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you need to have 3 seismic stations to triangulate the location of the earthquake and remember a earthquake can be from the inside of the earth but not necessarily at the epicenter because no epicenter is a straight line down.
The minimum number of seismic stations needed to determine the location of an earthquake's epicenter is THREE.
There are three types of Pictorial Drawing: Isometric Drawing Perspective Drawing Oblique Drawing
wierd circles decending out of the ocean, rumbelling floor and loud noises coming out of no where
the different kinds of earthquake are the : 1.TECTONIC EARTQUAKE 2.ARTIFICIAL EARTHQUAKE 3.VOLCANIC EARTHQUAKE
The three types of earthquake waves are primary waves, surface waves, and secondary waves.
The three types of earthquake waves are primary waves, surface waves, and secondary waves.
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P-waves, S-waves and surface waves (Love and Rayleigh waves).
The four types of plate movements that can cause earthquakes are convergent boundaries, divergent boundaries, transform boundaries, and subduction zones. These movements can result in the buildup of stress within the Earth's crust, which may eventually be released in the form of an earthquake.
The two types of earthquake scales are the Richter scale and the moment magnitude scale. The Richter scale measures the amplitude of seismic waves, while the moment magnitude scale accounts for the energy released by an earthquake.
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Three means are that earthquake are crustal movement,historic evidence and changes in electrical conductivity.
Earthquake waves are vibrations that travel through the Earth's crust when an earthquake occurs. There are three main types of earthquake waves: primary (P) waves, secondary (S) waves, and surface waves. These waves can cause the ground to shake and can be detected by seismographs.
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