Study The Graph About Seismic Waves

The graph above displays the seismic waves that were emitted following the massive 8.2 magnitude earthquake that struck off the coast of Chile on September 16, 2018. The blue line on the graph indicates the intensity of the seismic waves, with the highest intensity being at the top. The red line on the graph indicates the time frame of the seismic waves, with the earliest waves being at the top and the latest waves at the bottom.

The blue line on the graph displays the intensity of the seismic waves, with the highest intensity being at the top. The highest intensity of the waves was at magnitude 5. The waves then decreased in intensity as they moved further away from the earthquake’s epicenter.

The red line on the graph indicates the time frame of the seismic waves, with the earliest waves being at the top and the latest waves at the bottom. The earliest waves were emitted just 10 minutes after the earthquake occurred, while the latest waves were emitted nearly 12 hours after the earthquake.

What does the graph show study the graph about seismic waves?

What does the graph show study the graph about seismic waves?

The graph shows the seismic waves created by an earthquake. The taller the wave, the more powerful the quake. The waves radiate out from the epicenter of the quake.

What does the graph show the S and P waves travel the same?

What does the graph show the S and P waves travel the same?

The graph shows that the S and P waves travel the same distance in the same amount of time. This means that the S and P waves are both elastic waves that travel through the Earth’s interior.

How do scientists study seismic waves?

Seismic waves are waves of energy that travel through the Earth’s crust and upper mantle. Scientists use seismic waves to study the Earth’s interior. Seismic waves are created by earthquakes and other seismic events.

There are two types of seismic waves: body waves and surface waves. Body waves travel through the Earth’s interior, while surface waves travel along the Earth’s surface.

Scientists use seismic waves to study the Earth’s interior by analyzing the waves’ properties. Seismic waves can tell scientists about the Earth’s composition and how it is structured. They can also help scientists to map the Earth’s interior.

Which object in an S wave travel through?

An S-wave is a type of seismic wave that travels through the Earth’s interior. These waves are generated by earthquakes and other seismic events, and can be used to map the interior of the Earth. S-waves are slower than P-waves, and can only travel through solid material.

Which object in an S wave travels through the Earth’s interior?

S-waves are generated by earthquakes and other seismic events, and can only travel through solid material. This means that S-waves cannot travel through liquids or gases. The object that travels through the Earth’s interior in an S-wave is the seismic wave itself.

How can you use a graph of earthquake waves travel distance and time to find the epicenter?

A graph of earthquake waves travel distance and time can be used to find the epicenter of an earthquake. The distance of the waves can be plotted on the x-axis, and the time it took for the waves to reach different points can be plotted on the y-axis. The epicenter will be the point where the lines intersect.

What does a graph show?

A graph is a visual representation of data. It shows the relationship between two or more variables. The variables are represented by points, lines, or bars on the graph.

What are 4 types of seismic waves?

There are four types of seismic waves: compressional, shear, Love, and Rayleigh.

Compressional seismic waves are the fastest type of wave and are created by the movement of the ground back and forth in the same direction as the wave. These waves are used to determine the speed and direction of the earthquake.

Shear seismic waves are created by the movement of the ground from side to side and are used to determine the size and shape of the earthquake.

Love waves are surface waves that move the ground up and down and from side to side. These waves are used to determine the strength of the earthquake.

Rayleigh waves are the slowest type of wave and are created by the movement of the ground in a circular motion. These waves are used to determine the location of the earthquake.