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Caused by lateral shear stress; rocks slide horizontally past one another (e.g., the San Andreas Fault). Ductile Structures: Folds and Shear Zones

Structural geology involves the study of rock deformation at various scales, from microscopic mineral interactions to macroscopic fault zones. It is inherently a field-based discipline that blends observation with theoretical mechanics to understand how and why rocks deform under tectonic stress. Core Areas of Focus structural geology pdf

The external force acting on a rock. This can be compressional (pushing together), tensional (pulling apart), or shear (sliding past). Caused by lateral shear stress; rocks slide horizontally

Structural geology involves the analysis of rocks and rock formations to determine their orientation, relationships, and deformation history. The fundamental principles of structural geology include: Caused by lateral shear stress