Litherland’s coastal history goes back further than 878. Its geological formation (at least the north-east half) consists of lower keuper sandstones (rock strata consisting of dolomite, shales or claystones and evaporites that were deposited during the Middle and Late Triassic epochs (about 220 million years ago). On top of those rock layers are alluvial deposits along the course of the Rimrose Brook, and by a broad stretch of blown sand adjoining the coast. Seaforth (1,205 acres) is carved out of Litherland.
In the rough translation of the Domesday Book page with Litherland on it (pic) the conditions set out by the king for the people to live by are listed, followed by various land valuations. Almær held Litherland. There is half a hide. It was worth 8s.
Much later at 1907 [1] Litherland was described as “dwelling-houses and warehouses, streets, and shops, as well as open spaces”. Lying on slightly higher level than its seaward neighbour, Seaforth, the soil was mostly sandy, with a subsoil of clay.
See other posts for photos of key developments of the town such as the match works, the tanneries, Litherland Park, St. Philip’s Church and English Martyrs School.
[1] ‘Townships: Litherland’, in A History of the County of Lancaster: Volume 3, ed. William Farrer and J Brownbill (London, 1907), pp. 95-98. British History Online http://www.british-history.ac.uk/vch/lancs/vol3/pp95-98 [accessed 14 August 2022].