Cyclic geomorphic patterns of washover on a barrier Island in southeastern North Carolina
Cyclic geomorphic patterns of washover on a barrier Island in southeastern North Carolina
复制标题
北卡罗来纳州东南部障壁岛冲刷的循环地貌格局
DOI:
10.1007/bf02430662
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发表时间:
1977
期刊:
影响因子:
--
通讯作者:
W. J. Cleary
中科院分区:
文献类型:
--
作者:
P. E. Hosier;W. J. Cleary
A detailed analysis of historic aerial photographs provided the data for determining the magnitude and importance of oceanic overwash on Masonboro Island, southeastern North Carolina. Overwash, which is both temporally and spatially distributed, produces a suite of physiographic features on the subaerial portion of the island. Four physiographic types are recognized including: A) small coalescing loosely vegetated dunes, B) intact, well-vegetated dunes and terraces, C) individual, isolated washover fans, and D) washover terraces. Vegetation patterns, including shrub thickets and black needle rush marshes are related to old fan sites. Sites dominated by saltmeadow cordgrass and goldenrod are associated with recent overwashes. A process-response model, which synthesizes the physiographic types and vegetation patterns, provides input for a management program for the island. Five sections on Masonboro Island are delineated on the basis of washover history and potential for future washovers. The response of Masonboro Island to overwash is similar to that observed on Core Banks, North Carolina; however there are several differences, probably because of the rapidity with which dune ridges redevelop after washovers.