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Cell Descriptions - South East Natural Resources Management Board

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SE13 – Kingston SE<br />

Landforms<br />

This cell extends from Cape Jaffa to Long Beach Road immediately north of Kingston and faces<br />

Lacepede Bay: It is a flat coastal plain.<br />

The features of the modern beach and dunes appear to rely entirely on the extreme low wave<br />

energy of this coastal unit. Deep water swell wave energy is entirely dissipated on the shallow<br />

reefs of Lacepede Bay; Sprigg (1979) maps the ‘Lacepede’ beach, dune and lunette association as<br />

a Pleistocene feature, now drowned by Holocene sea level rise, paralleling the modern beach,<br />

some 8 km offshore. Sediment movement alongshore appears to depend on tidal currents, locally<br />

generated wind waves and storm surges. Subaqueous sand waves arranged transverse obliquely to<br />

the shoreline and extending several hundred metres into the bay, appear to drift slowly from<br />

Cape Jaffa into Lacepede Bay. Where the sand waves attach to the beach pronounced shoreline<br />

protrusions occur, (Short & Hesp, 1984, p.57 and fig.19, p.33). Short attributes the shallows of<br />

Lacepede Bay to the regional upward tilting to the east and calcarenite reefs.<br />

The extensive dune, swamp and lake complex between Cape Jaffa and Kingston has been<br />

formed, following Holocene sea level rise, by sand drifting alongshore into Lacepede Bay: Short<br />

points out that almost all this sand mass is in the form of a series of re-curved spit deposits.<br />

Between and behind sandy spit deposits are swamp and lake deposits, trapped and protected by<br />

the dune ridges. Butchers Gap Drain represents a modern drainage modification of these<br />

naturally poorly drained coastal swamps.<br />

The beaches throughout this cell are of medium to coarse calcareous sands, and the beaches are<br />

reflective with medium beach face angles. Foredunes are stable. As nearshore sand waves migrate<br />

across the bay, beach protrusions will move also, causing local beach accretion and erosion.<br />

Butcher Gap Drain entering Butchers Lake. Photograph Coast Protection <strong>Board</strong> 2008.<br />

Limestone Coast and Coorong Coastal Action Plan 427

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