What makes Upper Teesdale special?
Upper Teesdale, in England’s North Pennines, is an internationally important geological area within the North Pennines UNESCO Geopark. Its combination of calcareous geology, cold springs, high altitude and distinct local climate creates conditions unusual in Britain, allowing plant species with very different geographical distributions to occur together.
The site supports an almost complete range of typical English upland habitats and a nationally important assemblage of plants, including several species found nowhere else in England. This diversity has led to its designation as a Special Area of Conservation (SAC) and a Site of Special Scientific Interest (SSSI), while its bird assemblages also qualify it as a Special Protection Area (SPA). Moor House, England’s largest terrestrial National Nature Reserve, lies partly within the SSSI. The renowned botanist Dr Margaret Bradshaw published a book documenting her seven decades of work recording the flora of the area in 2023.
The assessment
A SSSI Condition Assessment in England evaluates the condition of a ‘feature’—a habitat, a species or an assemblage of species. Specific attributes are assessed, such as plant species diversity and the presence or absence of particular indicator species, alongside indicators of pressures such as overgrazing, undergrazing and drainage. Across the UK, the Joint Nature Conservation Committee (JNCC) sets the criteria through its Common Standards Monitoring guidance. Based on the assessment results, the feature is assigned a condition category ranging from unfavourable to favourable. The survey requires specialist surveyors with ecological and/or botanical expertise.
For peatland conservation, this assessment is particularly valuable: it is one of the few recent condition assessments of a large upland site containing a full range of upland peatland and associated mosaic habitats. These include approximately 8,000 hectares of blanket bog; internationally important alkaline fens and alpine flushes; spring-heads, rills and flushes; and alpine and sub-alpine dwarf shrub heaths.
The nationally rare calcareous fens and flushes support an exceptional concentration of rare arctic-alpine and northern montane plants that have survived there since the end of the last Ice Age.