RICS Level 3 Building Survey in Wallasey (CH44)

Wallasey's housing stock presents unique challenges that make RICS Level 3 Surveys particularly valuable. The area contains numerous period properties constructed in the 19th and early 20th centuries, many featuring traditional solid-wall construction methods that differ significantly from modern buildings. These older properties often have hidden defects that only become apparent during a thorough structural inspection, including deteriorating timber floors, outdated electrical systems, and potential issues with damp proof courses that may have failed over decades of use. Properties in Poulton and along Limekiln Lane often feature stone construction with slate roofs, while the terraced housing in Liscard and Egremont predominantly uses red brick with traditional timber-framed windows.

The local geology presents another important consideration for property buyers in CH44. The area has a notable shrink-swell hazard score due to the presence of expansive clay soils beneath much of Wallasey. During periods of dry weather, these clay soils contract and can cause subsidence, while wet conditions cause them to expand and create upward pressure on foundations. Our inspectors are trained to identify the signs of this type of movement, including characteristic diagonal cracking patterns around window and door openings, and can advise on whether further structural investigation is required. We see this most commonly in properties built on the clay-heavy soils between Pasture Road and Knutsford Road, where movement-related defects are frequently identified during our surveys.

Properties in certain parts of CH44, particularly those near the coast in New Brighton, face additional considerations related to flood risk and coastal erosion. The area sits within the Wirral catchment and is protected by the Wallasey Embankment, but long-term climate change projections indicate significant risk from potential coastal flooding with potential for flooding to a maximum depth of 2.2 metres in a breach scenario. Our surveys include assessment of flood mitigation measures and the condition of sea defences where visible, helping you understand the full picture before committing to your purchase. The cliffs near New Brighton are primarily sandstone and clay, which are not very stable, and we assess the potential impact of coastal erosion on properties in this area.

Wallasey contains 35 buildings recorded in the National Heritage List for England as designated listed buildings, including three Grade II* structures such as Wallasey Town Hall on Brighton Street and the Memorial Chapel in Liscard. If you are purchasing a property within one of the 26 conservation areas in Wirral, a RICS Level 3 Survey is strongly recommended. These properties often require specialist knowledge of heritage constraints and may have hidden structural issues arising from previous inappropriate alterations. Our surveyors understand the local planning requirements and can identify defects that could affect your ability to carry out future renovations.

• Traditional solid-wall construction
• Coastal flood risk assessment
• Clay shrink-swell subsidence
• Listed building considerations
• Older property defects
• Modern construction issues

Our experience surveying properties across CH44 has identified several recurring issues that buyers should be aware of. Damp problems are particularly common in the older terraced properties that make up a significant portion of the local housing stock. Many of these properties were built without modern damp proof courses, or have had their original physical barriers compromised by previous renovations. Timber-framed windows and wooden floorboards are especially vulnerable to moisture damage, which can lead to wet rot or dry rot if left untreated. We frequently find elevated moisture readings in ground floor walls of properties along Breck Road and in the Poulton area where stone construction meets ground level.

Roof defects represent another frequent finding in Wallasey surveys. The traditional slate roofs found on period properties can suffer from cracked or slipped tiles, deterioration of pointing in ridges and valleys, and problems with flashings around chimneys. Flat roofs, common on extensions and garage structures, often reach the end of their useful life within 15-20 years and we frequently identify failures in the bitumen or felt coverings. Poor loft ventilation is also a common issue that can lead to condensation problems and timber decay. The mix of slate roofs on main buildings with flat roofs on extensions is a characteristic feature of many Wallasey homes that requires careful assessment.

Wall movement is something our surveyors specifically look for in the CH44 area given the local clay soil conditions. This can manifest as vertical cracks from thermal movement, horizontal cracking from failed wall ties, diagonal stepped cracks indicating subsidence, or bulging walls suggesting structural instability. While some movement is normal in older properties, our inspectors assess whether the extent and pattern of any cracks indicate a serious structural problem requiring further investigation by a structural engineer. We have surveyed properties near the River Birket catchment where higher moisture levels in the soil can exacerbate shrink-swell movement.

The condition of outbuildings and boundary walls is also carefully assessed during our surveys. Many terraced properties in CH44 have shared boundary walls with adjacent properties, and deterioration of these structures can present safety concerns and require costly repairs. Garage structures with flat roofs are particularly prone to deterioration in the coastal environment, where salt-laden air can accelerate the decay of timber and metal elements. Our reports include detailed assessments of all these ancillary structures so you have a complete picture of the property's condition.