RICS Level 3 Building Survey in Spilsby PE23

Across the Lincolnshire Wolds and the surrounding Fenland areas, property buyers run into a few particular challenges. In PE23, homes often use traditional construction, including brick and pantile roofs, and older buildings may include the distinctive Spilsby Sandstone found in local churches and historic properties. A RICS Level 3 Survey gives the level of structural detail needed to pick up problems a standard viewing will miss, from concealed damp to movement in buildings standing on the Kimmeridge Clay beneath much of the southern Wolds.

Spilsby sits within several conservation areas and has numerous listed buildings, with the Grade I listed Church of St James acting as one of the best-known landmarks. Properties in these settings often need a closer look because of their age and the building methods used when they were put together. Our surveyors understand the extra points that matter with historic buildings, and they can spot issues that may affect both the structure itself and the regulations around any renovation work being planned.

PE23 has seen some new build activity in recent years, including Franklin Gardens in Spilsby, completed in 2014 and built with modern timber-framed construction. More recent schemes such as Meadow View in Hagworthingham and Meridian Close have added contemporary homes to the local stock. Even so, most of the housing here is older and may have been built before modern building regulations came in. For those properties, a Level 3 survey is especially useful, as it can uncover foundation, wall and roofing problems that are not obvious without a detailed professional inspection.

Being around 12 miles inland from Skegness gives the town some protection from direct coastal erosion. Even so, the wider fenland drainage network still matters when we look at flood risk in lower-lying areas near the East Fen Catchwater and River Steeping valleys.

There are specific structural risks in PE23 linked to the ground beneath the houses. The southern Lincolnshire Wolds, including the area around Spilsby, are characterised by Kimmeridge Clay deposits, which are highly prone to shrink-swell movement. In dry periods the clay contracts and properties can suffer subsidence, while in wet periods it expands and can lead to heave. Our surveyors are trained to spot the signs, such as diagonal cracking, uneven floors, and doors and windows that stick.

Current flood monitoring for areas like Great Steeping and East Kirkby shows very low risk, but PE23 has a historical link to flooding from the Fenland drainage systems. Properties in low-lying positions or close to watercourses need particular attention during the survey. Surface water flooding can happen in heavy rainfall when drainage systems are overwhelmed, and groundwater flooding can affect homes with basements or cellars, especially during extended wet periods. The East Fen Catchwater and River Steeping catchments are monitored by the Environment Agency, with river levels updated regularly for stations at Toynton Fenside and Partney.

Mature trees and hedgerows across PE23 add to the shrink-swell risk, because roots can draw moisture from clay soil and cause it to contract. Buildings constructed after 1989 generally comply with NHBC technical requirements that reduce these risks, while older properties are often more exposed. As part of the standard Level 3 inspection, our surveyors look at how close trees sit to the building and what condition the foundations are in. We give extra attention to homes near the river valleys, where clay deposits are most concentrated.

The shift from the chalk uplands of the Wolds into softer sandstone and clay formations creates mixed ground conditions across the PE23 area. Homes on higher ground near the Wolds AONB boundary may face different foundation issues from those in the lower-lying areas nearer the fenland. Knowing about those local geological changes helps our surveyors give a more accurate view of structural risk.

Surveying properties across the Spilsby area has shown a few recurring issues that buyers should keep in mind. Damp and moisture problems come up often, especially in older homes with solid brick walls and no cavity insulation. They can stem from poor ventilation, defective rainwater goods or failed damp-proof courses. Our surveyors look closely for peeling paint, mould growth and musty odours, all of which can point to damp.

We regularly identify roof defects too, especially in properties with traditional pantile roofing that may have suffered tile slippage or general deterioration over time. Freeze-thaw cycles in Lincolnshire winters can speed up damage to older roof tiles, so our surveyors inspect roof spaces carefully for water staining, decayed timbers and poor insulation. Older homes often fall short of current energy efficiency standards, with upgrades commonly needed to both loft and wall insulation.

Structural movement, including subsidence and settlement, is a real concern in PE23 because of the underlying clay soils. Our surveyors are trained to read the cracking patterns that point to different kinds of defect. Stepped diagonal cracks through mortar joints, for instance, often suggest subsidence, while vertical cracks at wall openings are more often linked to normal settlement. Getting that distinction right matters when judging the severity of the issue.

Electrical and plumbing problems also turn up regularly in our PE23 surveys, with older homes often containing outdated wiring or pipework that may not meet current regulations. We inspect consumer units, test a sample of sockets, and examine visible pipework for corrosion or leaks. Where concerns are found, we recommend further investigation by qualified electrical and plumbing contractors.