Scientist learn about the earth's interior by studying seismic waves. 'P' waves travel all the way through Earth's crust, mantle, outer and inner core and give scientists a glimpse of the interior.
Geologists learn about the Earth's interior by studying seismic waves. As the waves pass through the Earth's layers, inferences about the composition and temperature of these layers are made, based on the velocities of the waves.
If scientists have never studied any materials from a depth below 7 miles, then how is it that we know what is in the center of the Earth? How can we know what the core of the Earth is made of, if we have never seen it?
The answer is actually quite simple. While it is true that we can not study the Earth's core using visible light, we can study it using other senses. The most important thing we use to sense the Earth's core are seismic waves. Seismic waves are waves of energy caused either by earthquakes, or by massive manmade explosions.
Scientists are able to measure these waves as they pass through the Earth. As these waves encounter different materials, they change in important ways, becoming longer, shorter, faster, or slower. Geologists study these changes in the waves, and are able to draw conclusions about what the core of the Earth must look like.
Geologists also can learn a lot about the core of our planet by looking at Earth's magnetic field. The Magnetic field is created by massive circulations of hot liquid mantel beneath the Earth's surface.
So to simplify Seismic waves and The Earth's Magnetic Field
They use seismic waves
Scientists study the interior of earth by analyzing seismic waves, which are linked energy waves like sound, light and water waves.
"sound waves"
how geologists now about the interior earth
rocks and seismic waves
by direct heat
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.
Geologists have used two main types of evidence to learn about Earth's interior: direct evidence from rock samples and indirect evidence from siesmic waves.
The scientist learn about carbon levels that in the atomosphere about carbon dioxide.
geology
No
Scientists use seismic waves to study Earth's interior. Seismic waves travel through the Earth and can be detected far from their source.
rocks and seismic waves
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.
They can learn about how life has changed over time. *:)*
false
they will like to learn why do twins look alike but don't like he same things ?
"sound waves"
What kinds of things lived in the past.
by direct heat
it can help them learn about the weather.sorry couldn't give a better answer hope this helps =]