1.2 Mid Anglia
 Natural Areas
graphic
  • Numbers refer to natural areas accessible from the numbered nodes in the left hand window
  • Dark lines are county boundaries
  • White lines are boundaries of character areas within a natural area
The Mid Anglian region has examples of 16 natural areas.
 
1.2.1 33 Trent Valley & Rises
1.2.2 37 The Fens
1.2.3 38 Lincs & Rutland Limestone
1.2.4 39 Charnwood
1.2.5 44 Midland Clay Pastures
1.2.6 45 Rockingham Forest
The royal forest of Rockingham once comprised an extensive tract of semi-natural coppices, some of which were in large, continuous woods many thousands of hectares in extent. These have now been fragmented by clearance and opencast mining, and most of the surviving woods have been converted to plantations.
Of the remaining stands of semi- natural woodland, only the former Purlieu Woods at the north-eastern extremity of the forest are of outstanding importance. These formed one continuous woodland until the mid nineteenth century when the clearance of the western half of Thornhaw Woods cut the woods into two main blocks, Bedford Purlieus to the east and Easton Hornstocks to the west.
1977 Conservation Review
West
graphic
Pipewell
W.I28.  PIPEWELL  WOODS, NORTHAMPTONSHIRE
SP 8286.    80 ha
Grade 2
Monks Arbour and Pipewell Woods lie on deep, calcareous clay soils at the south-western extremity of Rockingham Forest and have a coppice- with-standards structure. Pedunculate oak is the main standard species, with ash, birch and a few planted beech. The coppice layer is dominated by hazel, with ash, dogwood and field maple locally abundant in Monks Arbour Wood. The field layer ranges from Mercurialis perennis-Galeobdolon luteum on the drier soils, to Filipendula ulmaria-Ranunculus repens in waterlogged patches, and Pteridium aquilinum-Rubus fruticosus-Hokus lanatus on the more acidic patches. The ground flora includes such local species as Iris foetidissima and Campanula latifolia. At the southern end of Pipewell Wood, English elm has invaded from the hedge to form a nearly pure community.
This is one of the Ancient Forest coppices. It is typical of such woods and has the advantage that it is not damaged by ironstone working or replanting with conifers, and indeed the coppicing continues actively. Other woods in Rockingham Forest, however, were once known to be richer faunally.
East
graphic
Castor Hanglands
W-44-  CASTOR  HANGLANDS, HUNTINGDON AND PETERBOROUGH
TF noi.    45 ha 
Grade i
The woodlands of Castor Hanglands NNR straddle a zone of marked geological variety in Jurassic rocks, ranging in north-south sequence from limestone to clay, cornbrash, sand and then clay again. The soils reflect this sequence with a range from calcareous loams to calcareous and neutral gleys. Most of the woodland was formerly coppice-with-standards, most of which has been removed, leaving a mixed ash-pedunculate oak woodland, with hazel, privet, dogwood and spindle. On wetter soils, large ash stools occur with hazel, willow and aspen. Part of Moore Wood, also in the reserve, is high forest pedunculate oak. Corresponding with the soil variation, a wide range of field layer types occur; Rubus fruticosus is locally dominant, but Mercurialis perennis-Endymion non-scriptus is the most widespread type, with Primula vulgaris, Anemone nemorosa, Lonicera periclymenum and Euphorbia amygdaloides. Paris quadrifolia, Oxalis acetosella and Allium ursinum occur on the wetter soils. The rides and clearings are kept open and this encourages the rich invertebrate fauna.
The woodlands are a good example of oak-ash woodland, but their most important feature is that they constitute part of a complex of habitats on a range of soil types in a relatively small area.
See also L.8i. 
Bedford Purlieus
W-43-   BEDFORD  PURLIEUS  GROUP, NORTHAMPTONSHIRE, HUNTINGDON  AND PETERBOROUGH
Grade 1
(a) Bedford Purlieus  TL 0499.    185 ha
(b) Wittering Coppice TF 0200.    15 ha.
(c) Easton Hornstocks TF 0100.    50 ha
(d) Collyweston Great Wood TFOOOO.    145 ha
These woods lie mainly on Jurassic limestone covered in places by clay drift with patches of sand. Thus, although the soils tend to be calcareous and poorly drained, there are appreciable areas of freely drained soils of a variety of texture, and some tracts of acidic, sandy soils. The coppice in consequence includes a wide range of types including lime coppice on soils which are appreciably more calcareous than most of its eastern locations, ash, hazel, wych elm, maple coppice on calcareous clays, birch and poplar groves, sessile oak-hazel coppice on acidic sands, valley Ulmus procera woodland and extensive areas of sycamore invasion.
Bedford Purlieus is clearly the most important part of the group. Structurally it is very limited, having been clear- felled in recent decades and partly replanted. Its outstanding feature is its assemblage of herbaceous species (over 450 species of vascular plants have been recorded), which include Euphorbia lathyrus, a species of national rarity, Melica nutans at the southern edge of its range, and E. amygdaloides towards its northern limit. Within this wood both calcicolous and calcifuge species occur together with those found more commonly in northern and western woodlands, including Galium odoratum, Melampyrum pratense, Platanthera chlorantha, Allium ursinum, Conval-laria majalis, Aquilegia vulgaris, Ophrys insectifera, Blechnum spicant, Paris quadrifolia, Luzulasylvatica, Atropa belladonna and Serratula tinctoria. On the grounds of this floristic richness, Bedford Purlieus has been described as one of the most important woods in Britain.
The fauna is also rich, and although it is still relatively unknown, it is regarded as the richest locality in this part of the east Midlands. Among the butterflies recorded are the white admiral, pearl-    bordered fritillary, the silver washed fritillary, the dark green fritillary, high brown fritillary, chequered skipper, brown hairstreak, and white- letter hairstreak. Numerous local moths have been recorded here. It is an isolated east Midland locality for both the palmate newt and the adder.
Coppicing has now stopped entirely in the group. Part of Collyweston Great Wood has become a plantation whilst the centre was cleared for an RAF establishment. A large quarry occupies the centre of Easton Hornstocks. Part of Wittering Coppice has been converted to a poplar plantation. Substantial areas of Bedford Purlieus have been replanted with oak, beech and a variety of conifers, and other sections have been destroyed by quarrying and military needs in wartime. Despite all this, substantial areas of semi- natural woodland exist in all four component woods of the site.
1.2.7 50 East Anglian Plain
1.2.8 51 East Anglian Chalk
1.2.9 52 West Anglian Plain
1.2.10 53 Bedford Greensand Ridge
graphic
1.2.11 54 Yardley-Wittlewood Ridge
graphic
Whittlewood Forest
W.I29-  WHITTLEWOOD FOREST, NORTHAMPTONSHIRE
SP 7342. no ha  
Grade 2
Three relics of this ancient woodland, in the south of the county, still remain. They once formed a link in the chain of woodlands which stretched across the clay belt from Oxfordshire to Huntingdon and Peterborough. Lying on calcareous clays and boulder clays they are typical examples of the woodlands on these soil types. Buckingham Thick Copse is the largest area; it contains fairly uniform oak-ash high forest. Understorey and shrub species are confined to the rides and edges; these include field maple, dogwood, Midland hawthorn and hazel. Sweet chestnut is also present. The ground flora is dominated by Rubus fruticosus, Chamaenerion angustifolium with Deschampsia cespitosa and Brachypodium sylvaticum. Patches of Lusula multiflora and Carex pendula indicate waterlogging. Say's and Smalladine Copses are similar but ash or English elm outnumber the oak in parts. The shrub layer is better developed here and is dominated by hazel. Cornus sanguined, Euonymus euro-paeus and Viburnum opulus are common in the hedgerows.
Lichens that are absent or rare elsewhere in the county are found here; these include Lecanora confusa, Usnea certatina, Opegrapha varia and Pertusaria lutescens.
East and West Ashall's Copses consist of ash scrub and
mature ash woodland and oak is only locally dominant. English elm occurs on the edge and hazel, hawthorn, field maple and Midland hawthorn are present in the understorey and shrub layers. The ground flora here is dominated by bramble interspersed with areas of Deschampsia cespitosa, Oxalis acetosella and Glechoma heeleracea. Other plants include Sanicula europaea, Epipactis helleborine, E. purpurata and Dactylorchis fuchsii.
1.2.12 55 Cotwolds
1.2.13 63 Thames & Avon Vales
1.2.14 64 Midvale Ridge
1.2.15 65 Chilterns
graphic
Burnham Beeches
Grade 2
W.28.   BURNHAM  BEECHES, BUCKINGHAMSHIRE
This woodland occupies a low plateau intersected by shallow valleys, on coarse gravelly sands derived from Reading Beds and areas of superimposed plateau gravel. Structurally the woods are very diverse with ancient pollards, closed stands of younger but mature woodland, old coppice and scrub by open grassland. Beech is the most abundant species, with pedunculate oak, birch and holly also locally abundant. The field layer is sparse, with mainly calcifuge species such as Deschampsia flexuosa, Luzula pilosa, bracken and in open areas heather and other heathland species. Although it is so close to London, it retains a moderately rich epiphytic lichen flora, including Graphis elegans and Thelotrema lepadinum. The rare moss Zygodon forsteri is also recorded. This wood has similarities to the New Forest, but differs structurally and is inferior in extent, diversity and floristics and so is not an alternative site.
su 9585.    450 ha
1.2.16 66 London Basin