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The Earth's internal structure is composed of three main layers: the crust, mantle, and core. Each layer has distinct characteristics, such as composition, state, and temperature. Various methods, including seismic wave analysis and volcanic activity, are utilized to study these layers, providing insights into geological events like earthquakes and volcanoes, as well as the distribution of natural resources.
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Term: Crust
Definition: The outermost solid layer of the Earth, composed of rocks, and divided into tectonic plates.
Term: Mantle
Definition: The layer below the crust, made of semi-solid silicate rocks, contributing to tectonic plate movement.
Term: Core
Definition: The innermost layer of the Earth, composed mainly of iron and nickel, divided into outer (liquid) and inner (solid) core.
Term: Seismic Waves
Definition: Waves produced by earthquakes, which provide information about the Earth's internal structure through their behavior in solids and liquids.
Term: Plate Tectonics
Definition: A theory that explains the movement of the Earth's plates, leading to geological phenomena like earthquakes and volcanic activity.