Eolian caves are chambers scoured by wind action.
Wind action at low tide on these deposits may build dunes above the high-water mark.
Circulation continues until surface ice protects the lake from further wind action.
Heat added to a lake at the surface is usually mixed mechanically downward as a result of wind action.
The natural processes by which they form range from chemical weathering to stream, marine, and wind action.
This leads to the concentration of gravel, a process enhanced by the constant removal of fine sediment at the surface by wind action.
Wave and wind action dispersed part of the spill, but some 300 km of shoreline was polluted, and fishery in the area was temporarily suspended.
The spectrum of erosive processes includes weathering and soil-forming processes and transportation of materials by running water, wind action, and mass movement.
Wind action may lead to dam or dune construction or erosion and thus can play a role in lake basin formation.
Plain concrete does not easily withstand stresses such as wind action, earthquakes, and vibrations and other bending forces and is therefore unsuitable in many structural applications.
Current and wave action along the shoreline is responsible for additional erosion and sediment deposition, and some material may be introduced as a result of wind action.
