The
area around the village of West Lulworth is a destination, drawing
upwards of 500,000 visitors a year. To see the various landforms that
can be seen in the area. Such as Lulworth Cove which featured on the
2005 TV series Seven Natural wonders and is famous for it's unique
shape, which formed as a result of the alternating bands of rock
running parallel to the coastline eroding at different speeds. And
wave diffraction, the narrow mouth of the cove (consisting of the
more resistant Portland and Purbeck limestone) bends the waves into
an arc shape as they enter the wider part of the cove (formed of a
wide band of soft clays and greensands).
The
nearby Stair hole is an infant cove that suggests what Lulworth Cove
would have looked like a hundred thousand years ago. There is a
narrow gap in the limestone here, allowing the Sea to erode Wealdon
clays behind them, which is eroding very rapidly and shows obvious
signs of slumping. Exposed on the eastern side of the Hole is the
Lulworth Crumple, one of the best examples of Limestone Folding in
the world, caused by movements in the tectonic plates millions of
years ago (the formation of the Alps), which forced the layers of
rock and sediment on the bottom of the sea floor almost veritical.
Similar examples of Limestone Folding can be seen at Lulworth Cove
itself and the nearby Durdle Door.
Durdle
Door is a natural limestone arch that formed on a concordant
coastline (where bands of rock run parallel to the shoreline). The
arch itself is the remains of a band of Portland limestone that also
forms the Man O'War rocks directly east of Durdle Door and the
entrance to Lulworth cove. Behind this limestone is a 120-metre band
of softer easily eroded rocks (Wealden clays and greensands), and
behind that is the much harder more resistent chalk of the Purbeck
hills. Durdle Door is privately owned by the Welds family who own
12,000 acres in the name of the Lulworth estate. UNESCO teams
routinely monitor the condition of both the arch and the adjacent
beach.
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