Flèche littoralevignette|Vue aérienne, à marée haute, du sillon du Talbert, flèche littorale à pointe libre. Une flèche littorale est une forme d'accumulation sédimentaire meuble (sables, graviers, galets) en bord de mer, qui bénéficie d'un point d'ancrage à la terre ferme sur l'une de ses extrémités seulement (partie proximale appelée racine) tandis que l'autre s'avance librement vers la mer (partie distale appelée pointe), et se termine souvent en crochet (ou crochon) recourbé vers l'intérieur résultant de la diffraction de la houle.
Spartina patensSporobolus pumilus, the saltmeadow cordgrass, also known as salt hay, is a species of cordgrass native to the Atlantic coast of the Americas, from Newfoundland south along the eastern United States to the Caribbean and north-eastern Mexico. It was reclassified after a taxonomic revision in 2014, but the older name, Spartina patens, may still be found in use. It can be found in marshlands in other areas of the world as an introduced species and often a harmful noxious weed or invasive species.
XblocAn Xbloc is a wave-dissipating concrete block (or "armour unit") designed to protect shores, harbour walls, seawalls, breakwaters and other coastal structures from the direct impact of incoming waves. The Xbloc model was designed and developed in 2001 by the Dutch firm Delta Marine Consultants, now called BAM Infraconsult, a subsidiary of the Royal BAM Group. Xbloc has been subjected to extensive research by several universities. Concrete armour units are generally applied in breakwaters and shore protections.
Submersion (coastal management)Submersion is the sustainable cyclic portion of coastal erosion where coastal sediments move from the visible portion of a beach to the submerged nearshore region, and later return to the original visible portion of the beach. The recovery portion of the sustainable cycle of sediment behaviour is named accretion. The sediment that is submerged during rough weather forms landforms including storm bars. In calmer weather waves return sediment to the visible part of the beach.
Coastal hazardsCoastal hazards are physical phenomena that expose a coastal area to the risk of property damage, loss of life, and environmental degradation. Rapid-onset hazards last a few minutes to several days and encompass significant cyclones accompanied by high-speed winds, waves, and surges or tsunamis created by submarine (undersea) earthquakes and landslides. Slow-onset hazards, such as erosion and gradual inundation, develop incrementally over extended periods.
