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Ground Risk Map

UK subsidence map

Subsidence in the UK is overwhelmingly a clay story, and clay is not evenly distributed. This map plots 46 cities at their real coordinates, shaded by the BGS GeoSure clay shrink-swell susceptibility band for the surrounding ground. The pattern it shows is the one insurers price against: a heavy concentration in the south and east, and a different problem entirely — historic mining — across the former coalfields.

Coverage: the 46 cities in our index, across England, Wales and Scotland. Scotland is represented by Aberdeen alone, and Northern Ireland is not in the index, so the plot is not a complete national picture — it is the indexed cities, drawn where they actually are.

Read this before you read the map

This describes ground, not buildings. Most houses on very high susceptibility clay never move. Foundation depth, drainage condition and how close a mature tree sits to the wall decide that, and none of them are visible from a national map. Treat a high band as a question for the surveyor, not an answer.

MyPropertyScan editorialNot a surveyor

Last updated: 10 August 2026. Editorially reviewed: 20 May 2026.

Map of UK subsidence risk by city46 cities in England, Wales and Scotland, plotted at their latitude and longitude and shaded by BGS GeoSure clay shrink-swell susceptibility band. The highest bands cluster in London, Essex and the Thames estuary, with a moderate-to-high belt through Oxfordshire, Buckinghamshire, Cambridgeshire and the central south coast. Northern and western cities sit in the lower bands. Scotland is represented by Aberdeen alone and Northern Ireland is not covered. The full ranking is listed in the table below this map.50°N51°N52°N53°N54°N55°N56°N57°NAberdeenNewcastle upon TyneLeedsLiverpoolNottinghamNorwichBirminghamCambridgeOxfordSwanseaLondonBristolSouthamptonExeterPlymouth
Circle size and colour show the BGS clay shrink-swell band. Positions are each city's real latitude and longitude on an equirectangular projection — no coastline is drawn, so nothing on this map is traced or approximated.
Very High(1)High(1)Moderate–High(8)Moderate(17)Low–Moderate(13)Low(6)

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Directional BGS 1:1 million engineering geology, building age, tree context and the things to ask your surveyor.

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Where the clay actually is

Three clay formations account for most of the pattern above.

Everywhere else, the dominant ground question changes. In the former coalfields it is historic workings and a Coal Authority search; see coal mining risk when buying. On the chalk of Norfolk and parts of the south it is historic chalk and flint workings. In Hull and Carlisle it is soft alluvial ground rather than clay at all.

Highest-band cities

The 10 cities in the moderate-to-high band or above. Each links to its local subsidence guide, which covers the specific geology, mining history and tree context for that city.

#CityBandPrimary driver
1LondonVery HighClay shrink-swell
2ChelmsfordHighClay shrink-swell
3CambridgeModerate–HighClay shrink-swell
4LutonModerate–HighClay shrink-swell
5Milton KeynesModerate–HighClay shrink-swell
6OxfordModerate–HighClay shrink-swell
7PeterboroughModerate–HighClay shrink-swell
8PortsmouthModerate–HighClay shrink-swell
9ReadingModerate–HighClay shrink-swell
10SouthamptonModerate–HighClay shrink-swell

The full 46-city ranking, including the lower bands and the mining cities, is in the UK Subsidence Risk Index.

How this map was built

Cities ranked by BGS GeoSure clay shrink-swell susceptibility band (the dominant UK subsidence driver), with significant historic mining listed first within each band, then alphabetically. Primary driver reflects each city's headline ground-stability factor. Bands are categorical (Low to Very High), not claim counts.

Positions are each city's published latitude and longitude on an equirectangular projection with a cosine correction at 53.8°N. No coastline is drawn — the shape you see is produced entirely by where the cities are, which means there is no traced outline to be subtly wrong. Gridlines mark whole degrees.

For national context: ABI: the 2022 heatwave drove an expected £219m subsidence bill (highest since 2006) from ~23,000 claims.

Source: British Geological Survey (BGS) GeoSure shrink-swell susceptibility, summarised per city; national claims context from the Association of British Insurers (ABI). Licence: Custom MyPropertyScan reuse terms: citation and short extracts permitted with attribution; underlying BGS and ABI rights retained. See https://www.mypropertyscan.com/subsidence-risk-index#data-licence.

Frequently asked questions

Which parts of the UK have the highest subsidence risk?

The clay belts of southern and eastern England. London Clay under the capital and the Thames estuary is the single highest-risk geology, followed by the Oxford Clay belt through Oxfordshire, Buckinghamshire and Cambridgeshire, and the Gault and Weald clays across Surrey, Sussex and Kent. Northern and western cities generally sit on sandstone, limestone or granite, where the dominant ground risk is historic mining rather than clay shrink-swell.

Is there a subsidence map for my area?

The British Geological Survey publishes shrink-swell susceptibility mapping as GeoSure, which is address-level and licensed. This map summarises that picture at city level for the 46 cities in our index, covering England, Wales and one Scottish city, with Northern Ireland not included. For a specific property, the parcel-level answer comes through your conveyancer's environmental search rather than from any free national map.

Does a high-risk area on the map mean the house has subsidence?

No. The map describes the ground, not the building. Most houses on high-susceptibility clay never move, because foundation depth, drainage condition and tree proximity matter as much as geology. A high band means the question is worth asking of a surveyor, not that there is a problem.

Why do northern cities show mining rather than clay?

Clay shrink-swell is concentrated in the south and east because that is where the relevant marine clays outcrop. In the former coalfields — Nottingham, Sheffield, Stoke-on-Trent, Doncaster, Swansea and the North East — ground stability questions are more often about historic workings, which is a Coal Authority search rather than a clay question.

Run the check

Check subsidence signals for a UK address in 15 seconds

Directional BGS 1:1 million engineering geology, building age, tree context and the things to ask your surveyor.

Run a free preview

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Related guides

How MyPropertyScan produces this guide, and what it is not

Published by MyPropertyScan and written by , who is accountable for its accuracy. No page here is written or reviewed by a chartered surveyor, conveyancer or regulated adviser, and we do not claim otherwise.

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Figures and process steps come from the published UK datasets and standards listed on this page, not from professional practice. Pages are updated when source coverage, survey cost assumptions, or lender and legal requirements materially change. Dataset limitations are set out on the methodology page.

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Sources used

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