RICS Level 3 Building Survey in Clumber and Hardwick

Clumber and Hardwick properties bring their own surveying quirks, which is why a Level 3 Survey is so useful here. Hardwick Village dates from the 1850s, built as a model village for estate workers, and the homes were put up with traditional brickwork, timber roof structures and slate or tile coverings. Many are now approaching, or have passed, 150 years of age, so they have usually seen more than one round of alteration, repair and maintenance. Our inspectors know how to read those older structures and spot the sorts of defects that build up over time.

Hardwick Village is managed by the National Trust as a commercial entity, with properties occupied under tenancy arrangements. That brings its own set of considerations for buyers, because covenants or planning constraints can affect what changes are possible. Book a Level 3 Survey with us and our inspector will flag any visible effects of those arrangements, then point you towards anything that needs checking further with the National Trust as landlord. We have surveyed several homes in the village and understand how the tenancy system operates.

Nottinghamshire’s geology includes Permian and Triassic sandstones and mudstones, alongside pockets of clay-rich soils, so shrink-swell movement can be a real issue for foundations. Detailed mapping would be needed for a precise picture in Clumber and Hardwick, but the risk of clay-related movement is present in this part of the county. Hardwick Ford, which may be the longest watercourse in Nottinghamshire, also points to alluvial deposits in valley locations, and those can change ground conditions. Our Level 3 Survey looks at the likelihood of subsidence and advises whether specialist follow-up is sensible.

• Victorian brick construction dating from 1850s
• 26 listed buildings requiring specialist knowledge
• Potential mining subsidence from Nottinghamshire coal mining history
• Traditional timber roof structures with age-related wear
• National Trust covenant considerations affecting modifications
• Properties approaching or exceeding 150 years of age

Homes in Clumber and Hardwick, most of them Victorian or Edwardian, often show defects that our inspectors know well. Damp is common, whether it appears as rising damp from a failed damp-proof course, penetrating damp from worn external render or roof coverings, or condensation linked to poor ventilation in older buildings. Because solid walls were standard in this period, there is no cavity wall insulation like you would find in modern houses, which can affect heat retention and add to moisture problems. We use professional moisture meters during inspection to find the source and spread of damp, not just to note that it is present.

Another recurring issue in this area is timber decay. Floor joists, structural beams and window frames made from softwood can suffer rot and woodworm over a lifespan of 150 years or more. Where we can reach them, our inspectors tap and probe timber members to judge their condition and recommend treatment when needed. In many older properties here we have found rot in floor joists and supporting beams, especially where water has entered through defective gutters or rising damp.

We often find roofing defects such as wear in slate and tile coverings, slipped or missing tiles that let water through, failing leadwork around chimneys and valleys, and sagging or damaged rafters. These traditional roofs were never built to carry the weight of modern additions like satellite dishes or solar panels, especially when they have been fitted over the years without proper thought for the structure. Our survey records any roof modifications that may have affected its integrity.

Chimney stacks deserve particular attention in homes of this age. Many Victorian and Edwardian chimneys have tired pointing, damaged flashings or cracked pots, all of which can let water in. Some have been capped or partly demolished for safety, and our survey notes the condition of any chimney and the repairs it needs. Because older houses often used several fireplace chimneys, the resulting stacks can be complex and need careful assessment.

• Rising and penetrating damp in solid wall construction
• Timber rot and woodworm in floor joists and beams
• Roof slate deterioration and slipped tiles
• Chimney stack defects and leadwork failures
• Original window frames requiring restoration
• Inadequate insulation and heating efficiency
• Deteriorated render and brickwork pointing

Nottinghamshire has a long coal mining history, and the Bassetlaw district around Clumber and Hardwick is no exception. A Coal Authority report would be needed for a precise mining history in the immediate area, but homes in this region may still be affected by historic workings. Subsidence can happen many years after mining has stopped, and old mine workings can alter ground stability. We look for signs of movement or cracking in walls and foundations that may point to subsidence, and we recommend a mining search report when our observations suggest it is sensible.

Clay soils are present in parts of Nottinghamshire, and they can shrink and swell as moisture levels change. After periods of drought followed by heavy rainfall, clay-rich ground may expand and contract enough to stress foundations and trigger subsidence or structural movement. Our Level 3 Survey looks for visible signs of ground movement and will recommend further investigation if we see anything of concern. We pay close attention to cracking patterns in walls that may indicate foundation movement.

The watercourses nearby, including Hardwick Ford which may be the longest in Nottinghamshire, point to superficial deposits and alluvium in valley areas. Properties in lower-lying parts of the parish may therefore be vulnerable to surface water flooding or fluvial flooding from these watercourses. As part of our survey we consider the setting of the property and note any obvious flood risk factors. For homes in valley locations, we recommend checking the Environment Agency flood risk maps as part of due diligence.

Clumber Park and the surrounding area sit within the historic "Dukeries" region of Nottinghamshire, long associated with country houses and estates. Geology here can change sharply over short distances, with superficial deposits of glacial till and alluvium lying over the solid bedrock. Our inspectors are used to spotting signs of ground instability in this part of the county and will say if a specialist geotechnical assessment looks necessary.