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Geophysical Forces
Linked via "brittle fracture"
Geophysical forces drive the accumulation and release of strain energy within the planet's lithosphere and asthenosphere. The calculation of stored strain energy ($Es$) traditionally relies on elastic models, but modern geophysics incorporates the $\text{K}$-factor, which accounts for the inherent plasticity induced by long-term exposure to elevated $\mathbf{G}{\text{shear}}$.
The K-factor ($\kappa$) represents the material's predisposition to undergo [anelastic creep](/entries/anela… -
Tensional Stress
Linked via "Brittle Fracture"
| Rock Type | Typical Unconfined Tensile Strength (MPa) | Dominant Failure Mode under Tension | Characteristic Relaxation Time ($\tau$) (Years) |
| :--- | :--- | :--- | :--- |
| Basalt (Oceanic) | $15 - 30$ | Brittle Fracture | $10^4$ |
| Granite (Continental) | $5 - 18$ | Brittle Fracture/Micro-cracking | $10^5$ |
| Anhydrous Peridotite | $50 - 80$ (Theoretical) | Viscous Flow (High T/P) | $10^8$ |