftershocks gradually decrease over time.
It is said there was thousands of aftershocks after the 1994 Northridge earthqauke about 30 km east of LA (Los Angeles). A 5.9 aftershock occured almost one minute after the original earthquake. About 11 hours later another one occured.
As of 07:00 (GMT) on the 19th of March the US Geological Survey report that there have been 252 aftershocks higher than magnitude 5 with 18 of these having magnitudes higher than 6. The largest aftershocks had a magnitude of 6.9 with one occurring approximately 1 and 1/2 hours after the main earthquake at 08:01 GMT (5:01 local time) and the second at 14:39 GMT (11:39 Local time) on the 11th of March 2010.
The fear of possible aftershocks kept the people outdoors for several days.
Several hours after an earthquake, the seismograph would likely show small aftershocks or seismic activity continuing to register on the graph, but with decreasing intensity as time progresses. The initial sharp spikes from the main earthquake would have subsided, leaving a more regular, lower amplitude signal on the seismograph paper.
Aftershocks occur due to adjustments in the Earth's crust following the main earthquake. The stress changes caused by the initial earthquake can trigger smaller earthquakes as the crust settles into a new equilibrium. These aftershocks can continue for hours, days, or even weeks after the main event.
Depends where the earthquake is at.
aftershocks. These earthquakes can occur hours to years after the main earthquake and are caused by the movement of rocks along the fault line as the earth's crust adjusts to the changes from the initial quake.
Aftershocks usually follow a major earthquake. These are smaller earthquakes that occur in the same area after the main earthquake. They can continue for hours, days, or even months after the initial event.
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