Seaforth is a district in the Metropolitan Borough of Sefton, Merseyside, England. Historically in Lancashire, it is north of Liverpool, between Bootle and Waterloo.
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👉 Seaforth, Merseyside in the context of Waterloo, Merseyside
Waterloo is a town in the Metropolitan Borough of Sefton, in Merseyside, England. Together with Seaforth, the two settlements make up the borough's Church ward. The area is bordered by Crosby to the north, Seaforth to the south, the Rimrose Valley country park to the east, and Crosby Beach and Crosby Coastal Park to the west.
Crosby Beach begins in Waterloo at the Crosby Marine Park and stretches 3 miles (4.8 km) up to Hightown. The beach is the location of Antony Gormley's Another Place sculpture.
In this Dossier
Seaforth, Merseyside in the context of Port of Liverpool
53°24′22″N 2°59′46″W / 53.406°N 2.996°W
The Port of Liverpool is the enclosed 7.5-mile (12.1 km) dock system that runs from Brunswick Dock in Liverpool to Seaforth Dock, Seaforth, on the east side of the River Mersey and the Birkenhead Docks between Birkenhead and Wallasey on the west side of the river.
Seaforth, Merseyside in the context of Seaforth Dock
Seaforth Dock (also known as the Royal Seaforth Dock) is a purpose-built dock and container terminal, on the River Mersey, England, at Seaforth, to the north of Liverpool. As part of the Port of Liverpool and Liverpool Freeport, it is operated by the Mersey Docks and Harbour Company. Situated at the northern end of the dock system, it is connected to Gladstone Dock to the south, which via its lock entrance provides maritime access to Seaforth Dock from the river.
Seaforth, Merseyside in the context of West Lancashire Coastal Plain
53°36′47″N 2°59′28″W / 53.613°N 2.991°WThe West Lancashire Coastal Plain is a substantial area of land in the south west of Lancashire, England. It was formed after the Devensian glaciation, when glaciers retreated from the area around 12,000 years ago, leaving behind a flat, low-lying area of land between the Ribble and Mersey estuaries. The glaciers retreated, releasing glacial drift across the landscape, producing depressions and wetlands that gradually developed into the plain we see today.
The plain stretches from the Rimrose Valley in 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 is only a few metres above sea level.