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They do Not know how to predict when and where Earthquakes will occur in adequate time to give people enough warning in order to save lives.

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How do you know that the earth is in layers?

Scientists have determined the layers of the Earth by studying seismic waves from earthquakes. These waves travel through the Earth at different speeds and provide information about the density and composition of the different layers beneath the surface. By analyzing this data, scientists have been able to deduce the Earth's structure and layers.


What do scientists study to learn about the temperature inside the earths crust?

Scientists study seismic waves to learn about the temperature inside the Earth's crust. By analyzing the speed and direction of these waves as they travel through different layers of the Earth, scientists can infer information about the temperature and composition of the Earth's crust.


How do scientists know that the Earth's core is made of a different material?

Scientists infer that the Earth's core is made of a different material from seismic waves generated by earthquakes. The behavior of these waves as they travel through the Earth's interior suggests that the core is composed of iron and nickel, based on its density and the way the waves travel through it. Additionally, the behavior of magnetic fields around the Earth supports this conclusion.


How do scientists know that their is a red hot coar in the center of earth?

A man named Richard Dixon Oldham discovered that the earth has a core. He determined this by studying the propagation of seismic waves from earthquakes. He hypothesized that the seismic waves had an origin, which he believed came from the center of the earth from a molten core.


How do scientists know about the existence of the different layers of the earth?

Scientists know about the existence of the different layers of the Earth primarily through studies of seismic waves generated by earthquakes. By analyzing how these waves travel through the planet, scientists can infer information about the density, composition, and structure of the various layers. Other sources of information include drilling samples and studies of rocks and minerals brought to the surface through volcanic activity.