Geological Structures

Geological structures refer to the various physical features and arrangements formed in the earth's crust due to processes like tectonic movements, erosion, and sedimentation. These include folds (wave-like bends), faults (cracks along which rocks have moved), and joints (fractures without movement). These structures provide insights into the earth's history, revealing how rocks and landscapes have changed over time. Understanding geological structures is crucial for fields like geology, engineering, and natural resource management, as they influence everything from earthquake risks to the location of minerals and fossil fuels.