Furner's Green | |
---|---|
Location within East Sussex | |
OS grid reference | TQ409262 |
• London | 33 miles (53 km) N |
Civil parish | |
District | |
Shire county | |
Region | |
Country | England |
Sovereign state | United Kingdom |
Post town | UCKFIELD |
Postcode district | TN22 |
Dialling code | 01825 |
Police | Sussex |
Fire | East Sussex |
Ambulance | South East Coast |
UK Parliament | |
Furner's Green is a hamlet in the civil parish of Danehill in East Sussex, England.
Furner's Green lies on the Greenwich Meridian about 9 miles (14 km) north-west of Uckfield and approximately 7 miles (11 km) to the east of Haywards Heath on the southern edge of Ashdown Forest.
Lime kilns at Annwood Farm ('Handwood Farm' on the 1795 Ordnance Survey map) are shown on the 1875 Ordnance Survey map. Lime would have been used locally to improve the heavy, clay-rich Wealden soil, in the mixing of mortar for construction, and was also used in Sussex for plasterwork and 'white washing'. There is no evidence of limestone outcropping in this area, but Sussex does have small workable outcrops of 'Sussex Marble' or 'Winklestone' and so it is likely that chalk was imported to this location from the chalk workings of the South Downs. The abundance of local timber in the nearby Annwood and Maskett's Wood would have been invaluable for lime manufacture [1]
In William Gardener's 1795 map of Sussex (1 inch to a mile scale), which was to some part based on the findings of an earlier (1778) survey by himself and Thomas Yeakell, Furner's Green is called 'Turners Green'. [2] A later anomaly can be found in the 1879 recollections of Thomas Chatfield, a long-time resident of the area, who is reported to call the hamlet 'Furriers Green' [3]
Colin Godman's Farm has been traced back to at least 1550 and reputedly was for a while involved in the smuggling of wool for export. It, and other substantial properties are clearly marked on the 1875 Ordnance Survey map. [4] John Baker-Holroyd (later Baron Sheffield) is noted as owning the property in 1768 records [5]
The iron workings at Sheffield Mill are reported in detail by John Shreve, master of works during the reigns of Henry VIII and Edward VI. [6]
A lease agreement dating to 1580 refers to the 'decaied Ironworks, sometimes called the furnes for the casting of raw iron there'. On the site there is also a 'corne' mill. The degree of development at Sheffield Mill, simply for grinding corn, was substantial at that time, for mention is made of 'banks, baies, ponds, waters, watercourses, waterlaies, fludgates and waterworcks'. The hammer mill and forge required waterwheels, bellows, coal houses and places in which to work the material. And yet, to visit the site now, evidence of this industrial history is almost gone.
Before selling of properties in the early to mid twentieth century, many of the properties in Furner's Green were part of the Sheffield Park or Danehurst estates.
The Weald is an area of South East England between the parallel chalk escarpments of the North and the South Downs. It crosses the counties of Hampshire, Surrey, Sussex and Kent. It has three separate parts: the sandstone "High Weald" in the centre; the clay "Low Weald" periphery; and the Greensand Ridge, which stretches around the north and west of the Weald and includes its highest points. The Weald once was covered with forest, and its name, Old English in origin, signifies "woodland". The term is still used today, as scattered farms and villages sometimes refer to the Weald in their names.
The South Downs are a range of chalk hills that extends for about 260 square miles (670 km2) across the south-eastern coastal counties of England from the Itchen valley of Hampshire in the west to Beachy Head, in the Eastbourne Downland Estate, East Sussex, in the east. The Downs are bounded on the northern side by a steep escarpment, from whose crest there are extensive views northwards across the Weald. The South Downs National Park forms a much larger area than the chalk range of the South Downs and includes large parts of the Weald.
Birdsedge is a small village in the borough of Kirklees in West Yorkshire, England, on the edge of Yorkshire's Pennine Hills, standing just below 1,000 feet (305 m) above sea level. It is approximately 6 miles (10 km) south-east from Huddersfield and about 4 miles (6 km) north-west from Penistone, between the villages of Shepley and Upper Cumberworth and is linked with the neighbouring hamlet of High Flatts, a former Quaker settlement.
Lindfield is a village and civil parish in the Mid Sussex District of West Sussex, England. The parish lies 1 mile (2 km) to the north-east of Haywards Heath, of which the village is a part of the built-up area. It stands on the upper reaches of the River Ouse. The name 'Lindfield' means 'open land with lime trees.'
Brightling is a village and civil parish in the Rother district of East Sussex, England. It is located on the Weald eight miles (13 km) north-west of Battle and four miles (6 km) west of Robertsbridge.
Plumpton is a village and civil parish in the Lewes District of East Sussex, England. The village is located five miles (8 km) north-west of Lewes. The parish measures 6.5 miles in length on its north–south axis and 1 mile at its widest on the B2116 Underhill Road. The southern half of the parish lies within the South Downs National Park and at the highest point, 214m (702 feet), the South Downs Way traverses the crest of Plumpton Plain. The parish includes the small village of Plumpton adjacent to the Downs and to the north the larger village of Plumpton Green where most of the community and services are based. Plumpton is known for its race course, and also Plumpton College, which farms over 2500 acres of land and has become one of the leading centres for land-based education in the UK.
Fulking is a village and civil parish in the Mid Sussex District of West Sussex, England. The parish lies wholly with the South Downs National Park.
The Blackburn Brook is a stream in Sheffield, South Yorkshire, England which flows through the Blackburn Valley along the M1 and Ecclesfield Road and joins the River Don near the Meadowhall shopping centre. Downstream from the A61 road at Chapeltown the Blackburn Brook is defined as a main river by the Environment Agency, which requires new building development to be at least 26 feet (8 m) from the bank side as a flood defence measure and to allow access to the watercourse for maintenance.
Warnham is a village and civil parish in the Horsham district of West Sussex, England. The village is centred 2 miles (3.2 km) north-northwest of Horsham, 31 miles (50 km) from London, to the west of the A24 road. Other named settlements within the parish include the hamlets of Goosegreen, Kingsfold and Winterfold as well as parts of Strood Green and Rowhook. The area is in the northwest of the Weald, a gently sloped remnant forest in southeast England and largely a plain by erosion.
Oldland Windmill is an 18th-century post mill situated near the village of Keymer, West Sussex, England.
The Medway and its tributaries and sub-tributaries have been used for over 1,150 years as a source of power. There are over two hundred sites where the use of water power is known. These uses included corn milling, fulling, paper making, iron smelting, pumping water, making gunpowder, vegetable oil extraction, and electricity generation. Today, there is just one watermill working for trade. Those that remain have mostly been converted. Such conversions include a garage, dwellings, restaurants, museums and a wedding venue. Some watermills are mere derelict shells, lower walls or lesser remains. Of the majority, there is nothing to be seen.
The Hampshire Basin is a geological basin of Palaeogene age in southern England, underlying parts of Hampshire, the Isle of Wight, Dorset, and Sussex. Like the London Basin to the northeast, it is filled with sands and clays of Paleocene and younger ages and it is surrounded by a broken rim of chalk hills of Cretaceous age.
The western Weald is an area of undulating countryside in Hampshire and West Sussex containing a mixture of woodland and heathland areas.
The geology of East Sussex is defined by the Weald–Artois anticline, a 60 kilometres (37 mi) wide and 100 kilometres (62 mi) long fold within which caused the arching up of the chalk into a broad dome within the middle Miocene, which has subsequently been eroded to reveal a lower Cretaceous to Upper Jurassic stratigraphy. East Sussex is best known geologically for the identification of the first dinosaur by Gideon Mantell, near Cuckfield, to the famous hoax of the Piltdown man near Uckfield.
Brooks Green is a hamlet in the Shipley civil parish of the Horsham District of West Sussex, England. It is in the north-west of the parish, approximately 2 miles (3 km) from the parish village of Shipley, and 4.5 miles (7 km) south-west from the district town of Horsham. The hamlet is within the Southwater South and Shipley ward for West Sussex County Council.
Cocking Lime Works and its associated chalk quarry are abandoned industrial sites in the South Downs of England. They are to the south of the village of Cocking, West Sussex, close to the South Downs Way. The works are on land owned by the Cowdray Estate and are not open to the public. Cocking was the source of lime used for the manufacture of Midhurst White bricks and for agricultural purposes.
The geology of Kent in southeast England largely consists of a succession of northward dipping late Mesozoic and Cenozoic sedimentary rocks overlain by a suite of unconsolidated deposits of more recent origin.
The geology of West Sussex in southeast England comprises a succession of sedimentary rocks of Cretaceous age overlain in the south by sediments of Palaeogene age. The sequence of strata from both periods consists of a variety of sandstones, mudstones, siltstones and limestones. These sediments were deposited within the Hampshire and Weald basins. Erosion subsequent to large scale but gentle folding associated with the Alpine Orogeny has resulted in the present outcrop pattern across the county, dominated by the north facing chalk scarp of the South Downs. The bedrock is overlain by a suite of Quaternary deposits of varied origin. Parts of both the bedrock and these superficial deposits have been worked for a variety of minerals for use in construction, industry and agriculture.
Upper Rapeland Wood is a mixed mature woodland in Old Holbrook, a hamlet close to Horsham, England. It lies on Rapeland Hill, on the north-western fringes of Old Holbrook, 1.2 miles (1.94 km) north of the A264 dual carriageway. It is directly opposite Northlands Copse, an area of ancient woodland and a partially managed plantation in the neighbouring hamlet of Graylands.