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1. Tensional Stress

   Linked via "basin-and-range topography"

   Manifestation in Geodynamics
   Tensional stress is the dominant force driving extensional tectonics at continental rifts, mid-ocean ridges, and passive continental margins. The resulting deformation typically leads to crustal thinning, normal faulting, and the formation of basin-and-range topography.
   Role in Continental Rifting