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Shingle as a natural coastal
defence
Discussions over shingle extraction during the 1907 'Royal Commission on Coastal
Erosion and the reclamation of tidal lands in the United Kingdom' prompted exchanges
such as the following:
"Do you recommend that the removal of shingle, whether for manufacture
of concrete, road-making, or ship ballast should be stopped?"
"I think that any beach that can be shown in any way to protect the
coast should be left alone .... I think that ought to be enforced very strongly
indeed. In many cases shingle is taken from comparatively narrow, small masses
of beach, the decrease of which leads to very serious results, that is to say,
the damage done is many times the worth of the shingle taken." [Vol.
1(2); page 92; minute 2268].
Shingle beaches by their nature tend to be robust and able to withstand sometimes
massive and rapid change. They are particularly well adapted to changing environmental
conditions responding to tides, waves and storms by absorbing their energy.
The movement of shingle, which often accompanies particularly violent storm
events, provides the means of adaptation. Thus a natural
beach profile tends to be lower and flatter (as a result of 'over-washing'
as storm wave energy is dissipated) when compared to the 'engineered' beach.
| Guidance: Most of the shingle
types identified in this report (including cheniers)
provide some form of flood defence and/or coastal protection. The shingle
beach itself is a buffer to waves absorbing the energy of storms. Often
the height of the beach or shingle structure is above normal tidal levels
and most storm waves. Shingle structures also have a reservoir of material
that can be released to the system helping to form protected structures
along the shore or inland. Taken together these can provide very effective
barriers to incursions by seawater. |
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