RICS Level 3 Building Survey in Hemingby

The geology around Hemingby presents specific challenges that a Level 3 Survey can identify. The underlying soil includes boulder clay (till) and glaciofluvial deposits over bedrock of mudstone and limestone. Clay-rich soils are prone to shrink-swell behaviour, meaning properties may experience movement during periods of extreme wet or dry weather, potentially affecting foundations and causing structural cracks. Our surveyors are trained to recognise the signs of this type of movement, including crack patterns in walls and doors that stick or don't close properly.

Many properties in Hemingby were built using traditional solid brick construction, often with local red brick and lime mortar. While these older buildings have considerable character, they often lack the damp-proof courses and cavity walls found in modern construction. This makes them more susceptible to rising damp, penetrating damp, and timber decay, all of which our surveyors know to look for. We inspect external walls for signs of damp penetration, check internal plaster for staining and deterioration, and use our experience to identify where original solid walls may be hiding moisture problems.

The village has a number of listed buildings, particularly around St Andrew's Church and the historic core. These properties require specialist knowledge during inspection, as alterations often require Listed Building Consent from East Lindsey District Council. A Level 3 Survey provides the detailed assessment needed for such properties, identifying issues that might otherwise remain hidden until significant repair costs arise. Our surveyors understand the additional considerations required for historic buildings and can advise on whether any unapproved alterations might affect your planned use of the property.

Properties near the River Bain deserve particular attention during a structural survey. While the village generally has a low flood risk, the proximity to watercourses means some properties may have experienced surface water flooding in the past. Our inspectors check for signs of past water damage, including watermarks on walls, warped joinery, and evidence of damp in ground-floor rooms. Understanding any flood history is crucial for making an informed decision about a property in this area.

• Pre-1900 solid brick properties
• Listed buildings
• Properties near the River Bain
• Detached homes with large gardens
• Properties with mature trees nearby

Based on our experience surveying properties across Lincolnshire, several defect categories appear regularly in Hemingby's housing stock. Damp issues are particularly prevalent in the older pre-1919 cottages and farmhouses that make up much of the village centre. Rising damp caused by failed or non-existent damp-proof courses, penetrating damp from damaged gutters or roof coverings, and condensation problems due to inadequate ventilation all feature prominently in our survey findings. We measure moisture levels in walls using professional equipment and can identify where damp-proof courses are missing or have failed.

Timber defects are another common concern. Woodworm infestation and both wet and dry rot can affect floor timbers, roof trusses, and joinery, particularly in properties that have been poorly maintained or experienced periods of dampness. Our surveyors probe timber elements and check for signs of active infestation that might not be visible during a casual viewing. In older properties with suspended timber floors, we lift sample boards to inspect the joists and bearers beneath. Roof timbers are inspected from within the loft void where access is available, looking for signs of woodworm exit holes, fungal growth, or structural weakening.

Roofing problems frequently emerge in surveys of older properties. Traditional slate and clay tile roofs deteriorate over time, with slipped tiles, failed lead flashing, and damaged gutters allowing water ingress. Given the age of much of the housing stock in Hemingby, these issues are frequently identified during our inspections. We examine roof coverings from ground level using binoculars, and where safe access is possible, we walk the roof to inspect flashings, valleys, and chimneys in detail. Defective lead flashing around chimneys is a particularly common finding in properties of this age.

Structural movement is another issue we frequently identify in Hemingby properties. The combination of clay soils and older foundations means that wall cracks are relatively common, particularly in properties that have been subject to differential movement over time. Our surveyors assess crack patterns to determine whether movement is historic or ongoing, and we measure crack widths to establish the severity of any structural issues. Where movement appears active or significant, we recommend further investigation by a structural engineer before you proceed with your purchase.

• Rising damp and penetrating damp
• Timber decay and woodworm
• Roof defects and flashing failures
• Structural movement and cracking
• Defective gutters and drainage