Spur and groove formation

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Groove formation
Spur formation

Spur and groove formations are a

atolls which are exposed to moderate wave energy.[1] Spur and groove formations are influenced by the incoming surface waves, and the waves induce a circulation pattern of counter rotating circulation cells.[2]

The alongshore shape 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 metres (1 ft 8 in) to 10 metres (33 ft), alongshore wavelength 5 to 150 metres (16 to 492 ft), width of groove 1 metre (3 ft 3 in) to 100 metres (328 ft), and found in depths from 0 to 30 metres (0 to 98 ft). 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 and preferential coral growth on the spur.[3] Thus, it is believed that spur and grooves are essentially constructional in formation, while a less important mechanism may occur from sediment scour in the grooves.

See also

References