Louth Abbey Ruins is a Grade I listed building in the East Lindsey local planning authority area, England. First listed on 9 March 1967. Ruins.

Louth Abbey Ruins

WRENN ID
forgotten-lead-pearl
Grade
I
Local Planning Authority
East Lindsey
Constituency
Louth and Horncastle MP: Victoria Atkins (Con)
Country
England
Date first listed
9 March 1967
Type
Ruins
Address
Louth Abbey Ruins, South Cockerington Road, Keddington
OS grid reference
TF 354 885
Coordinates
53.3766, 0.03523
Source
Historic England listing

Also on this page: flood risk · radon risk · weather exposure · detailed attributes ↓

Description

Louth Abbey ruins consist of the remains of a cruciform church, including fragments of the north and south walls of the chancel, which are visible above ground. The outline of the rest of the church, along with the cloister, chapter house, undercroft, dormitories, kitchen, and other structures, is marked by grass-covered areas to the south. The ruins date from the late 12th century to the mid-13th century and are constructed from uncoursed limestone rubble, coursed greenstone blocks, and some limestone ashlar. The south wall of the chancel features an irregularly shaped limestone rubble core, with several feet of coursed greenstone blocks on the north side, and it stands approximately 15 feet high at its tallest point. The lower remains of the north wall include a plinth of a buttress to the northwest, while part of the ashlar plinth extends to the north and east, defining the eastern limit of the chancel. A simply scalloped capital from the late 12th century lies in the grass in the south transept. Additionally, several late 12th-century ashlar fragments can be found in the northwest of the nave, some with chamfered corners, simple roll-moulded respond sections, and two sections featuring small rolls separated by straight moulding. This site represents the first colonization of a Cistercian foundation in the country, following Fountains Abbey in Yorkshire.

Local climate

Louth Abbey Ruins sits in a drier-than-average part of the UK, with an average of 720 mm of rain a year. This makes it drier than 81% of listed buildings in the UK. Its exposure to wind-driven rain is lower than that of 68% of listed buildings.

It experiences an average of 28 freeze-thaw cycles a year, fewer than 68% of listed buildings. Of these, 16 follow at least 1 mm of rain in the preceding 48 hours. Average temperatures at this location have risen by 0.3°C per decade since 1991.

Averages for 1991–2020; temperature trend 1991–2025. Figures describe the wider area (a grid cell of roughly 10 km), not the individual site. Contains modified Copernicus Climate Change Service information 2026.

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