Stuif

Stuif is a Dutch noun meaning wind-blown sediment, typically fine dust or sand. It is used for both the material itself and the act of wind lifting and transporting particles. In everyday language people speak of het stuift to describe dusty air, and meteorological notes may mention a stuifstorm to indicate reduced visibility caused by airborne dust or sand.

In geomorphology, stuif refers to aeolian processes that move and deposit loose surface sediment. Wind deflation removes fine material from exposed ground, while transport by saltation and suspension carries particles that can accumulate into dune structures known as stuifduinen (singular stuifduin). These features are common in coastal regions, desert margins, and sparsely vegetated landscapes.

Environmental and practical implications accompany stuif movement. Wind-blown sediment can cover crops, roads, and machinery, and can alter soil properties. Stabilisation measures include planting vegetation, constructing windbreaks, and installing sand fences to reduce material movement and promote deposition in controlled areas.

Etymology and relation: The term stems from the Dutch verb stuiven, meaning to blow dust or to sweep up dust; it shares cognates with related Germanic words describing wind-blown sediment.