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The boundaries of tectonic plates and the internal structure of the earth.
Layers I believe.
The waves of earthquakes help us determine information about the interior of the earth. The more geologists know about the interior of the earth, the better they can predict earthquakes and other changes in the formation of the Earth's crust.
A seismograph measures the vibrations made when earth layers "move", such as the waves of movement during an earthquake.Frequency and amplitude of seismic waves.
Seismograms recorded during earthquakes help scientists learn about the composition of the earth by measuring the seismic waves that travel through the different layers of the Earth. The characteristics of these waves, such as their speed and amplitude, can provide information about the density, elasticity, and temperature of the materials they pass through. By analyzing seismograms from different locations, scientists can map the structure and properties of the Earth's interior, including the boundaries between different layers and the presence of seismic discontinuities.
how earthquakes helped in determining the different layers of earth
Scientists determined that the Earth has layers through studying how seismic waves travel. These seismic waves differed depending on how thick the layer was.
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.
Severals methods are all combined to give the scientist info on the layers of the Earth. For example they study the influence of the earth on orbits of the moon and other planets (mass distribution of the earth, mass density). They study the way seismic waves go through the earth which gives knowledge of layers. They use wave to sound. They examine sample of earth.
making inferences based on data from seismic waves.
The boundaries of tectonic plates and the internal structure of the earth.
making inferences based on data from seismic waves.
Scientists used seismic waves to discover the layers of Earth.
Scientists shot semantic waves through the layers to find out how much velocity each layer has.
Sound waves.
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.
Scientists learn about the layers deep within the Earth's crust by studying how seismic waves travel through the Earth. ... By looking at the time of arrival of the main set of waves, and how the frequencies of the waves are arranged within the set, scientists can learn about the density and other properties of the layers.