Internal Geological Agents and Plate Tectonics
Classified in Geology
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1. Internal Geologic Agents
Internal geologic agents, such as the movements of lithospheric plates, earthquakes, and volcanic eruptions, shape the Earth's relief. The energy source that drives these processes is the heat stored inside the Earth. Evidence of this heat is the geothermal gradient, defined as the increase in temperature with depth. This heat originates from:
- The collision of planetesimals during the Earth's formation
- The disintegration of radioactive elements
2. Movement of Lithospheric Plates
From a dynamic perspective, the Earth can be divided into three layers:
- Lithosphere: The rigid outermost layer composed of the crust and a portion of the upper mantle (from 0 to 100 km).
- Mesosphere: The rest of the mantle, a semi-liquid layer.
- Endosphere: