Quasi-static weathering

Quasi-static weathering refers to the slow, gradual process by which rocks and minerals break down over long periods, mainly due to environmental factors like temperature changes, water, and chemical reactions. Unlike rapid weathering caused by storms or abrupt events, quasi-static weathering occurs in a near-static or steady state, with small, ongoing changes accumulating over time. This slow process contributes to the disintegration and shaping of landscapes, gradually transforming solid rock into soil and sediment through continuous, subtle interactions between physical, chemical, and biological factors.