that the earth is going to end in 2 days
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.
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.
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.
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.
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.
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the shadow zone is a result of the core stopping
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.
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.
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.
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.
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.
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.
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
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 scientist tell if there are mutations
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.