RICS Level 3 Building Survey in Bowland-with-Leagram

Bowland-with-Leagram sits within the Forest of Bowland Area of Outstanding Natural Beauty, and this designation significantly influences the type of properties you will find here. The housing stock is dominated by historic farmsteads, traditional stone cottages, and isolated rural dwellings, many of which date back to the 18th century or earlier. These properties were built using local materials and traditional techniques that differ substantially from modern construction standards.

The local geology presents particular considerations for surveyors. The area features Carboniferous rocks including Pendle Grit and Bowland Shale, with the latter creating clay-rich soils that can lead to shrink-swell movement. Properties built on these substrates, particularly those on steep valley sides near Chipping Brook, may show signs of historical movement or subsidence that our inspectors know to assess carefully.

Flood risk is another factor that affects properties in Bowland-with-Leagram. The River Hodder and its tributaries flow through the valley floors, and properties in low-lying areas face potential flood exposure. Our surveyors will assess flood resilience and any existing flood damage or remediation measures when inspecting properties in these locations.

Many properties in this area are listed buildings or fall within conservation considerations, which imposes strict planning controls on any future alterations or repairs. Our surveyors will identify any listed building status and note how this may affect your plans as an owner. Always check the National Heritage List for England (NHLE) for specific property designations before purchasing.

• Traditional stone construction
• Historic farmsteads
• Clay-rich soil movement
• Flood risk zones

Properties in Bowland-with-Leagram were predominantly built using traditional stone construction techniques that reflect the local geology and available materials. The characteristic gritstone walls, often rendered with lime plaster, form the external envelope of most historic properties. These solid wall constructions lack the cavity spaces found in modern buildings, which has significant implications for both thermal performance and moisture management.

The roofing on period properties in this area typically consists of natural slate, sourced historically from local quarries in Lancashire and Cumbria. Our inspectors examine slate conditions carefully, checking for slipped or damaged tiles, deterioration of lead flashings, and the condition of stone-flagged verges and ridges. Traditional features such as stone chimneys, parapet walls, and dormer windows require specific attention during our inspection, as these elements are common sources of water penetration in older properties.

Foundation construction in the area typically consists of shallow strip footings, with some older properties built directly on ground beams or even on stone flags laid directly on the ground. These foundation approaches can be vulnerable to movement in the clay soils prevalent throughout the Bowland Shale formations, particularly during periods of drought or sustained wet weather. Our surveyors assess the relationship between the property and the surrounding ground, looking for signs of differential settlement or ongoing movement.

Traditional outbuildings and agricultural structures form an important part of the property inventory in Bowland-with-Leagram. These buildings, often constructed of timber frame with stone panel infill or using traditional barn brick, may have been converted to residential use or may remain as ancillary structures. Our Level 3 survey includes assessment of all buildings within the property curtilage, ensuring you have a complete picture of condition and any potential liabilities.

Properties in this area face several specific risks that our Level 3 surveys address in detail. The clay soils prevalent throughout the Bowland Shale formations can cause significant ground movement during periods of drought or heavy rainfall. This shrink-swell activity can lead to subsidence or heave, particularly in properties with shallow foundations on unstable ground. Our surveyors will identify any signs of historic movement, including cracking patterns that may indicate ongoing structural stress.

Land stability represents another consideration, especially for properties on steep slopes near watercourses. Historical landslip risks exist in upland areas and valley sides, and our inspectors assess the surrounding topography as part of their evaluation. Properties near Chipping Brook or other tributaries of the River Hodder require particular attention to boundary conditions and any existing retaining structures.

The agricultural heritage of the area means many properties include traditional outbuildings, barns, or agricultural structures that may have been converted or may form part of the property boundary. These structures often have their own set of condition issues, from asbestos in older barn roofs to timber frame deterioration in traditional farm buildings. Our Level 3 survey includes assessment of all structures within the property curtilage.

Flood risk from the River Hodder and its tributaries affects properties in valley floor locations. Our surveyors identify whether properties fall within flood risk zones and assess any existing flood resilience measures. We note evidence of previous flood damage and advise on potential mitigation measures that may be required.