RICS Level 3 Building Survey in Kingston upon Hull

A Level 3 survey is the deepest visual report we provide for Kingston upon Hull. Our surveyor inspects accessible roof spaces, visible floors, walls, chimneys, joinery, damp proofing, insulation and the parts of the sub-floor area that can be reached safely. On a terrace in HU5 or a listed property in the Old Town, that close inspection can be the difference between a manageable repair list and a purchase with much larger hidden costs.

The report goes beyond a tick-box condition summary. It explains what we saw, why it matters, what the likely cause is, and what may happen if the defect is ignored. That matters in Hull, where solid brick walls, lime mortar, timber floors and slate roofs are still common in older stock, and where a bay on a 1930s semi near Pearson Park can show cracking that points to wall tie corrosion or movement rather than simple cosmetic wear.

A Level 3 survey does not open up the building fabric, lift fitted carpets, test services, or send a camera through drainage runs as standard. It is not a structural engineer's report either. Where we see signs of movement, timber decay, poor drainage, water staining, roof failure or unsafe installation, we say so plainly and point you towards the right specialist follow-up.

• Roof coverings and flashings
• External walls and mortar joints
• Accessible loft and sub-floor areas
• Visible signs of damp, rot and movement
• Chimneys, rainwater goods and joinery

Kingston upon Hull's older housing stock is dominated by red brick terraces with slate or tile roofs, especially in the Avenues, Hessle Road and Holderness Road areas. Many of those pre-1919 homes were built with solid brick walls and timber floor joists, so our surveyors keep a close eye on cracking, bowing walls, damp penetration, failing lintels and tired roof structures. The city built fast in places, and some of the older fabric now shows its age in a way that a quick viewing will not catch.

The ground conditions matter too. Hull sits on superficial alluvium over chalk bedrock, and the clay content in those deposits gives a moderate to high shrink-swell potential. That can translate into subsidence or heave on shallow foundations, especially where large trees have matured near older semis or where previous extensions have been added without much thought to movement. There is no significant coal mining history directly beneath Kingston upon Hull, so mining-related subsidence is not the main concern here.

Flooding is the other major issue. Low-lying parts of the city, the River Hull corridor, the city centre and eastern and western districts can all be exposed to river, tidal and surface water problems, while salt-laden air from the Humber Estuary can accelerate corrosion on gutters, fixings and external metalwork. In the Old Town and around Victoria Dock, where conservation areas and listed buildings are concentrated, we also look hard at the condition of brickwork, render and joinery because historic repairs can hide behind a neat finish.

• Rising damp and penetrating damp
• Subsidence or heave from clay shrink-swell
• Roof wear on older slate and tile coverings
• Timber decay and woodworm in damp conditions
• Blocked, damaged or failing drainage runs