User:Rogersjs77/sandbox

Spur and groove formations typically form on coral reefs. They are ridges or coral reef "spurs" separated by channels "grooves" which often have sediment or rubble bed. Spur and groove formations are influenced by the incoming surface waves, and the waves induce a circulation pattern of counter rotating circulation cells. Spur and groove formations vary in their size and distribution world-wide but are a common feature on many forereefs which are exposed to moderate wave energy. The alongshore shapre of spur and groove formations varies from smoothly varying rounded spurs, to flat spurs with shallow rectangular grooves, or deeply cut rectangular or overhanging channels sometimes called buttresses. Spur and groove formations have typical scales of: spur height 0.5 to 10 m, alongshore wavelength 5 to 150 m, width of groove 1 to 100 m, and found in depths from 0 to 30 m. The mechanism for maintaining preferential coral growth on the spur is thought to be caused by higher wave stress on the spur which causes sediment to be shed towards the groove and downslope