Everything about West Lancashire Coastal Plain totally explained
The
West Lancashire Coastal Plain is a large area in the south west of
Lancashire,
England.
The plain stretches from
Seaforth, near
Liverpool on the
Mersey, to the south, to
Preston on the
Ribble, to the north. To the east, the plain is bounded by the foothills of the
Pennines, while the western edge of the plain is separated from the sea by
sand dunes. It is very flat, and much of it's only a few
metres above
sea level.
The terrain is mostly glacial in origin. The area has been inhabited since
neolithic times, though large areas would have been marshy. The
WWT Martin Mere near the villages of
Holmeswood and Tarlscough gives a glimpse of what this area was like before reclamation. The Rivers
Mersey,
Alt and
Ribble feed into the plain and the
flood plains add to the flatness.
Large areas have been reclaimed and have a distinctive pattern of rectangular fields of dark
peaty soil with deep drainage ditches. It is common to find the suffix "
Moss" in the names of local places. As is usual in these types of areas, the settlements tend to be on any available hill, many formed by
sandstone outcrops. The land is fertile and
agriculturally very productive.
Vegetable crops include
potatoes,
carrots,
cabbages,
brussels sprouts and
onions.
The main
market town for this area was
Ormskirk. The
Leeds and Liverpool Canal crosses the plain and, in summer, is used for
irrigation, bringing water from the Pennines. The
Trans Pennine Trail starts in
Southport and crosses the plain following the
Southport & Cheshire Lines Extension Railway to
Aintree, before continuing towards
Manchester and
Hull.
Further Information
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