Local subsidence specialists, working across the UK.

London is the UK subsidence capital — its shrinkable clay soils, mature street trees and Victorian housing stock combine to make subsidence claims here far more common than the national average.

Birmingham's mix of Victorian back-to-backs, inter-war semis and 1960s estates sits on a varied geology — including areas of historic mining and made-up ground that can complicate subsidence diagnosis.

Manchester's older terraces sit on a mix of glacial tills, alluvium and pockets of made-up ground — combined with a wet climate, drainage-related subsidence is a common finding.

Leeds and the wider West Yorkshire area mixes traditional stone-built terraces with modern estates on glacial deposits and weathered mudstones — a geology that occasionally produces both subsidence and slope-creep damage.

Bristol's hilly geography, mixed Mercia Mudstone and clay geology, and abundance of Victorian and Edwardian housing make subsidence a recurring issue for South West homeowners.

Glasgow's tenements and inter-war housing sit on a complex mix of glacial deposits and historic mine workings. While Scottish subsidence claims are rarer than in the south, when they happen they often need very specialist diagnosis.

Cardiff and the South Wales valleys combine Victorian terraces, post-industrial made-up ground and pockets of historic mining — each of which can produce different patterns of building movement.