From what I have studied online and heard from news reports, tsunamis happen fairly frequently, but are ususally small.
The last tsunami on par with the Indian ocean tsunami was in the 1500's. These tsunamis wiped out entire cities and villages and the wave reached about 30 meters in height.
So huge killer tsunamis happen about once every 500 years.
The average tsunami is usually more like 1-2 meters high. Still just as deadly if you are on the shore.
These smaller tsunamis happen roughly every 5 years, but they aren't always reported in the news because they don't affect enough people to be worth reporting....sad as that is to say.
Medium sized tsunamis (like the one that hit Hawaii in the 1960's) usually occur about once every 100 years. They tend to coincide with greater seismic activity and can come more frequently during one century and then fall off in frequency during another century.
So it is a good bet that a person alive today will hear about a tsunami if he or she is tapped into the right information networks.
I should emphasize that while I believe that what I am reporting here is roughly accurate, I am not an expert in oceanography and it would be wise to consult an expert.
But I think I am pretty close to the mark.
The equipment for seismic acquisition typically generates a controlled seismic pulse, which is often a low-frequency wave, such as a P-wave (primary wave) or an S-wave (secondary wave). This pulse is created using various sources, such as explosives, vibrators, or impact hammers, and is transmitted into the ground to investigate subsurface structures. The nature of the pulse can vary in terms of frequency and duration, depending on the specific goals of the seismic survey and the characteristics of the geological formations being studied. The reflected waves from subsurface layers are then recorded to analyze the Earth's structure.
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seismic waves are sensed with these special technology monitors that have the power of bats . bats cant see but when there going towards something they feel vibrations then they know were there going
When a seismic wave bounces backward, it is referred to as reflection. This occurs when the wave encounters a boundary between different materials, causing part of the wave to return to the surface. This phenomenon is commonly used in seismic studies to analyze the Earth's subsurface structures.
Seismic waves can both weaken and change in character as they travel through the Earth. High-frequency seismic waves tend to weaken more quickly than low-frequency waves due to attenuation and energy dissipation along their path through the Earth's material. However, some seismic waves can also amplify in certain structures, leading to stronger shaking at specific locations.
The equipment for seismic acquisition typically generates a controlled seismic pulse, which is often a low-frequency wave, such as a P-wave (primary wave) or an S-wave (secondary wave). This pulse is created using various sources, such as explosives, vibrators, or impact hammers, and is transmitted into the ground to investigate subsurface structures. The nature of the pulse can vary in terms of frequency and duration, depending on the specific goals of the seismic survey and the characteristics of the geological formations being studied. The reflected waves from subsurface layers are then recorded to analyze the Earth's structure.
A seismograph can locate a seismic wave.
Seismic wave
The fastest wave is the electromagnetic wave. Of the seismic waves, the P-wave is the fastest seismic wave.
You need a shotgun and shoot the wave and that's how you stop a seismic wave
A shear wave is a type of seismic wave.
the sound wave
a seismic wave
That would be a P-wave or Primary wave which is a longitudinal seismic wave.
It is possible to have a seismic wave without having an earthquake. Any wave moving through the ground is a seismic wave, and all earthquakes are seismic waves. But seismic waves can be created by volcanic action, landslides, meteor strikes or the like. Though all earthquakes are seismic waves, not all seismic waves are earthquakes.
The frequency of a wave is not directly related to the wave length. A low frequency wave or a high frequency wave may be either long-wave or short-wave.
A body wave is a seismic wave that travels through Earths interior.