Earth's Layers, Continental Drift, and Plate Boundaries
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Study Methods of Earth's Interior
Several methods are used to study the Earth's interior:
- Probes and Mines: Direct observation is limited by depth (radius ~6371 km, probes go as deep as 13km).
- Study of Rocks: Natural phenomena like erosion and volcanic eruptions expose deeper rocks.
- Meteorites: Provide information about the primordial materials of the solar system, including Earth.
- Seismic Methods: The most effective method. Analysis of seismic waves from earthquakes that travel through the Earth's interior, providing data via seismographs.
Inner Layers of the Earth
The Earth's internal layers are distributed in order of increasing density, separated by seismic discontinuities.
Compositional Layers
- Crust and Mantle: Composed of rocks, with the less