RICS Level 2 Survey Holme upon Spalding Moor

Holme upon Spalding Moor brings its own points for buyers to consider. The village sits on Mercia Mudstone bedrock, a clay-rich geology that can cause ground movement during wet and dry cycles. Our inspectors look for subsidence, cracking, and movement that might point to problems in the underlying soil. Alluvium deposits from the historic marshland add another layer of complexity to foundation checks, especially in the lower-lying parts of the village.

Most homes here date from the 18th and 19th centuries, although some are older still. Holme Hall, a Grade II* listed country house dating from 1720-30, is a good example of the traditional brick and rendered construction used in the area. All Saints' Church, a Grade I listed building with origins in the 13th century and mentioned in the Domesday Book, shows just how long settlement has been established here. Our surveyors are used to older buildings, so we check for damp, timber decay, and the condition of traditional features that newer survey methods can miss.

Because Spalding Moor was once marshland, some parts may be prone to surface water flooding and dampness. We inspect drainage around properties, look for signs of water ingress, and assess how well existing damp-proof courses are performing. That matters most for lower-lying homes or those with gardens edging the historic watercourses. Gypsum beds recorded in the local geology can also influence foundation conditions in some areas.

Brick produced from the clay-rich Mercia Mudstone helped shape the look of many properties in Holme upon Spalding Moor. Historical occupations in the village, including bricklayers and ornamental plasterers, reflect that legacy, and brick and render still define a lot of homes today. Our surveyors know these traditional methods well, so they can pick up issues specific to older brickwork, such as cement mortar degradation or rising damp.

• Foundation and subsidence assessment
• Damp and timber decay inspection
• Roof and chimney condition check
• Electrical and plumbing visibility review
• Drainage and flood risk evaluation
• Energy efficiency advisory

Below Holme upon Spalding Moor lies geology that deserves close attention from buyers. Mercia Mudstone bedrock is made up of mudstone that expands and contracts as moisture levels change, which can affect foundations. This shrink-swell behaviour is often most noticeable during drought or heavy rainfall, both familiar in the Yorkshire region. Add in the alluvial deposits from the historic marsh, and differential movement can occur in some properties, particularly those with shallower foundations.

Our surveyors are trained to spot the tell-tale signs of ground movement. They look for cracks in walls that follow certain patterns, doors and windows that stick or fail to close properly, and uneven floors. Older homes without modern deep foundations can show these issues more clearly, especially after heavy rainfall or drought. The Keuper marl hill the village sits on adds more complexity to ground conditions in some areas.

Drainage is another important consideration, given the village's proximity to historic watercourses and the character of Spalding Moor. Older drainage systems may need checking, so our surveyors assess guttering, downpipes, and how surface water is being disposed of. Any concerns are set out clearly in the report, along with recommendations for further investigation. Surface water flooding can be an issue in areas with alluvial deposits, especially during heavy rainfall.

Ground conditions can vary quite a bit between the single hill of Keuper marl and the lower-lying marshland. When we assess a property, we take its exact position in the village into account. Purchasing near the historic centre around All Saints' Church or on the newer outskirts, we adapt the inspection to the conditions affecting that home.

From our experience surveying homes across the East Riding, a few issues keep turning up in Holme upon Spalding Moor. Rising damp is common in older brick properties, especially where there is no modern damp-proof course or an existing one has failed. Our surveyors use visual clues and moisture meters to gauge damp levels and suggest the right form of remediation. Timber decay, including wet and dry rot, is also seen in many period properties, particularly where ventilation is poor or there has been historical water ingress.

Roof defects appear regularly in our surveys, especially on older properties with original slate or tile coverings. We check for missing or damaged tiles, deteriorated pointing to ridge tiles, and evidence of past leaks. Chimney stacks, which are common on period homes, often show decay to lead flashings, damaged brickwork, or deteriorating pargetting. Left alone, those faults can let water in and lead to bigger problems.

Movement linked to the local clay soils is another frequent finding. We see diagonal cracking at the corners of windows and doors, differential settlement in bay windows, and movement in rendered walls. Some movement is normal in older properties, but our surveyors judge whether it is active and whether more investigation is needed. Properties showing subsidence indicators may benefit from a structural engineer's assessment before purchase.

Defective guttering and downpipes cause a great deal of damage in the properties we inspect. In Holme upon Spalding Moor, where older drainage systems are common, we often find blocked or damaged gutters that overflow and saturate walls. That can make damp worse and, over time, contribute to structural issues too. Any drainage defects are flagged clearly in our report, with the repairs we recommend.