1. A
  2. B
  3. C
  4. D
  5. E
  6. F
  7. G
  8. H
  9. I
  10. J
  11. K
  12. L
  13. M
  14. N
  15. O
  16. P
  17. Q
  18. R
  19. S
  20. T
  21. U
  22. V
  23. W
  24. X
  25. Y
  26. Z
  1. A

    Ancient woodland

    The Ancient Woodland Inventory (Provisional) for England (English Nature 1999 ) defines ‘ancient woodland’ as ‘land that has had continuous woodland cover since at least 1600’.
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    Anglian Glaciation

    The Anglian glaciation occurred between approximately 475,000 and 425,000 years ago. This was the last time that major ice sheets reached East Anglia. There were two subsequent periods of glaciation in the British Isles but the ice sheets did not reach as far south as East Anglia on these occasions. This glaciation deposited a thick layer of glacial till or boulder clay across central Suffolk, radically altering the landscape and the drainage pattern.

    Glaciation timeline

    Glaciation mapsThe Shaping Of Suffolk From An Historical Atlas of Suffolk (1999)

     

    Arthur Young

    1741-1820  Young’s family had an estate at Bradfield Combust in Suffolk and it was there that he started his farming career. His great interest in farming techniques and improvements led him to become one of the most influential agricultural writers of his day. In recognition of this, the government appointed him as Secretary to the Board of Agriculture in 1793. His General View of the Agriculture of the County of Suffolk was published in 1797, with a new edition in 1813.

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  2. B

    Beccles series

    Fine loamy over clayey soils formed from chalky glacial till (qv) which are slowly permeable, but seasonally waterlogged if not underdrained

  3. C

    capability Brown

    Lancelot ‘Capability’ Brown (1716-1783)  - One of the most famous and influential landscape designers of the 18th century, Brown was born in Northumberland and worked on various garden projects in the 1740s before becoming an independent landscape gardener and architect around 1750. Based initially at Hammersmith on the outskirts of London and later at Wilderness House, Hampton Court, he had a thriving nationwide business.

    In Suffolk, he worked at Branches Park, Cowlinge (1763-5 for Ambrose Dickens); Redgrave (1763 for Rowland Holt); Euston Park (1767-9 for the 3rd Duke of Grafton), Ickworth Park (1769-76 for the 2nd Earl of Bristol); and at Heveningham Park (1781-2 for Sir Gerald Vanneck). He was also consulted, in 1782, by Sir Charles Egleton Kent about Fornham Hall, Fornham St Genevieve, but it is uncertain whether any of his ideas were implemented. Brown is also often said to have worked at Elveden c.1766/8-9 for Admiral Keppel, but this is an error – the records indicate that Brown worked for the Admiral’s cousin, General Keppel, at Dyrham in Gloucestershire.Redgrave Hall and park in 1818

     

     

    Redgrave Park 1818

    carr

    A type of wet woodland which occurs on poorly drained or seasonally wet soils and is typically composed of alder, willow or birch

    clay lump

    An East Anglian building technique that used large, unfired, clay bricks set in a clay mortar. The bricks were made of local clays mixed with chopped straw, shaped using a simple wooden mould and air-dried. The sizes could vary from about 22 x 12 x 5 inches to 18 x 6 x 6 inches. The wall surfaces were originally finished with a clay plaster, which was often tarred for weatherproofing and then sanded to take a colour-wash, but by the 1920s cement rendering was the most frequent surface treatment.  In some cases the clay lumps were hidden behind a brick facing. A brick or stone plinth was usual to give the blocks a dry foundation

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    One of Copinger Hill’s clay cottages in Buxhall

    Clay Lump cottage at Buxhall

    clunch

    A form of hard chalk used as a building stone. The mains sources of this material were on the north-west edges of Suffolk – at Lakenheath on the fen-edge, at Thetford in Norfolk and at Burwell (‘Burwell stone’), Orwell and Barrington (‘Barrington stone’ a grey-green variety with glauconite) in Cambridgeshire. lthough hard enough to be worked into blocks, it was still susceptible to rapid weathering if exposed. So, for external walls, its use was mainly limited to vernacular buildings in its source areas, as can be seen in Lakenheath. In many cases it was combined with flint or brick to make more durable structures But it was also more widely used in medieval church interiors, where the material’s softness could be protected from weathering and exploited for richly carved decoration, as in Wingfield church.Clunch wall at Lakenheath

     

    Clunch wall

    coastal squeeze

    Occurs where fixed sea defenses prevent the natural migration of saltmarsh inland as estuaries become subject to sea level rise

    co-axial

    A field system with one prevailing axis of orientation. Most of the field boundaries either follow this axis (axial boundaries) or run at right angles to it (transverse boundaries). This type of landscape can be most clearly seen on old maps of the South Elmhams and IIketshalls in north-east Suffolk. Unfortunately this area suffered from a high rate of hedgerow removal in the 20th century and the patterns are now much weakened.
     

    colour-washed

    This refers to the ‘washing’ or painting of the walls of buildings with plastered or rendered surfaces with coloured paint. Today this is done with modern masonry paints in a variety of colours, but in the past distemper or limewash were used.  Distemper consists of whiting (ground chalk) mixed with size (weak glue) and water, while limewash consists of slaked lime and water. Both could be used uncoloured as ‘whitewash’ or coloured with pigments. Earth pigments such as red or yellow ochre were most common, giving a range of colour from cream through pink to red. Tales of the use of animal blood in colour washes are probably apocryphal, but sloe juice may have been used.  

    Documentary evidence suggests that, up to about 1900, most house walls were either left a raw ‘plaster white’ or given a coat of whitewash. There was then a gradual increase in the use of colours – firstly creams and pinks, with brighter colours such as lavender, orange and red being mentioned by the 1930s. By the 1970s there were authoritative statements about a traditional ‘Suffolk pink’ house colour. In part this might be confusion with ‘pinking’, a technique of decorating exterior plasterwork with lightly incised marks that is mentioned as being prevalent in north Suffolk in the 1920s. The commercial marketing of ‘Suffolk Pink’ as a colour has also undoubtedly been a factor in its perception as a long-established tradition.

    A preservative brown staining used on weather-boarded barns and farm buildings is mentioned in 1783 and red-painted timber barns can be seen in John Constable’s pictures, such as his 1815 view of Golding Constable’s flower garden in East Bergholt.  A red barn also features in the infamous murder of Maria Marten at Polstead in 1827. It is probable that these timber stains and paints were oil-based rather than washes. By the 1830s, it was an established practice to give timber-clad barns a preservative coating of tar and by the end of the 19th century black-tarred farm buildings of timber, clay-lump or clunch were a common sight in the landscape.

    Commons

    Land in communal use. Most frequently this is grassland or heathland used for animal grazing (see also greens and tyes), but the term can also be applied to arable, meadows or woods. Historically, the soil of the commons belonged to the manorial lords, but its use was subject to the common rights of the tenants. The number and definition of the common-right holders varies from common to common, but is often limited to the properties bordering a particular common. The pasturing of a set number of animals (variously called a beast-going, gate, share or stint ) is the most frequent common right, but additionally the tenants could have rights to take firewood (estover), timber for ploughs, gates or house repairs (bote), to dig for peat for fuel (turbary) or for ‘stone’ for road repairs. 

    Since the Commons Registration Act of 1965, greens and commons have become legally distinct: commons are subject to communal grazing rights, but greens are used for exercise or recreation – but in the past the terms were interchangeable.

    South Elmham Green

     

     

     

    Sth Elmham Common

    coppiced

    Trees cut down to ground level and then allowed to regenerate. Most native trees, with the notable exception of pines, will regenerate from stumps (stools) or will send up suckers from the root system (notably elms).The vigour of an established root system will quickly send up a number of fast-growing shoots that will produce a crop of straight poles that can be used for fencing, wattle-work and fuel. The poles are harvested at intervals and allowed to re-grow again. The process can go on indefinitely and in many woods the oldest trees are the coppice stools – some may be as much as 1000 years old.One problem with coppicing is that the young shoots are vulnerable to attack from grazing animals, so they need to be excluded from recently coppiced areas.

    cursus

    18th-century antiquarians borrowed this Latin term, meaning a ‘racecourse’, to describe a particular type of Neolithic (qv) monument, exemplified by the Dorset Cursus, the largest and best-preserved of them. This consists of a very elongated enclosure that is 10km (6¼ miles) long but only 82m wide, marked by parallel earthen banks with external ditches. However most cursuses are now only visible as cropmarks, their banks having been flattened long ago. Through aerial photography over 150 have now been recorded, the majority occupying low-lying positions beside rivers and streams. In eastern England, Cambridgeshire has 5 or 6, Suffolk has 3, and Essex and Norfolk have one each. The Suffolk examples are beside the River Lark at Fornham All Saints (1.9km or 1.2 miles long x 25-40m wide), and two beside the River Stour, one at Stratford St Mary (290m long x 68m wide) and a smaller one at Bures St Mary (190m+ long x 24m wide).

    The characteristic straight sides of these monuments suggest that they were laid out in areas already cleared of forest to give an open countryside that allowed clear viewpoints. Their purpose is not fully understood, but a ceremonial or ritual use is most likely, and this could have included races or processions. Many have concentrations of cropmark rings around their terminals, which are either flattened burials mounds or other ritual monuments. Excavations on the cursus at Springfield in Essex revealed a circular setting of posts, 26m in diameter, at one end and small pits nearby contained sooty deposits and cremated animal bones. In general, these monuments date from c.3,500-3,000 BC and the example at Fornham appears to overlie an earlier Neolithic ritual monument in the form of a causewayed enclosure.Plan of the Neolithic cursus and other cropmarks at Fornham All Saints

     

     

    Fornham All Saints Cursus

  4. D

    decoy

    Duck decoys are ponds or other bodies of water designed to attract and trap wildfowl. Attached to the ponds are a number of narrow curving channels, known as pipes, which were covered with nets; wildfowl were lured into these and captured. A particular distinctive form of decoy, known as the ‘skate’s egg’ form has a rectangular pond with a curving pipe at each corner.
     
    Decoys were very much a feature of eastern England, with the largest numbers being recorded in Lincolnshire, Norfolk, Suffolk and Essex. In 1886 Suffolk had the largest number of working decoys in the country, with a concentration in the coastal areas. But a decline soon set in and today very few are in working condition.
     
    The idea for decoys seems to have been imported from Holland in the early 17th-century, with the earliest English decoys dating from around the 1620s. The decoy at Friston is probably of 17th-century origin, making it contemporary with the oldest in England.The Friston decoy in 1882, showing its ‘skate’s egg’ plan

     

    Friston Decoy

    deer parks

    Areas enclosed for the farming and, sometimes (depending on their size) the hunting of deer to provide venison for lordly elites. The parks often have rounded outlines, defined by earthen banks and ditches, supplemented by expensive wooden fences called pales.
     
     The interiors usually contained a mixture of woodland and open glades or launds. Medieval deer parks were often created from existing woodland or land that was for unsuited for agriculture. Parks could also include other sources of high status foods, such as rabbits from warrens, fish and waterfowl from ponds, and doves from dovecotes. Park keepers and visitors were accommodated in lodges within the parks.Staverton Park
     

     

     

    Staverton Park

    Droveway

    Roads or tracks used by farmers to move their animals between pastures or fields. Sometimes these can take the form of metalled roads with wide grass verges, while others have minimal or no hard surfacing. They are usually defined by ditches and/or hedges on either side

  5. F

    flushwork

    A decorative use of flint on the walls of buildings. In this the flints are knapped to expose the inner colour of the flint (usually black, but sometimes grey or brown) and set in the walls with the flat smooth surface outermost. In some cases the flints are shaped into squares to fit together to make large smooth panels. In others the flints are fitted into recesses in limestone blocks to make patterns and lettering, the black knapped flints contrasting with the white of the limestone (the flints are fitted to be flush with the surface of the limestone, hence the term flushwork). In a minority of cases the flints are combined with bricks.Flushwork appears suddenly in the early 14th century, with the gatehouse of Butley Priory being both one of the earliest and most magnificent examples. It was used extensively in the 15th and early 16th centuries on churches throughout East Anglia.A detail of the flushwork on the Butley Priory gatehouse, dating from c.1310-23

     

     

     

    Butley Priory Gatehouse

  6. G

    Gipping divide

    The area to the south of the Gipping valley has an undulating landscape which had (and still has) a high potential for arable farming in pre-modern times, while to the north the landscape is much flatter and less well-drained, making it more suited to pasture and dairy farming.  

    The ‘Gipping divide’ has also been recently recognised as being a significant historic cultural boundary. The areas on either side differ in the proportion of land formerly held in common fields, in the way their vernacular buildings were constructed and laid out, in their terminology for common pasture and woods and in their inheritance customs (for more detail, see: E. Martin & M. Satchell, Wheare most Inclosures be. East Anglian Fields: History, Morphology and Management, East Anglian Archaeology 124, 2008). The patterns seen in south Suffolk extend into Essex and those in north Suffolk extend into Norfolk, indicating that this was a boundary of regional importance that has a greater cultural significance than the existing county boundaries.
     

    glacial till

    Also called Lowestoft Till or chalky boulder clay, this is a chalky bluish-grey to brown clay that is variably silty, sandy and stony. Chalk fragments and flints are ubiquitous, with occasional sandstone erratics and fossils such as belmnites . The material was deposited by the retreating glaciers of the Anglian Glaciation (qv) and covers a broad diagonal band across central Suffolk, extending from Haverhill to Lowestoft. The deposit is thickest in the Chedburgh/Rede area where thicknesses in excess of 50m have been proved by boreholes

    Greens

    Traditionally, this was a term used to describe an area of grassland used for communal grazing by a defined group of common-right holders (see commons). Greens were (and sometimes still are) fringed by the houses and farmsteads of the common-right holders. Archaeological evidence suggests that some greens started to be established in the 11th century, but with greater numbers following in the 12th and 13th centuries. The largest greens, up to about 530 acres in extent, were on the wide and poorly-drained clay interfluves (qv) of north Suffolk. Many greens were enclosed in the 18th and early 19th centuries, but often their outlines survive as ‘ghosts’ in the landscape. The surviving greens frequently have great biodiversity value as areas of undisturbed ancient grassland.Since the Commons Registration Act of 1965, greens and commons have become legally distinct: commons are subject to communal grazing rights, but greens are used for exercise or recreation – but in the past the terms were interchangeable. In south Suffolk, the term tye (qv) is a synonym for a greenChippenhall Green

     

    Chppenhall Green

  7. H

    hall-and-church

    In the Suffolk landscape there is a recurrent pairing of medieval churches and manorial halls, usually in prime valley side locations close to a water supply. The halls were often surrounded by water-filled moats in the 13th or 14th centuries as an indication of their status, but the actual ‘hall-and-church’ clusters are probably older. Evidence from Suffolk and elsewhere in England suggests that these clusters originate in the Late Saxon period (c.AD 850-1066), when the possession of a church was one of the indicators of thegnly rank. These complexes often consist of a roughly square area that contains a church in one quarter, as at Wattisham. These could well be the hitherto elusive Late Saxon thegnly fortifications called burhs. If so, the defences were fairly minimal, perhaps just a ditch and fence, but with perhaps an accent on the entrance – the burhgeat (‘fort gate’) referred to in the 11th-century list of the qualifications for thegnly status. In some cases the clusters have grown into hamlets or villages, but others have remained as small units.Brockley Hall and Church

     

     

     

    Brockley hall and church

    Hanslope

    Slowly permeable chalky clayey soils formed from chalky glacial till

    Hoxnian

    This was a warm period, c.425,000 to 390,000 years ago, between the Anglian and Wolstonian glaciations. It is termed the Hoxnian Interglacial after important deposits of this date at Hoxne in north Suffolk.

    Glacial timeline

    Humphry Repton

    1752-1818  Born in Bury St. Edmunds, Repton later moved to Norfolk and Essex, where he set himself up as a ‘landscape gardener’ (a term he coined) in 1788. He famously produced ‘Red Books’ detailing his landscape designs for his clients.
     
    In Suffolk he produced Red Books for: Shrubland Hall, Barham/Coddenham (1789 for Sir William Middleton); Culford Hall (1791 for the 2nd Earl Cornwallis); Glemham Hall, Little Glemham (1791 for Dudley North); Glevering Hall, Hacheston (1791 [or 1793] for Chaloner Arcedeckne); Henham Park (1791 for Sir John Rous); Livermere Park (1791 for Nathaniel Lee Acton); Broke Hall, Nacton (c.1792 for Philip Bowes Broke); Tendring Hall, Stoke-by-Nayland (1791 for Sir William Rowley); and Wherstead Park (c.1792-4 for Sir Robert Harland).
     
    He also published 3 books: Sketches and Hints on Landscape Gardening (1795), Observations on the Theory and Practice of Landscape Gardening (1803), and Fragments on the Theory and Practice of Landscape Gardening (1816).Livermere Hall and park in 1818  More...

     

     

     Livermere Hall

  8. I

    Interfluves

    Literally ‘between rivers’, this term refers to the areas between river valleys or major water courses. These are higher than the valley floors and can be either ridges or more extensive plateaux. The wider interfluves may have significant water problems, either a lack of it, as on the sandy soils of the Breckland or the Sandlings, or too much, as in some parts of the clayland plateaux where the gradient is slight or where there are actually concave depressions, resulting in poor drainage. 

  9. L

    lacustrine

    Freshwater lake deposits fine-grained soils resulting from material brought into freshwater lakes by streams or rivers

    Land Description Unit

    The basic land units used in this landscape character study. The area within each unit or polygon has a relatively homogenous character, defined by four principal attributes: physiography, ground type, landcover and cultural pattern. These are derived from six mapable datasets: relief, geology, soils, tree cover, farm type and settlement.

    Landscape type

    Landscape character types (LCT) are landscapes with broadly similar patters of natural and cultural chracteristics found in a range of locations. Whereas landscape character areas are geographically descreet areas of one landscape type, or in some methodologies may contain several diffrent landscape types.

    loess

    A fine-grained, silty, pale yellow or buff, windblown (aeolian) sediment derived from either glacial or glacial outwash deposits, where glacial activity has ground the parent materials into a very fine ‘rock flour’. Loess deposits often give rise to very rich soils. In Suffolk, loess deposits are particularly notable in the Felixstowe and Shotley peninsulars.

  10. M

    Martello Towers

    A string of towers (of which ten survive) built 1808-12 from Aldeburgh southward to Shotley to defend the coast against Napoleon. Held to be named after a prototype at Mortella Point in Corsica, however Italian coastal watch towers were also known as 'Torre di Martello' or 'Hammer Towers' in which a hammer was used to strike a bell to warn of the approach of pirates. The most northerly of Suffolk’s Martello Towers is at Slaughden, at the south end of Aldeburgh. This was built 1810-12 and has a unique quatrefoil plan. ©M Farrow

     

     

     

     

    The Tower at Slaughden

    moat

    A moat is a broad water-filled ditch that surrounds a central platform or 'island' where a house usually placed. Although inspired by castles, the defensive banks and walls of true castles are characteristically absent on moated sites. The possession of a defended residence was closely linked in the medieval mind with concepts of lordship and social status: great lords had their castles, lesser members of the free classes (knights, esquires, clergy and freehold farmers) had, where conditions were suitable, moated houses.

    A social hierarchy is apparent in the size of moats: those that are an acre or more in extent tend to be manorial (e.g. Brockley Hall) or monastic (e.g. Flixton Priory). Moats of about half an acre in size are much more likely to be associated with parsonages (e.g. The Old Rectory, Whatfield) or farms that are ancient free tenements (e.g. Oak Tree Farm, Hitcham).

    The majority of moats function like ponds, relying on an impervious base or lining, though some are connected to water-courses. Suffolk has over 850 moats and vies with Essex for the distinction of having the largest number