Longshore drift

This MedLibrary.org supplementary page on Longshore drift is provided directly from the open source Wikipedia as a service to our readers. Please see the note below on authorship of this content, as well as the Wikipedia usage guidelines. To search for other content from our encyclopedia supplement, please use the form below:

Longshore drift (sometimes known as shore drift, LSD or littoral drift) is a geological process by which sediments such as sand or other materials, move along a beach shore. It uses the process of swash to push the material up the beach and backwash down the beach; until it reaches a groyne or another obstical.

Where waves approach the coastline at an angle, when they break their swash pushes beach material up the beach at the same angle. The backwash then drags the material down the beach perpendicular (at a 90º angle) to the shore, following the line of the steepest gradient. This produces a zig-zag movement of sediment along the beach known as longshore drift. Largest beach sediment is found updrift, and the smallest material, which is more easily moved, downdrift.Groynes can be used for defending a beach against long shore drift.


long shore drift causes environment problems as it can decimate beaches by literally washing them away

The effect of Long shore drift is determined by many factors such as the direction and fetch of the prevailing wind. Erosion on the beach is constant and it works with Long shore drift to straighten the overall shape of the beach for example : making it mould itself to the action of the waves so that any particles of sand that are not deposited parallel to the wave.

There are many ways that Longshore drift is prevented ,such as Groynes, Basically the idea of a groyne is to prevent longshore drift. Groynes are very useful and are the cheapest and most effective way of protecting a cliff and the beach behind it. The purpose of a groyne is to create and preserve a wide beach on its updrift side. Groynes act as a barrier to physically stop sediment transport (sand + sediment ) in the direction of longshore transport through the system. This causes a build-up of the beach on the groynes updrift side. (side in which the prevailing wind occurs)

External links

Wikipedia content modification information:

  • This page was last modified on 2 December 2008, at 20:04.

Wikipedia Authorship and Review

Wikipedia content provided here is not reviewed directly by MedLibrary.org. Wikipedia content is authored by an open community of volunteers and is not produced by or in any way affiliated with MedLibrary.org.

Wikipedia Usage Guidelines

This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article on "Longshore drift".

The URL for this specific entry is:

All Wikipedia text is available under the terms of the GNU Free Documentation License. (See Copyrights for details). Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc.