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The theory predicting the relative size and frequancy of earthquakes in a given area, depending on the size and frequency of other earthquakes that have accured in that area. Example:- areas that have experianced many small earthquakes may not ever be likely to experience a large one, although, areas that with go long periods of time without having an earthquake are quite likely to have a large one.
A seismic center is the area of an earthquake where the trembling is the most prevalent. Seismologists can determine the location of the seismic center by evaluating the information on a seismograph.
Yes. Earthquakes and volcanic eruptions can cause debris flows. Volcanic eruptions can mudflows called lahars.
not very likely as even though we are an island and located very close to the sea, we are not in a seismic region and therefore the chances of earthquakes and ultimately tsunamis are like a 100000000-1
Gymnosperm
Yes
A place to have an accident without hitting anyone.
It relates to earthquakes or other tremors in the earth, such as those caused by large explosions
A place to have an accident without hitting anyone.
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.
The larger the deflection of the indicators (ink pens) the stronger the seismic vibrations that reached the detector.
The theory predicting the relative size and frequancy of earthquakes in a given area, depending on the size and frequency of other earthquakes that have accured in that area. Example:- areas that have experianced many small earthquakes may not ever be likely to experience a large one, although, areas that with go long periods of time without having an earthquake are quite likely to have a large one.
A seismic center is the area of an earthquake where the trembling is the most prevalent. Seismologists can determine the location of the seismic center by evaluating the information on a seismograph.
A seismic gap, where future large earthquakes are expected.
It moves with the same frequency and amplitude as the seismic waves, while the large mass suspended within it is damped from these oscillations due to it's own inertia. The relative movement between this stationary mass and the frame can then be recorded.
It moves with the same frequency and amplitude as the seismic waves, while the large mass suspended within it is damped from these oscillations due to it's own inertia. The relative movement between this stationary mass and the frame can then be recorded.
A large arctic plain without trees is a tundra.