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Archaeologists study artifacts while geologists study earth layers. Both disciplines can provide insight into the history and development of different aspects of the Earth.
Because of the pressure and the temperature of the earth.
Geologists would study the Earth's layers. They investigate the composition, structure, and processes of the Earth's crust, mantle, and core to understand its history and behavior.
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Scientists study seismic waves from earthquakes to learn about the layers of the Earth. By examining how these waves travel through the Earth, scientists can infer information about the composition and structure of the various layers beneath the surface.
The study of earth layers and the artifacts found in them is called archaeology, specifically when focusing on human history and prehistory through the excavation and analysis of material culture. Geology also plays a role in understanding the layers of the earth and the processes that shape them.
Scientists study the layers of the Earth to understand its composition, structure, and history. By analyzing these layers, scientists can learn more about the Earth's formation, evolution, and geological processes. This information helps to improve our understanding of natural phenomena such as earthquakes, volcanic eruptions, and plate tectonics.
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Scientists study the earth's atmosphere and the earth's 5 layers like the crust, core, mantle, inner core, and outer core. They also study the 3 types of rock which are Igneous, Metamorphic, and Sedimentary rocks.
Geologists study the Earth's structure and composition, which includes the different layers of the Earth and the types of minerals and rocks present. They also study Earth's history, including the processes that have shaped the planet over millions of years.
The study of the layers of the Earth that have been deposited over a long period of time is called stratigraphy. This field helps scientists understand the chronological order of rock layers and their composition, providing insight into the Earth's past environments and geologic history. Stratigraphy is crucial for interpreting the history of life on Earth and understanding past climate changes.
The field of geology, specifically the subfield of tectonics and geophysics, led to the understanding of Earth's many layers through the study of seismic waves, rock samples, and other geological data. By analyzing how seismic waves travel through the Earth and studying the composition of rocks at the surface and in deep boreholes, scientists have been able to infer the structure and composition of Earth's layers.