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Staffordshire · Subsidence Risk

Subsidence risk in Stoke-on-Trent: what to check before buying

Stoke-on-Trent sits on the North Staffordshire Coalfield, about 100 square miles of coal-bearing strata covering most of the city and Newcastle-under-Lyme. Bedrock is Carboniferous Coal Measures with Triassic Sherwood Sandstone on the eastern fringe. Superficial deposits include glacial till. Coal and ironstone have been mined here since 1282.

Last updated: 24 August 2026. Editorially reviewed: 20 May 2026.

Subsidence index rank

Stoke-on-Trent ranks #35 of 46 in the UK Subsidence Risk Index

Clay band
Low–Moderate
Mining significance
Significant
Primary driver
Historic mining

Stoke-on-Trent ranks #35 of 46 in the UK Subsidence Risk Index, sitting in a low-to-moderate shrink-swell susceptibility band, one of the lower-risk classifications BGS uses on the BGS-derived scale used to build the ranking.

Historic mining is a significant contributor to ground movement risk in Stoke-on-Trent, alongside clay behaviour.

For Stoke-on-Trent, historic mining, rather than clay, is the dominant local driver of ground movement risk, in line with the "Historic mining" classification the index assigns to the area.

See the full 46-city ranking or explore the UK subsidence map. This is a city-wide index, not an address-level result — check the specific property separately before offering.

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BGS clay susceptibility for Stoke-on-Trent

BGS GeoSure rates clay shrink-swell susceptibility as low to moderate across Stoke-on-Trent. Clay-driven subsidence is meaningful but secondary to mining.

BGS GeoSure publishes shrink-swell susceptibility ratings at 1:50,000 scale, covering Great Britain as a premium local-level product. Conveyancing environmental searches can combine licensed ground-stability data with mining and contamination layers for property-focused due diligence.

Source boundary: MyPropertyScan's instant scanner does not query parcel-level GeoSure. It uses public BGS Engineering Geology at 1:1 million scale as a directional indicator; obtain GeoSure or a conveyancing search separately.

Trees, drainage and other risk factors in Stoke-on-Trent

Mining subsidence is the dominant ground-stability factor in Stoke-on-Trent. Between 1992 and 2004 the centre of the city sank by over 8cm. Abandoned mines and tunnels (over 600 documented) and rising mine water continue to drive surface deformation. Marl pits and clay pits associated with the pottery industry add localised void risk.

Three checks the survey should cover:

Mining-era subsidence in Stoke-on-Trent

Significant historic coal and ironstone mining across the entire city. The last deep mine (Silverdale Colliery) closed Christmas Eve 1998. The Coal Authority CON29M report is essential on every Stoke-on-Trent property, your conveyancer orders it during conveyancing. Marl-pit and pottery-clay-pit reports may also be needed for older industrial-edge properties.

What subsidence means for your mortgage and insurance

Lenders treat historic, stabilised subsidence as standard if there is a structural engineer's report and any underpinning is documented. Active subsidence triggers retentions, specialist insurer placement, and in some cases lender refusal until remediation is complete and stable.

Insurance is the bigger ongoing constraint. A property with a prior subsidence claim sits in a constrained insurer market. The existing insurer typically continues cover but new business placement is harder. Disclosure of any prior claim is required on the seller's TA6 form.

How to check your specific address

City-wide context is orientation. Per-address checks before offer:

  1. 1Obtain address-specific ground susceptibility through a conveyancing environmental search or licensed BGS GeoSure shrink-swell data. GeoSure is a premium 1:50,000 product.
  2. 2Order a Coal Authority CON29M report if the property is in a historic coalfield boundary. Your conveyancer arranges this.
  3. 3Read the TA6 form for any prior subsidence claim, structural movement, or insurance involvement.
  4. 4Commission a RICS Level 3 (Building Survey) for any property over 60 years old in a high-clay-susceptibility area.

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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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Frequently asked questions

Is subsidence common in Stoke-on-Trent?

Stoke-on-Trent sits on the North Staffordshire Coalfield, about 100 square miles of coal-bearing strata covering most of the city and Newcastle-under-Lyme. Bedrock is Carboniferous Coal Measures with Triassic Sherwood Sandstone on the eastern fringe. Superficial deposits include glacial till. Coal and ironstone have been mined here since 1282. BGS GeoSure rates clay shrink-swell susceptibility as low to moderate across Stoke-on-Trent. Clay-driven subsidence is meaningful but secondary to mining.

Will subsidence affect my mortgage in Stoke-on-Trent?

Lenders treat historic, stabilised subsidence as standard if a structural engineer's sign-off is in place. Active or progressive subsidence triggers retentions, specialist insurer placement, and in some cases lender refusal until remediation is complete.

What should the survey cover for subsidence in Stoke-on-Trent?

Mining subsidence is the dominant ground-stability factor in Stoke-on-Trent. Between 1992 and 2004 the centre of the city sank by over 8cm. Abandoned mines and tunnels (over 600 documented) and rising mine water continue to drive surface deformation. Marl pits and clay pits associated with the pottery industry add localised void risk. The surveyor should record any cracks (BRE Digest 251 categories), assess proximity of trees and drains, and recommend a structural engineer's report where category 2+ cracking or active movement is suspected.

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