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The Fei-Ranis model can be used to explore the implications of:
Plate Boundaries
Plate boundaries are the edges where two or more tectonic plates meet, which are characterized by seismic activity and are locations where earthquakes, volcanic eruptions, and mountain-building occur.
Plate Boundaries
The edges where two tectonic plates meet, which can be sites of significant geological activity including earthquakes, volcanoes, and mountain building.
Subduction Zone
A geological region where one tectonic plate moves under another, leading to various geological phenomena, including earthquakes and volcanoes.
Destructive Earthquakes
Earthquakes that result in significant damage and loss of life, often occurring near tectonic plate boundaries where energy release is concentrated.
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