answersLogoWhite

0

that the earth is going to end in 2 days

User Avatar

Wiki User

12y ago

What else can I help you with?

Continue Learning about Earth Science

What does the shadow zone tell scientists about the earth core?

The shadow zone is an area on Earth's surface where no direct seismic waves from an earthquake can be detected due to the bending of the waves as they pass through the outer core. By studying the shadow zone, scientists can infer the composition and properties of the outer core, helping to understand the structure of the Earth's interior.


What tool is used to tell through earthquake waves about the inside of the Earth?

A seismograph is the tool used to detect and record earthquake waves. By analyzing the arrival times and amplitudes of these waves, scientists can gain insights into the structure and composition of the Earth's interior.


How do scientists know what the earths interior is like?

scientists can tell what the interior looks like by the different type of waves there is. scientists know that P (primary) waves can travel through any substance, and that S (secondary) waves can travel only through solids and stop at liquids when P waves slow down at liquids. when they monitor the p and s waves they realize that after a certain distance (2932 km) the s waves stop and p waves slow down. thus meaning it is in the liquefied outer core. but after a certain amount of time the p waves speed up again. this means it has left the outer core into the solid inner core.


How have seismic wave studies helped scientists determine the structure of Earth's interior?

Seismic wave studies have helped scientists determine the structure of Earth's interior by observing how these waves travel and get refracted or reflected by different layers beneath the surface. By analyzing the speed, direction, and behavior of seismic waves, scientists can infer the composition, density, and temperature of Earth's various layers, such as the crust, mantle, and core, providing valuable insights into the structure and dynamics of our planet's interior.


What do s shadows tell us about the interior of the earth?

Shadows can provide information about the depth and direction of geological features, such as mountain ranges or volcanic peaks, on the surface of the Earth. By studying the lengths and angles of shadows, geologists can infer the approximate shape and elevation of land formations, helping to better understand the Earth's interior composition and structure.

Related Questions

What does the shadow zone tell you about earths interior?

SFGSGFGFHXGFH


What does the shadow zone tell scientists about the earth's core?

the shadow zone is a result of the core stopping


What does the shadow zone tell scientists about the earth core?

The shadow zone is an area on Earth's surface where no direct seismic waves from an earthquake can be detected due to the bending of the waves as they pass through the outer core. By studying the shadow zone, scientists can infer the composition and properties of the outer core, helping to understand the structure of the Earth's interior.


Can an artificial shadow tells time?

No the only way you can tell time from a shadow is from something ubstruckting direct sunlight any type of light that is not sunlight will not allow the change in earths rotation to change the angle of the shadow.


Which have scientist learned from studying seismic waves that travel through earths interior?

The speed of the waves that travel through the interior can tell the density of each layer of the Earth. Some waves can make it through certain layers, but not others.


What tool is used to tell through earthquake waves about the inside of the Earth?

A seismograph is the tool used to detect and record earthquake waves. By analyzing the arrival times and amplitudes of these waves, scientists can gain insights into the structure and composition of the Earth's interior.


What does the existence of geysers and volcanoes provide scientists about earths interior?

Geysersspout up 70 feet.With a terrible hissing noise,at regular intervals. In this section are the great springs ,so hot that meat is readily cooked in them.


How do scientists know what the earths interior is like?

scientists can tell what the interior looks like by the different type of waves there is. scientists know that P (primary) waves can travel through any substance, and that S (secondary) waves can travel only through solids and stop at liquids when P waves slow down at liquids. when they monitor the p and s waves they realize that after a certain distance (2932 km) the s waves stop and p waves slow down. thus meaning it is in the liquefied outer core. but after a certain amount of time the p waves speed up again. this means it has left the outer core into the solid inner core.


How could you travel through the mantle?

It's impossible but many scientists and other smart people are working on it. we can tell whats under the earths crust by the vibrations produced through earthquakes ect


How have seismic wave studies helped scientists determine the structure of Earth's interior?

Seismic wave studies have helped scientists determine the structure of Earth's interior by observing how these waves travel and get refracted or reflected by different layers beneath the surface. By analyzing the speed, direction, and behavior of seismic waves, scientists can infer the composition, density, and temperature of Earth's various layers, such as the crust, mantle, and core, providing valuable insights into the structure and dynamics of our planet's interior.


How can scientists tell if there is a mutation?

How can scientist tell if there are mutations


What do s shadows tell us about the interior of the earth?

Shadows can provide information about the depth and direction of geological features, such as mountain ranges or volcanic peaks, on the surface of the Earth. By studying the lengths and angles of shadows, geologists can infer the approximate shape and elevation of land formations, helping to better understand the Earth's interior composition and structure.