RICS Level 3 Building Survey in Clumber and Hardwick

The properties in Clumber and Hardwick present unique surveying considerations that make a Level 3 Survey particularly valuable. Hardwick Village was created in the 1850s as a model village for estate workers, with properties constructed using traditional brick methods and timber roof structures with slate or tile coverings. These buildings, while full of character, are now approaching or exceeding 150 years of age, meaning they will have experienced various phases of alteration, repair, and maintenance over the decades. Our inspectors understand how to assess these aging structures and identify problems that have developed over such a long lifespan.

The National Trust manages Hardwick Village as a commercial entity, and properties are occupied under tenancy arrangements. This creates specific considerations for prospective purchasers, as properties may be subject to covenants or planning constraints that affect what modifications can be made. When you book a Level 3 Survey with us, our inspector will note any visible implications of these arrangements and advise you on what to investigate further with the National Trust as landlord. We have surveyed multiple properties in this village and understand how the tenancy system works.

Nottinghamshire's geology, which includes Permian and Triassic sandstones and mudstones alongside areas of clay-rich soils, can present shrink-swell risks that affect property foundations. While specific geological data for Clumber and Hardwick requires detailed mapping, the potential for clay-related movement exists in this region. The presence of Hardwick Ford, potentially the longest watercourse in Nottinghamshire, indicates alluvial deposits in valley areas that can affect ground conditions. Our Level 3 Survey includes assessment of potential subsidence risks and advice on whether further specialist investigation is warranted.

• 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

Properties in Clumber and Hardwick, predominantly dating from the Victorian and Edwardian periods, commonly exhibit certain defects that our inspectors are well-versed in identifying. Damp issues are frequently encountered, whether rising damp from compromised damp-proof courses, penetrating damp from deteriorated external renders or roof coverings, or condensation resulting from inadequate ventilation in older properties. The solid wall construction typical of this era lacks the cavity wall insulation found in modern homes, which can affect thermal performance and contribute to moisture-related issues. When we inspect, we use professional moisture meters to identify the source and extent of any damp problems rather than just noting their presence.

Timber defects represent another significant concern in this area's housing stock. Floor joists, structural beams, and window frames constructed from softwood are susceptible to both rot and woodworm infestation over their lifespan of 150 years or more. Our inspectors tap and probe timber elements where accessible to assess their structural integrity and recommend appropriate treatment where necessary. We have found rot in floor joists and supporting beams in many older properties in this area, particularly where water has penetrated from defective gutters or rising damp.

Roofing problems commonly identified include wear and tear to slate and tile coverings, slipped or missing tiles allowing water penetration, deteriorated leadwork around chimneys and valleys, and sagging or damaged rafters. The traditional roofs on these properties were not designed to support the weight of modern equipment such as satellite dishes or solar panels, which may have been added over the years without proper consideration of structural implications. Our survey will note any modifications to the roof structure that may have compromised its integrity.

Chimney stacks are a particular concern in properties of this age. Many chimneys in Victorian and Edwardian houses have deteriorated pointing, damaged flashings, or cracked pots that allow water ingress. Some may have been capped or partially demolished for safety reasons, and our survey will note the condition of any chimney and advise on necessary repairs. The historic practice of using multiple fireplace chimneys means many properties have complex chimney stacks that require 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 history of coal mining, and the Bassetlaw district around Clumber and Hardwick is not exempt from this legacy. While specific mining data for the immediate area would require a Coal Authority report, properties in this region may be at risk from historic mining activity. Surface subsidence can occur many years after mining operations cease, and the presence of old mine workings can affect ground stability. We include visual assessment of walls and foundations for signs of movement or cracking that may indicate subsidence issues, and we recommend a mining search report where appropriate based on our observations.

Clay soils, which are present in parts of Nottinghamshire, can undergo shrink-swell movement depending on moisture content. During periods of drought followed by heavy rainfall, clay-rich soils can expand and contract significantly, putting stress on foundations and potentially causing subsidence or structural movement. Our Level 3 Survey includes assessment of visible signs of ground movement and will recommend further investigation if concerns are identified. We pay particular attention to cracking patterns in walls that may indicate foundation movement.

The watercourses in the area, including Hardwick Ford which is potentially the longest in Nottinghamshire, indicate the presence of superficial deposits and alluvium in valley areas. Properties in lower-lying parts of the parish may be susceptible to surface water flooding or fluvial flooding from these watercourses. Our survey includes observation of the property's setting and will note any apparent flood risk factors. We recommend checking the Environment Agency flood risk maps as part of your due diligence for properties in valley locations.

Clumber Park and the surrounding area fall within the historic "Dukeries" region of Nottinghamshire, an area known for its country houses and estates. The geology in this part of Nottinghamshire can vary significantly over short distances, with superficial deposits of glacial till and alluvium overlying the solid bedrock. Our inspectors are experienced in identifying the signs of ground instability that can affect properties in this region and will advise if a specialist geotechnical assessment is warranted.