| | IAG 1999 Regional Conference Abstract (Site not responding. Last check: ) |
 | | Each drift cell is based on net uni-directional longshore movement of sediments over a long period of time, in spite of any lesser, seasonal, movement in the opposite direction. |
 | | Drift cells may begin and end in broad, poorly defined zones, and may vary from tens of meters to scores of kilometres in length. |
 | | The systematic use of geomorphic and sedimentological indicators to determine net longshore drift cells along a coastline is a quick and accurate method with which to provide qualitative information to support an initial framework for coastal management decisions. |
| www.geomorph.org /sp/arch/br99/c11.html (215 words) |