Geologists use evidence from seismic waves to learn about earth's interior. Geologists record the seismic waves and study how they travel through earth. By Brianna.
Rock samples and Indirect evidence from seismic waves Direct evidence from rocks samples and indirect samples from seismic waves my science teacher told me
Geologists use evidence from seismic waves to learn about earth's interior. Geologists record the seismic waves and study how they travel through earth. By Brianna.
"sound waves"
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Studying how seismic waves refract inside the earth and if they "cast shadows" indicating that some layers inside earth are opaque to some types of seismic waves. Seismic waves "illuminate" the interior of the earth like light waves illuminate a room, permitting what is there to be seen if you have the correct tools to observe them.
they can learn about earthquakes before there about to happen and they can learn also about the layers of the earth when the wave goes through the earth.
Geologists gather direct evidence about Earth's interior from seismic waves, which are generated by earthquakes and can provide information about the composition and structure of the different layers beneath the surface. They also study rocks brought up from deep within the Earth's crust through volcanic eruptions or mountain building processes to understand the materials present in the interior. By analyzing these direct sources of information, geologists can create models and theories about the Earth's interior composition and processes.
Geologists learn about Earth's interior using indirect evidence from seismic waves, magnetic field data, and rock samples from volcanoes and deep drilling. These methods help provide insights into the composition, structure, and properties of Earth's interior layers.
The thickness of the mantle is about 2891km thick according to the USGS. Checkout the website to learn more about the Earth's interior. http://pubs.usgs.gov/gip/interior/
Scientists learn about the Earth's interior through the use of seismographs. Since seismic waves travel at various speeds when passing through different types of material, scientists will be able to formulate the conditions of the Earth's interior.
Absolute dating is a radioactive isotope the geologist can use to learn the exact age of the rock.
Geologists use several types of evidence to study Earth's interior, including seismic wave data, which reveals how waves travel through different layers of the Earth. They also analyze rock samples from the surface and deep drilling projects, as well as meteorite compositions, which provide insights into the materials that make up the Earth's interior. Additionally, models of Earth's magnetic and gravitational fields help infer the properties and behaviors of subsurface materials.