RICS Level 3 Building Survey in Tixall

The character of Tixall as an unspoilt estate village means that a significant proportion of its housing stock predates modern building regulations. Properties here were constructed using traditional methods that differ substantially from contemporary construction, including solid wall construction, lime-based mortars, and original timber frame elements. These age-related characteristics bring specific risks that our inspectors assess in detail during every Level 3 Survey we conduct in the village. Many cottages date from the 18th and 19th centuries, built when different standards applied entirely to structural design.

The predominant building materials in Tixall include red brick ranging from orange-red to brown-red tones, along with the locally distinctive Tixall Stone sourced from historic quarries. Staffordshire blue clay tiles dominate the roofing, though some properties feature dark grey slate or red clay tiles. Our surveyors understand how these materials perform over time, identifying issues such as mortar erosion in lime-based pointing, tile slippage on heritage roofs, and stonework deterioration that may require specialist conservation repairs. At properties like Tixall Farm and Tixall Lodge, we pay particular attention to stone lintels and sills which can suffer from frost action.

Given that Tixall lies within both a Conservation Area and the Cannock Chase Area of Outstanding Natural Beauty, properties here face additional considerations that affect their value and maintenance requirements. The presence of 15 listed buildings within the civil parish, including the Grade I listed Gatehouse, means that many transactions in this village involve properties with special architectural or historic interest. A Level 3 Survey provides the detailed assessment necessary for informed decision-making on such significant investments. Our reports specifically address conservation area constraints and listed building implications.

Properties adjacent to the River Sow and the Staffordshire and Worcestershire Canal face potential flood risks that warrant careful assessment during any survey. The canal expands into Tixall Wide near the historic Gatehouse, creating additional water management considerations for nearby properties. Our inspectors examine drainage systems, retaining walls, and flood mitigation measures as part of every Level 3 assessment in this area.

• Assessment of historic construction methods
• Identification of potential conservation area constraints
• Evaluation of aging building fabric
• Analysis of flood risk from River Sow proximity
• Review of structural movement in older properties

Properties in Tixall, given their age and traditional construction methods, commonly exhibit specific defects that our Level 3 Survey is specifically designed to identify and assess. Damp issues represent one of the most frequent problems we encounter, arising from rising damp in solid wall constructions, penetrating damp through aged brickwork and stonework, and condensation in properties with inadequate ventilation. The original lime-based mortars used in many Tixall cottages are particularly susceptible to moisture ingress when compared to modern cement-based alternatives, and our inspectors know exactly how to assess the extent of any damp-related damage.

Timber defects also feature prominently in our surveys of Tixall properties. Older structural elements, including floor joists, ceiling timbers, and roof rafters, can suffer from woodworm infestation or wet and dry rot, particularly in areas where moisture has been allowed to accumulate over years of occupation. Original joinery such as windows, doors, and fitted furniture may show signs of decay or movement that reflects the natural settling of the building over decades. Our inspectors physically probe timber elements where appropriate and assess the overall structural integrity of wooden components.

Roofing issues are particularly common given the prevalence of Staffordshire blue clay tiles and slate roofing throughout the village. Tile slippage, cracked tiles, and deterioration of leadwork around chimneys and valleys all feature in our defect assessments. At properties with slate roofs such as Tixall Court, Tixall Mews, and The Bothie, we examine the condition of individual slates and their fixings, as well as the integrity of underfelt which may have deteriorated over time. The red clay tiles found at St John the Baptist Church and the Village Hall require similar attention to prevent water ingress.

The underlying geology of Tixall, with its combination of Lower Keuper sandstone and areas of Mercia Mudstone, can contribute to foundation movement in some properties. Clay-related subsidence or heave may affect properties built on the eastern and western fringes of the village where mudstone is present, particularly following periods of drought or heavy rainfall. Our surveyors examine walls for characteristic cracking patterns, assess door and window operation, and measure floor levels to identify any signs of structural movement that might suggest foundation issues.

Tixall's position in the Sow Valley, approximately 4 miles east of Stafford, brings specific environmental considerations that our inspectors take into account during every survey. The River Sow forms a natural boundary to the south of the village, joining the River Trent on the nearby Shugborough estate. Properties in lower-lying areas adjacent to the river and the Staffordshire and Worcestershire Canal face potential fluvial and surface water flooding risks that warrant careful assessment. The canal expands into Tixall Wide near the historic Gatehouse, creating additional water management considerations for nearby properties.

The local geology beneath Tixall consists primarily of Lower Keuper sandstone from the Sherwood Sandstone Group, characterised by fine-grained red-buff sandstones. However, Mercia Mudstone (Keuper Marl) is found to the east and west of the village, and this clay-rich geology presents a potential shrink-swell risk when moisture levels change. Our inspectors examine properties for signs of foundation movement, cracking patterns, and other indicators that may suggest clay-related subsidence or heave, particularly in properties with shallower foundations typical of their construction period. The area between the Hopton and Tixall Faults overlies the Cannock Chase Formation or Bunter Pebble beds, which can also affect ground conditions.

While no specific mining activity is recorded within Tixall itself, Staffordshire has a broader history of mining that sometimes affects properties in the county. Our surveyors are experienced in identifying signs of mining-related subsidence or ground movement, checking for characteristic crack patterns, uneven floors, and other structural indicators that might suggest ground instability from historical mining activity. We specifically look for evidence of past mining in the broader Staffordshire area that might affect properties in this village.