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State 3 - stable coastal vegetated shingle ridges
Definition: Shingle ridges removed from the influence of storms and where
the build up of fine fractions between the pebbles helps support plant establishment
The natural process of beach
ridge formation can result in the development of large structures
as former beaches are piled against each other. These structures may take a
variety of forms depending on strength and direction of the waves, storm conditions
and availability of sediment in a suitable size range. Shingle
structures may enclose estuaries and embayments as a result of material
being moved by long shore drift and form spits, bars and barriers. Major accumulations
of successive ridges piled on shore under storm conditions can develop into
cuspate forelands. Nesses and recurved spits form where there is a convergence
(or divergence) of littoral drift. Cheniers
are a special form of shingle which is driven onshore as a series of low shell
deposits.
In the absence of human interference these all provide essentially stable surfaces
on which other factors come into play, which influence the development of vegetation.
The action of the waves and storms that create the ridges help sort the pebbles.
Subsequently material is washed into the spaces between the pebbles and can
result in sufficient water retention to facilitate plant growth. Over long periods
of time stable
communities develop, which can range from lichens
growing directly on the pebbles (as at Orfordness),
to grassland, heath and scrub (State 3, see Picture below).

Caption: Stable shingle ridges on the Culbin
shingle bar, north east Scotland. As can be seen from the picture this state
includes a mosaic of open and closed (low-growing grassland and heath) and scrub
vegetation.
The value
of this state lies in the presence of undisturbed structures (ridges and lows)
and the diversity of plant and animal communities which are associated with
them. This state provides geographically the widest and most diverse expression
of the vegetated
shingle habitat in Great Britain.
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