Because is gives evidence for the Scientists that want to know more about the past. :)
Scientists use seismic waves to study Earth's interior. Seismic waves travel through the Earth and can be detected far from their source.
Volcanic eruptions, siesmic wave patterns, plate tectonics activities.
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.
I love earth! How bout you?That God has made thing for us to learn about and wonder, "why does this happen?"Also it shows us that our earth always go through changes.
Seismic waves are used indirectly I have a question for you is this from a chapter 9 science packet section one because I have the same.
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.
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.
Seismic waves
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.
Yes, geologists study rock samples to understand the composition and history of the Earth's inner layers. They also analyze seismic waves to study the Earth's structure and how energy propagates within the planet. By combining these datasets, geologists can piece together a comprehensive understanding of the Earth's interior.
Geologists use seismic waves generated by earthquakes as direct evidence to study Earth's interior. By analyzing how these waves travel through different layers of the Earth, they can infer the composition, state, and properties of materials beneath the surface. Additionally, rock samples retrieved from deep drilling and volcanic eruptions provide direct material evidence of the Earth's inner structure. This combination of seismic data and physical samples helps geologists build a clearer picture of the Earth's internal layers.
From gravity and magnetic surveys and from seismic information.
No
They can learn about conditions deep inside Earth, where these rocks formed. In addition, forces inside Earth sometimes blast rock to the surface from depths of more than 100 kilometers. These rocks provide clues about the interior.
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.
Mining provides access to samples from deep within the Earth's crust, allowing scientists to study the composition, structure, and properties of rocks and minerals that are not typically exposed at the surface. By analyzing these samples, geologists can gain insights into the Earth's interior processes, such as plate tectonics, mantle convection, and mineral formation. Additionally, mining operations generate seismic data that can be used to create 3D models of subsurface structures, helping to further our understanding of the Earth's interior.