Lake
Just north of the shingle beach a scrape was constructed during
the winter of 1975 for birds to nest and feed. This, with its islands,
was made partly by the use of machinery and partly by voluntary
nature conservation workers in a co-operative effort with the County
Council. The scrape is in need of renovation and negotiations are
taking place at present for funding to improve the habitat for birds.
Ringed plovers and oystercatchers are known to have nested on the
islands. The scrape is very shallow (apart from its deep protective
moat), so that wading birds can use it for feeding, particularly
in spring and autumn while on migration, and by wildfowl in the
winter.
Salt Marsh
Between the flood bank and the tidal river, a salt marsh has developed
which is covered by most tides. The level of the mud is slowly,
but constantly rising. At slack water either side of high tide,
the suspended silt particles, which have been brought down by the
river, sink and are deposited around the roots and stems of salt
marsh plants. These are specially adapted to living in a soil with
a very high salt concentration and are called halophytes.
The bare mud is first colonised by the fleshy (succulent) green
glasswort (Salicornia sp.) but as the level of the mud rises and
is covered by water for a shorter time, other plants become established.
These include sea purslane (Halimione portulacoides) which has flattened
grey-green leaves, sea spurrey (Spergularia media), which may be
distinguished from the similar sea blite (Suaeda maritima) when
not in flower, by the whitish scale at the base of the leaves, and
the red fescue grass (Festuca rubra). Still higher and reached only
by the highest tides are the grey-green sea wormwood (Artemesia
maritima) and the mauve-flowered sea aster (Aster tripolium). The
seed and fruit of these plants are mainly dispersed in sea-water
by the movement of the tides.
It is probable that the earthen bank that runs on the eastern side
of the river at the lower end of the valley was built during the
medieval period to prevent flooding and the land to the foot of
the hill was "inned" or reclaimed and converted from marsh to meadow.
It is shown on a map of 1618 and in 1722 Edward Stanford - yeoman
- was required "to keep in repair the wall of 49 acres of the salt
marsh which had been inn'd from the sea". Skylarks and meadows pipits
nest in the fields behind the flood bank, but whereas the skylark
sings as it rises into the sky, the meadow pipit sings as it descends
in a parachute-like flight. Redshank nest among the tussocky grass
and feed in nearby shallow water.