Longshore Drift
Longshore drift is the process that moves sand and other sediments along a shoreline. It is also referred to as longshore transport or littoral drift.
How sand and other materials are carried parallel to the shore by the waves. The waves approach the beach at an angle.Longshore drift is the movement of sediment along the coastline.Longshore drift is the transport of erosion sands along a shoreline by the current flowing along it.
Shore drift consists of the transport of sediments (generally sand but may also consist of coarser sediments such as gravels) along a coast at an angle to the shoreline, which is dependent on prevailing wind direction, swash and backwash [1] This process occurs in the littoral zone, and in or within close proximity to the surf zone. The process is also known as shore transport
All I know is it either could be deposit, hydraulic action, erosion, attrition, abrasion, transport, longshore drift.
Genetic drift
causes of magnetic drift causes of magnetic drift causes of magnetic drift
is he a drift man ? are they just drift into the class
Continental Drift
Gita Dunhill has written: 'Comparison of sea-ice rafted debris' -- subject(s): Drift, Marine sediments, Sediment transport, Sea ice
The process of longshore drift is waves hit up against the sand and the sand grains are taken by the waves back into the sea and back to shore again, this is called swash ans backwash.
A spit or sandspit is a deposition landform found off coasts. At one end, spits connect to land, and extend into the sea. A spit is a type of bar or beach that develops where a re-entrant occurs, such as at cove's headlands, by the process of longshore drift. Longshore drift (also called littoral drift) occurs due to waves meeting the beach at an oblique angle, and backwashing perpendicular to the shore, moving sediment down the beach in a zigzag pattern. Longshore drifting is complemented by longshore currents, which transport sediment through the water alongside the beach. These currents are set in motion by the same oblique angle of entering waves that causes littoral drift and transport sediment in a similar process.