RICS Level 2 Survey in Cosby

Cosby is in the Blaby district, and its housing ranges from long-established village homes to more recent development. Beneath much of the village sits Mercia Mudstone, a red silty mudstone with significant clay deposits. That matters. It creates a moderate to high shrink-swell risk, especially where mature trees are close by or moisture levels change through the year. Our team knows the signs this ground can leave behind, including cracking patterns, door and window binding, and problems with damp proof courses made worse by movement in the soil.

The designated Conservation Area covers the historic core of Cosby, including parts of Main Street, Church Street, and Little Thorpe. There are also several Listed Buildings, among them St Michael and All Angels Church, which is Grade I Listed, along with historic cottages and farmhouses that are Grade II Listed. Homes in these parts often call for closer attention. Our surveyors are used to older construction in the village, from local red brick to solid wall construction and original lime mortar pointing, all of which can need a different maintenance approach.

A good number of Cosby homes date from the pre-1919 period, with more building taking place across the twentieth century. As a result, a substantial share of properties are now over 50 years old, which is one reason a RICS Level 2 survey can be so useful. Age brings its own risks. Hidden defects can include worn timber, outdated electrical installations, and original materials that may contain asbestos, such as Artex coatings or floor tiles from the mid-to-late twentieth century. Census data for the Blaby district shows around 40-45% of properties are detached, with another 30-35% semi-detached, so many homes in Cosby have sizeable external elements that deserve a proper inspection.

Cosby's location near the River Soar catchment area puts some homes, especially those in lower-lying parts of the village or close to the watercourse, at potential risk from both surface water and fluvial flooding. We look at drainage conditions and flood risk indicators as part of every Level 2 survey and flag anything that could affect the purchase. That local grounding helps. It means we can read the village's infrastructure and historic development patterns in a way a standard, non-local survey often will not.

From the work we carry out across Cosby and the wider Blaby district, a few problems come up time and again. Damp is high on that list, especially rising damp in older solid-wall homes where the original damp proof course has failed or been bridged over the years. Penetrating damp is another regular finding, often tied to defective rainwater goods, worn pointing, or damaged roof coverings on houses with traditional slate or clay tile roofs. Because Cosby has both older solid-wall stock and newer cavity wall homes, the way damp shows itself can vary quite a bit from one property type to the next.

Roofing needs a careful look. In older properties, we often see wear to original roof coverings, defective flashings, and roof structures that have started to sag. Flat roofs can also show deterioration where they exist. Timber defects turn up as well, including woodworm infestation and wet or dry rot, usually where damp is present or ventilation is poor. These repairs can become expensive, which is why we inspect all accessible roof spaces and timber elements in detail.

Because much of Cosby's housing stock is older, outdated electrics and plumbing are common findings. Homes built before the 1980s often need full rewiring and plumbing upgrades to meet current standards. As part of our usual assessment, we check consumer units, wiring condition, and plumbing materials. There is another point to watch too. Asbestos-containing materials may be present in homes built or refurbished between the 1950s and 1990s, including Artex wall coatings, floor tiles, or insulation materials. Our surveyors know the usual locations and will flag any suspected asbestos for specialist sampling.

Mercia Mudstone sits under Cosby, and its clay content means movement is something we examine carefully. We look for cracking patterns, especially diagonal cracks around window and door openings, and for doors or windows that sticks or fail to close properly. We also check for signs of uneven settlement. Large trees can increase the shrink-swell risk because roots draw moisture from the clay soil, which then contracts and expands with seasonal change. Where we see indicators of movement, we assess tree proximity and may recommend further investigation by a structural engineer.