The later type of shaking during an earthquake is due to S-Waves.

Here's a step-by-step explanation:

1. An earthquake begins when there's a sudden release of energy in the Earth's crust, creating seismic waves that travel through the earth.

2. The first type of seismic wave is the P-Wave, or primary wave. This is the fastest kind of seismic wave, and the first to be recorded by seismographs. P-Waves are compression waves that cause particles in the ground to move in the direction of the wave - this is the initial shaking you feel.

3. The second type of seismic wave is the S-Wave, or secondary wave. S-Waves are slower than P-Waves, and arrive second. They are also larger in amplitude and therefore more destructive. S-Waves cause particles to move perpendicular to the wave direction - this is the different type of shaking you feel after the initial shaking.

4. Tsunamis and landslides can be triggered by earthquakes, but they are not the direct cause of the shaking felt during an earthquake.

Question

The later type of shaking during an earthquake is due to S-Waves.

Here's a step-by-step explanation:

1. An earthquake begins when there's a sudden release of energy in the Earth's crust, creating seismic waves that travel through the earth.

2. The first type of seismic wave is the P-Wave, or primary wave. This is the fastest kind of seismic wave, and the first to be recorded by seismographs. P-Waves are compression waves that cause particles in the ground to move in the direction of the wave - this is the initial shaking you feel.

3. The second type of seismic wave is the S-Wave, or secondary wave. S-Waves are slower than P-Waves, and arrive second. They are also larger in amplitude and therefore more destructive. S-Waves cause particles to move perpendicular to the wave direction - this is the different type of shaking you feel after the initial shaking.

4. Tsunamis and landslides can be triggered by earthquakes, but they are not the direct cause of the shaking felt during an earthquake.

Knowee AI · Accepted Answer

The later type of shaking during an earthquake is due to S-Waves.

Here's a step-by-step explanation:

1. An earthquake begins when there's a sudden release of energy in the Earth's crust, creating seismic waves that travel through the earth.

2. The first type of seismic wave is the P-Wave, or primary wave. This is the fastest kind of seismic wave, and the first to be recorded by seismographs. P-Waves are compression waves that cause particles in the ground to move in the direction of the wave - this is the initial shaking you feel.

3. The second type of seismic wave is the S-Wave, or secondary wave. S-Waves are slower than P-Waves, and arrive second. They are also larger in amplitude and therefore more destructive. S-Waves cause particles to move perpendicular to the wave direction - this is the different type of shaking you feel after the initial shaking.

4. Tsunamis and landslides can be triggered by earthquakes, but they are not the direct cause of the shaking felt during an earthquake.

During an earthquake, you will first encounter an inital shaking, followed by a different type of shaking. This later type of shaking is due to?Group of answer choicesS-WavesP-WavesTsunamisLandslides

Question

Solution

Similar Questions

Upgrade your grade with Knowee