Outcome NR1 Peatland and heathland

Outcome NR1

Peatlands are under restoration to good hydrological and biological condition. Heathland mosaics are larger in extent and more structurally diverse.

Peatlands of any depth, with their associated mire, fen, flush, carr, wet and dry heath and grassland habitats, should be managed as dynamic landscape-scale mosaics to support the full range of species associated with these habitats. Hydrological integrity is the key to this, and hydrological restoration is, therefore, often the primary intervention required to restore good ecological condition on peat soils.

A new England Peat Map was published by Natural England in 2025 [74]. Using the integration of AI techniques with satellite imagery, pre-existing peat survey data, new field survey data, data on geology, topography (LIDAR) and historic land-use, the models underlying the maps give an overall accuracy of 95% for the extent of peat soils. Natural England defines peat soil as any soil with an organic content of 20 percent or more and a thickness of at least 10 cm. This definition is used as the basis for the phrase 'peat soils' in the measures, and as the basis for the map for Outcome NR1.

71% percent of the North Pennines National Landscape is covered in peat soils. A variety of different vegetation communities exist on these peat soils in an intricate mosaic. Where these communities exist on deep peat (30cm or more) they are broadly categorised as blanket bog (36% of the National Landscape), and on shallower peat soils they are broadly categorised as heathland (17% of the National Landscape).

The discrepancy between the total area of peat soils (71%) and the total area of blanket bog and heathland habitats which are recorded on them (43% of the National Landscape) is due to a number of factors, including inaccuracies in the peatland data model, the existence of other priority habitats such as flushes and fens which exist on peat soils, the misclassification of habitats, and the existence of some plantation of conifers on peat. However, the biggest contributor to the gap is from degraded habitat known as grass moorland or ‘white moor’, which no longer meets the definitions of blanket bog or heathland (although it may have other conservation benefits – e.g. for wading birds.

59% of the North Pennines National Landscape is covered in deep peat soils (30cm and over). However only 36% of the National Landscape is classified as blanket bog on the Priority Habitat Inventory because much former blanket bog has degraded and dried out and been misclassified as upland heath or grass moorland, or not included at all on the Priority Habitat Inventory.

On shallower peat soils in the North Pennines the predominant type of heathland habitat should be wet heath [76](See also Box 3 Some components of the heathland mosaic at the bottom of this page). Natural England defines peat soils of 10-30 cm depth as indicative of a wet heath habitat that should be restored to support Favourable Conservation Status (FCS), requiring restoration of natural hydrology and habitat mosaic. [75]

Blanket bog

The North Pennines contains 37% of England's blanket bog.

Blanket bog forms in areas of high rainfall where peat has developed, not only in hollows, but across large expanses of flat and undulating ground. Peat formation results from the incomplete decomposition of plants in waterlogged conditions, and their accumulation over time. Blanket bog habitat is what one would expect to see on all but the more steeply sloping high ground [66].

A good quality tract of blanket bog in the North Pennines contains a hummock-hollow complex of multiple peat-building Sphagnum moss species accompanied by dwarf shrubs such as heather, cross-leaved heath, crowberry, cloudberry and bilberry, and other characteristic plants such as cotton grasses, deergrass and bog asphodel. This plant community, and the invertebrates it supports, relies on keeping the water table high (within 10cm of the surface for most of the year). When in good condition these areas will also be actively forming peat.

From the mid-1940s, land managers were paid to drain peatlands in the North Pennines to make them more accessible for grazing by sheep. The consequences have been a disastrous loss of blanket bog and the accompanying biodiversity, carbon and water storage capacity. A very high priority for nature recovery, but also for recovering water storage and carbon sequestration, is the re-wetting of peat.

Upland heath

Heathlands are an important part of naturally functioning upland ecosystems. On shallower peat soils and on mineral soils with peat pockets there is often an intricate mosaic of geology, slope and peat depth. This should, in turn, lead to a complex mosaic of wet and dry heath, dwarf shrubs of various ages, species-rich grasslands and developing scrub, and provide food and shelter for a wide diversity of species, and resilience to climate change.

Over 17% of the North Pennines is classified as heathland, although (see above) some of this is likely to be misclassified blanket bog which has been drained and degraded. Extensive areas of upland heathland (and blanket bog) are managed for grouse, which involves the rotational burning or cutting of the heathland to ensure the plentiful supply of young heather shoots for the grouse to eat, and to control heather beetle, an invertebrate that can defoliate large areas of heather. However, this results in extensive areas of heathland (and blanket bog) comprising a simplified plant community dominated by young heather.

Maximising the potential of upland heath for wildlife requires the development of a dynamic mosaic of heathland habitats, including wet and dry heath, acid grassland, fen and open water habitats, wood pasture, bracken, and native scrub extending across the full altitudinal range for these habitats, from lowland to montane heath. The wet and dry heath elements of this mosaic should have dwarf shrubs with a varied age structure. Alongside hydrological restoration, management of grazing and browsing can deliver most of this change. See Box 3 Some components of the heathland mosaic, for a fuller description of a healthy heathland mosaic.

Increasing the amount of vegetation within upland heathlands needs to be considered in terms of potential fire risk. Heather species (in particular Calluna vulgaris) and purple moor grass burn easily and fiercely, and so any increase in the amount of these vegetation types in an unbroken formation potentially increases the fuel available to a wildfire, making it more intense and harder to control. Conversely, blocking drains on both peatland and heathland increases the amount of time that soils are wet, if not saturated, and much of the vegetation comprising the potentially increased fuel load would comprise deciduous tree and scrub species that are not flammable when alive due to their high moisture content. However, it is important that wildfires are planned for, especially given the increasing temperatures being experienced during dry spells due to climate change.

There is room for an increase in the extent of heathland mosaic through the restoration of other areas on shallow peat and mineral soils, including restoration of grass moorland (often derived from former heathland through overgrazing and/or burning), and through removal of conifer plantation (planted on former heathland) and the restructuring of woodland blocks (planted on former heathland) towards scrubby heath.

Non-native gamebirds, such as pheasants and red-legged partridges, are released in large numbers each year for shooting. Large concentrations of these birds have a range of ecological effects. Their predation of reptiles such as adder is a concern, and their impact on invertebrate food sources may also be so. The birds themselves, and the food put out for them, support species such as carrion crow, which in turn can be a threat to important breeding wader populations. While the release of gamebirds within 500m of Special Protection Areas (sites of international importance for birds) requires licensing by Natural England, this does not extend to other important wildlife sites. See Box 4 Non-native game birds.

What other services does this outcome provide?

Healthy peatlands with sphagnum mosses help to slow the flow of water through the landscape and provide a natural flood defence function for areas downstream. This is true even when peatlands are already saturated with water, as flow rates are significantly slowed by surface roughness. [67,68,69.70,71,72]
Much of our drinking water passes through upland peat soils and peat can filter and retain atmospheric pollutants. In contrast, eroding peat can release sediment and carbon into watercourses resulting in higher costs to water companies and, ultimately, higher prices for consumers.
Peatlands are the largest natural carbon store in the world and globally store more carbon (more than 600 gigatonnes - up to 44% of all soil carbon) than all other vegetation types including the world’s forests. Damaged peatlands are a source of anthropogenic carbon dioxide, making peatland restoration an important tool for reducing greenhouse gas emissions.

Which species are supported by this outcome?

Champion species

Black grouse; Cuckoo; Curlew; Dunlin; Hen harrier; Ring ouzel; Adder; Bilberry bumblebee; Green hairstreak; Large heath; the Arctic Alpine assemblage

Annex 1 species

Curlew, Golden plover; Merlin, Yellow Marsh Saxifrage

Map1 shows the extent of peat soils (target area for Outcome NR1) and of deep peat (30cm and above). Explore Map 1 in a new window

Map 2 shows the major habitats overlying peat soils in the North Pennines. Explore Map 2 in a new window

Measures for outcome NR1

Select each measure for its full detail and to view the organisations and groups with an important role in making them happen.

Targets and monitoring data for peatland restoration can be found in the Measuring Progress section.