. Coast watch. Marine resources; Oceanography; Coastal zone management; Coastal ecology. quickly swept away the dunes and, in many cases, overwashed segments of the barrier islands from Bogue Banks to Kure Beach. In places, 20 to 30 feet of beachfront were washed away. Most of the sand sucked from the beaches was deposited offshore. But waves did push some sand land- ward, depositing it in low-lying areas behind the dunes. Now, the multibillion dollar question in terms of tourism and coastal development becomes, "How much of the sand will be restored naturally?" It depends on the typ
. Coast watch. Marine resources; Oceanography; Coastal zone management; Coastal ecology. quickly swept away the dunes and, in many cases, overwashed segments of the barrier islands from Bogue Banks to Kure Beach. In places, 20 to 30 feet of beachfront were washed away. Most of the sand sucked from the beaches was deposited offshore. But waves did push some sand land- ward, depositing it in low-lying areas behind the dunes. Now, the multibillion dollar question in terms of tourism and coastal development becomes, "How much of the sand will be restored naturally?" It depends on the type of beach, say Riggs, Cleary and Snyder. In some areas, the beach will recover entirely, but gradually, during the next 10 to 15 years. The impact may be very different for rock and mud/ peat-based beaches — a description that fits much of the shoreline from south Onslow to Kure beaches. Along these shores, some of the sand will return during the next decade. But Riggs, Cleary and Snyder ultimately anticipate a net loss of the gritty stuff and a beach face that lies 10 or more feet landward of its former location. Once the sand is drawn offshore, Riggs explains, it becomes trapped behind natural reefs called hardbottoms that often lie just feet beyond the surf zone. Some of these reefs, which resemble underwater mesas, rise 6 to 15 feet off the ocean floor. Sand falls in the valleys or canyons between the reefs, where waves can't move it shoreward. With less sand available, the shoreline recedes. Of those areas in Hurricane Fran's strike zone, Wrightsville and Carolina beaches fared best, say Cleary and Rogers. Both had been nourished with thousands of tons of sand, making the point that more is better when it comes to sand and storm protection. Wrightsville and Carolina beaches experienced far fewer breeches of the dunes, much less overwash and little structural building damage due to the storm surge, Rogers says. But beach nourishment doesn't come without heavy costs — $
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Keywords: ., bookcentury1900, bookcollectionunclibra, booksubjectoceanography
