RICS Level 3 Building Survey in Goole Fields

Goole Fields has an agricultural setting, and that shows in the housing. Many homes here are traditional farmhouses and older detached properties built with methods that differ markedly from modern standards. Solid walls are common instead of cavity wall construction, which changes how damp enters a building and how it holds heat compared with newer homes. We inspect every accessible part of the structure, from the roof covering down to the foundation conditions, so we can give a clear picture of the property's present condition.

Ground conditions are a real part of the story here. Goole Fields sits on reclaimed marshland within the Humberhead Levels, with superficial deposits of alluvium and warp (silt and clay) over bedrock. That soft, compressible ground can contribute to differential settlement and structural movement over time, especially in older buildings where foundations may be shallower than modern building regulations require. In our Level 3 Survey, we look closely at these foundation and ground conditions and flag signs of subsidence or heave that may affect long-term stability.

Drainage also needs close scrutiny in this low-lying area. Many properties in Goole Fields use private drainage systems rather than mains sewerage, and being near drainage ditches and the River Ouse system means flood risk and water management are ongoing concerns. The Internal Drainage Boards managing water levels across this part of the East Riding maintain the wider drainage infrastructure, but owners remain responsible for their own systems. We inspect the visible drainage arrangements, look for evidence of previous flooding, and consider how well any flood mitigation measures are working.

A Level 3 Survey is particularly important here because of the age of the housing stock. Many homes in this area date from the 18th or 19th century, from a time when materials and construction standards were very different from those used now. Period properties often include traditional methods that need informed assessment, such as lime mortar instead of cement, traditional timber frame construction, and hand-made bricks that can be more vulnerable to frost damage than modern equivalents.

Building styles in Goole Fields reflect the East Riding marshland and the practical methods developed over centuries to deal with local conditions. Traditional farmhouses here were often built with local bricks made from the region's clay-rich soils, usually bedded in lime mortar rather than cement. Because lime mortar lets a building "breathe" and has more flexibility than modern cement-based mortars, maintenance needs to be approached differently, and that is something we understand well.

Older properties in the parish often have pantile or slate roofs, and some farmhouses still have thatched roofs that need specialist assessment. The roof structure may include traditional timber rafters and purlins, sometimes with evidence of historic alteration or repair. We are used to assessing these older roof forms and looking for structural weakness or signs that previous storm damage has led to repairs.

Solid wall construction, which is common in Goole Fields, brings its own issues with insulation and moisture control. There is no cavity, so these walls do not offer the same thermal separation or moisture barrier as modern cavity walls, and that can leave a property more vulnerable to condensation and heat loss. Our Level 3 Survey reviews the property's current thermal performance and sets out ways to improve energy efficiency without harming the building fabric.

In this rural parish, outbuildings and agricultural structures come up regularly. Barns, stables, and former pig houses may all form part of a property, and they are often built to different standards from the main dwelling. Some will also have been adapted for other uses over the years. We include these ancillary buildings in our assessment because they can influence the value and practical use of the property, and in some cases they may have structural implications for the main house.

From our survey work across the East Riding, including the rural parishes around Goole, a few patterns appear again and again. Damp penetration is one of the most frequent findings, especially in older farmhouses with solid wall construction. In Goole Fields, the high water table and nearby drainage channels can draw moisture into walls by capillary action, particularly where render or pointing has broken down. To pick up both visible and concealed problems, we use moisture meters and thermal imaging equipment.

Structural movement is another issue we watch closely in this part of the East Riding. Because the alluvial soils are compressible, buildings can settle unevenly over time, which may show up as cracked walls, sloping floors, or doors and windows that no longer close properly. We distinguish between minor settlement cracks that are cosmetic and more serious movement that could call for underpinning or other remedial work. Our report explains how severe any movement appears to be and what follow-up action makes sense.

Roofing condition on traditional properties needs careful checking too. Many farmhouses in the Goole Fields area have older roof coverings that may have been patched or repaired several times over the years. We look for missing or damaged tiles, evidence of past leaks, and the condition of fascias and soffits. We also record any nearby agricultural buildings or other structures, since they can sometimes affect the main dwelling through movement or drainage issues.

Private drainage is a regular source of trouble here, as many properties depend on septic tanks or cess pools instead of mains sewerage. These systems need ongoing maintenance, and where that has been neglected they can fail, creating health risks and environmental problems. We inspect the visible drainage infrastructure, note the position of septic tanks or cess pools, and comment on their condition and maintenance history where that can be established.