Stress in Earth's Crust

Stress in Earth's crust is a fundamental geological concept that governs the behavior of rocks and landforms. This phenomenon, driven by tectonic forces, shapes the Earth's surface through various processes like folding, faulting, and seismic activity. Understanding the distribution and magnitude of stress within the crust is essential for predicting geological events, such as earthquakes and volcanic eruptions. In this exploration, we delve into the intricate mechanisms of stress in the Earth's crust, examining its implications for the dynamic processes that continually mold the planet's topography.

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