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41-607: Wendover Woods is an area of woodland on the north edge of the Chiltern Hills in England. Named after the nearby town of Wendover , the woods are part of the Public Forest Estate and are managed by Forestry England . Covering 325  ha (800  acres ), the woods are a mixture of coniferous and broad-leaved trees . There are several signed walks for recreation, as well as bridleways , picnic and barbecue areas and

82-654: A children's playground . A Go Ape treetop adventure course opened in 2008. There are views of the countryside in the Aylesbury Vale to the north, and a stone monument marking the highest point of the Chilterns which lies within the woods on Haddington Hill . The Aston Hill Mountain Bike Area is at the edge of the woods. 51°46′18″N 0°42′42″W  /  51.77171°N 0.71154°W  / 51.77171; -0.71154 This Buckinghamshire location article

123-861: A fertilizer produced from glauconitic siltstone units belonging to the Serra da Saudade Formation, Bambuí Group, of Neoproterozoic / Ediacaran age. The outcrops occur in the Serra da Saudade ridge, in Alto Paranaíba region, Minas Gerais . It is a silt-clay sedimentary rock, laminated, bluish-green, composed of glauconite (40–80%), potassium feldspar (10–15%), quartz (10–60%), muscovite (5%) and minor quantities of biotite (2%), goethite (<1%), titanium and manganese oxides (<1%), barium phosphate and rare-earth elements phosphates (<1%). Enriched levels of potash have K 2 O grades between 8% and 12%, thickness up to 50 m (160 ft) and are associated to

164-610: A line between Dunstable and Tatsfield and of uncertain extent to the east of London. Outcrops of the Upper Greensand occur in the southwest of England including the Blackdown Hills and East Devon Plateau and the Haldon Hills , remnants of a once much wider extent. The green color of greensand is due to variable amounts of the mineral glauconite , an iron potassium silicate with very low weathering resistance; as

205-404: A result, greensand tends to be weak and friable. It is a common ingredient as a source of potassium in organic gardening and farming fertilisers . Greensand glauconite is used as a water softener for its chemical-exchange properties. Greensand coated with manganese oxide (called manganese greensand) is used in well water treatment systems to remove dissolved (reduced) iron and manganese with

246-470: Is Coombe Hill , 260 m (852 ft.) above sea level. The more gently sloping country – the dip slope – to the southeast of the Chiltern scarp is also generally referred to as part of the Chilterns; it contains much beech woodland and many villages. Enclosed fields account for almost 66% of the " Area of Outstanding Natural Beauty " (AONB) area. The next most important, and archetypal, landscape form

287-442: Is woodland , covering 21% of the Chilterns, which is thus one of the most heavily wooded areas in England. Built-up areas (settlements and industry) make up over 5% of the land area; parks and gardens nearly 4%, open land (commons, heaths and downland) is 2%, and the remaining 2% includes a variety of uses, including communications, military, open land, recreation, utilities and water. The Chilterns are almost entirely located within

328-401: Is a stub . You can help Misplaced Pages by expanding it . Chiltern Hills The Chiltern Hills or the Chilterns are a chalk escarpment in southern England, northwest of London, covering 660 square miles (1,700 km ) across Oxfordshire , Buckinghamshire , Hertfordshire , and Bedfordshire , stretching 45 miles (72 km) from Goring-on-Thames in the southwest to Hitchin in

369-579: Is a more prominent hill, although its altitude is only 249 m (817 ft.). It is the starting point of the Icknield Way Path and the Ridgeway long-distance path , which follows the line of the Chilterns for many miles to the west, where they merge with the Wiltshire downs and southern Cotswolds . To the east of Ivinghoe Beacon is Dunstable Downs, a steep section of the Chiltern scarp. Near Wendover

410-440: Is believed to be Brittonic in origin. According to Eilert Ekwall , Chiltern is possibly related to the broader ethnic name Celt ( Celtæ in early Celtic languages ); the root celto- "high" (and suffix -erno- ) could provide the origin of Chiltern . Before the 18th century, the population lived dispersed across the largely rural landscape of the Chilterns in remote villages, hamlets, farmsteads, and market towns along

451-587: Is made between the Upper Greensand and Lower Greensand. The term greensand was originally applied by William Smith to glauconitic sandstones in the west of England and subsequently used for the similar deposits of the Weald , before it was appreciated that the latter are actually two distinct formations separated by the Gault Clay . The Upper Greensand was also once known as either the "Malm" or "Malm Rock Of Western Sussex". Both Upper and Lower Greensand outcrops appear in

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492-610: Is quite varied, ranging from fertile to fairly sterile. On the fertile soils chestnut and stands of hazel and oak are common, while Scots pine and birch colonise the poorer soils. These Greensand Ridges are popular long distance walking routes, for instance the Greensand Way in Kent. The Lower Greensand (known as the Woburn Sand north of the London Basin ) is of Aptian age. In

533-623: The Chalk Group which underlies the basin; the Gault lies directly on eroded Jurassic or Devonian rocks under much of the area. The Upper Greensand is of Albian age. It represents a sandy lithofacies deposited in areas of stronger currents than the Gault Clay . Like the Lower Greensand it is not present beneath the whole of the London Basin, apparently passing laterally into Gault clay east of

574-1064: The Chiltern Hundreds . By established custom, Members of Parliament (MPs) in the House of Commons of the United Kingdom , who are prohibited from resigning their seats directly, may apply for the Stewardship of the Chiltern Hundreds as a device to enable their departure from the House. Hills in The Chilterns more than 200 metres in elevation and with more than 30 metres of topographic prominence are listed from southwest to northeast. Upper Greensand Greensand forms in anoxic marine environments that are rich in organic detritus and low in sedimentary input. Having accumulated in marine environments, greensands can be fossil -rich, such as in

615-933: The Isle of Wight and the South Downs in the south. In the north, the chalk formations continue northeastwards across Hertfordshire , Norfolk and the Lincolnshire Wolds , finally ending as the Yorkshire Wolds in a prominent escarpment, south of the Vale of Pickering . The beds of the Chalk Group were deposited over the buried northwestern margin of the Anglo-Brabant Massif during the Late Cretaceous . During this time, sources for siliciclastic sediment had been eliminated due to

656-747: The London to Aylesbury Line via Amersham , the West Coast Main Line via Berkhamsted , and the Midland Main Line all run through the Chiltern Hills. The Great Western Main Line and its branches such as the Henley and Marlow branch lines link the southern side of the Chilterns with London Paddington . The Chinnor and Princes Risborough Railway is a preserved line. High Speed 2 (HS2) will pass underneath

697-942: The River Thames drainage basin , and also drain towards several major Thames tributaries, most notably the Lea , which rises in the eastern Chilterns, the Colne to the south, and the Thame to the north and west. Other rivers arising near the Chilterns include the Mimram , the Ver , the Gade , the Bulbourne , the Chess , the Misbourne and the Wye . These are classified as chalk streams , although

738-514: The River Thames , there are no navigable rivers. The Grand Union Canal passes through the Chilterns between Berkhamsted and Marsworth following the course of the Gade and Bulbourne . Also, after crossing a watershed, the Ouzel is partly in the Chilterns. During the Iron Age , the Chiltern ridge provided a relatively safe and easily navigable route across southern Britain. The toponym , Chiltern ,

779-512: The Weald Basin of southern England, underwent structural inversion . This phase of deformation tilted the chalk strata to the southeast in the area of the Chiltern Hills. The gently dipping beds of rock were eroded , forming an escarpment. The chalk strata are frequently interspersed with layers of flint nodules which apparently replaced chalk and infilled pore spaces early in the diagenetic history. Flint has been mined for millennia from

820-559: The AONB. Third, to publish and promote the implementation of a management plan for the AONB. In contrast to National Parks , The Chilterns – as other AONBs – do not possess their own planning authority . The Board has an advisory role on planning and development matters and seeks to influence the actions of local government by commenting upon planning applications . The local authorities (two County Councils, three Unitary Authorities and four District and Borough Councils) are expected to respect

861-518: The Chiltern AONB area. The Board's purposes are set out in Countryside and Rights of Way Act 2000 : In summary these are:- First, to conserve and enhance the natural beauty of the AONB, and increase the understanding and enjoyment by the public of the special qualities of the AONB. Second, while taking account of the first purpose, to foster the economic and social wellbeing of local communities within

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902-449: The Chiltern Hills overlooks the Vale of Aylesbury and roughly coincides with the southernmost extent of the ice sheet during the Anglian glacial maximum . The Chilterns are part of a system of chalk downlands throughout eastern and southern England, formed between 65 and 95 million years ago, comprising rocks of the Chalk Group ; this also includes Salisbury Plain , Cranborne Chase ,

943-537: The Chiltern Hills. They were first extracted for fabrication into flint axes in the Neolithic period, then for knapping into flintlocks . Nodules are to be seen everywhere in the older houses as a construction material for walls. The highest point is at 267 m (876 ft.) above sea level at Haddington Hill near Wendover in Buckinghamshire; a stone monument marks the summit . The nearby Ivinghoe Beacon

984-556: The Chilterns in the Chiltern tunnel . This tunnel, the longest under construction on the HS2 route, will be 16 km (9.9 miles) in length. The Conservation Board has made clear it was opposed to the routing of HS2 through the Chilterns AONB. Bus services are provided by Arriva Shires & Essex and Carousel Buses . Air corridors from Luton Airport pass over the Chilterns. Apart from

1025-750: The Chilterns, including long-distance trackways such as the Icknield Way and The Ridgeway . The M40 motorway passes through the Chilterns in Buckinghamshire and Oxfordshire sections with a deep cutting through the Stokenchurch Gap . The M1 motorway crosses the Bedfordshire section near Luton . Other major roads include the A41 and the A413 . The Chiltern Main Line Railway via High Wycombe and Princes Risborough ,

1066-806: The Lea is degraded by water from road drains and sewage treatment works. The Thames flows through a gap between the Berkshire Downs and the Chilterns. Portions around Leighton Buzzard and Hitchin are drained by the Ouzel , the Flit and the Hiz , all of which ultimately flow into the River Great Ouse (the last two via the Ivel ). Several transport routes pass through the Chilterns in natural or human-made corridors. There are also over 2,000 km (1,200 mi) of public footpaths in

1107-675: The Weald the Lower Greensand consists of four deposits which are partly diachronous : the Atherfield Clay 5–15 m (15–50 ft) thick, the Folkestone Beds 20–80 m (60–250 ft) thick; the Hythe beds 20–110 m (60–350 ft) thick and the Sandgate Beds 2–37 m (5–120 ft) thick. Although it appears both north and south of the London Basin it is not present everywhere beneath

1148-509: The addition of an oxidant, usually potassium permanganate, under controlled pH conditions. It is also used as a type of rock for stone walls in areas where greensand is common. In Roman times in Britain, coarse grits derived from the lower greensand were used to line the inner surface of mortars (grinding bowls) produced in Oxfordshire pottery kilns. Recently, glauconitic greensand has become

1189-466: The area's status as a designated Area of Outstanding Natural Beauty. Examples of historical architecture in the Chiltern region are preserved at the Chiltern Open Air Museum near Chalfont St Giles . This open-air folk museum contains reconstructed buildings which might otherwise have been destroyed or demolished as a result of redevelopment or road construction. The Chilterns include

1230-486: The chalk aquifer is exploited via a network of pumping stations to provide a public supply for domestic consumption, agriculture and business uses, both within and well-beyond the Chilterns area. Over-exploitation has possibly led to the disappearance of some streams over long periods. In a region without building stone, local clay provided the raw materials for brick manufacture. Timber and flint were also used for construction. Mediaeval strip parishes reflected

1271-545: The diversity of land from clay farmland , through wooded slopes to downland. Their boundaries were often drawn to include a section of each type of land, resulting in an irregular county boundary. These have tended to be smoothed out by successive reorganisations. As people have come to appreciate the open country, the area has become a visitor destination and the National Trust has acquired land to preserve its character, for example at Ashridge , near Tring . In places, with

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1312-656: The exceptionally high sea level. The formation is thinner through the Chiltern Hills than the chalk strata to the north and south and deposition was tectonically controlled, with the Lilley Bottom structure playing a significant role at times. The Chalk Group, like the underlying Gault Clay and Upper Greensand , is diachronous . During the late stages of the Alpine Orogeny , as the African Plate collided with Eurasian Plate , Mesozoic extensional structures, such as

1353-609: The glauconitic levels, dark green in color. Glauconite is authigenic and highly mature. The high concentration of this mineral is related to a depositional environment with a low sedimentation rate. The glauconitic siltstone has resulted from a high level flooding event in the Bambuí Basin. The sedimentary provenance is from supracrustal feldsic elements on a continental margin environment with an acidic magmatic arc (foreland basin). In Great Britain , greensand usually refers to specific rock strata of Early Cretaceous age. A distinction

1394-491: The government confirmed that the landscape qualities of AONBs are equivalent to those of National Parks, and that the protection given to both types of area by the land use planning system should also be equivalent. The Chilterns Conservation Board was established by Parliamentary Order in July 2004. It is an independent body comprising 27 members drawn from the relevant local authorities and from those living in local communities within

1435-763: The late- Cretaceous deposits of New Jersey . Important exposures are known from both northern and western Europe , North America , southeastern Brazil and north Africa . Well known and important greensands are the Upper and Lower Greensands of England and occur within Eocene and Cretaceous sedimentary strata underlying the coastal plains of New Jersey and Delaware . Although greensand has been found throughout Phanerozoic and Late Precambrian sedimentary deposits, it appears to be most common in Eocene, Cambrian , and Cretaceous sedimentary deposits. In Brazil , greensand refers to

1476-409: The main turnpike routes which coursed through the navigable valleys. The development of canals in the 18th century and railways in the 19th century encouraged settlement and the growth of High Wycombe , Tring , and Luton . Significant housing and industrial development took place in the first half of the 20th century and continued throughout the 20th century. In 1965 almost half of the Chiltern Hills

1517-474: The northeast. The hills are 12 miles (19 km) at their widest. In 1965, almost half of the Chilterns was designated as an Area of Outstanding Natural Beauty (AONB). The northwest boundary is clearly defined by the escarpment . The dip slope is by definition more gradual, and merges with the landscape to the southeast. The southwest endpoint is the River Thames . The hills decline slowly in prominence in northeast Bedfordshire. The chalk escarpment of

1558-788: The reduction of sheep grazing , action has been taken to maintain open downland by suppressing the natural growth of scrub and birch woodland. In the 1920s and 1930s, the Youth Hostels Association established several youth hostels for people visiting the hills. The hills have been used as a location for telecommunication relay stations such as Stokenchurch BT Tower and that at Zouches Farm . The Chilterns are an Area of Outstanding Natural Beauty (AONB) and so enjoys special protection from major developments, which should not take place in such areas except in exceptional circumstances. This protection applies to major development proposals that raise issues of national significance. In 2000

1599-400: The scarp slopes surrounding the London Basin and the Weald. Prominent seams are to be found in the Vale of White Horse , in Bedfordshire , in Kent , Surrey , the South Downs National Park , elsewhere in Hampshire , the Isle of Wight , and the Jurassic Coast in Dorset . Some minor seams are found further west in Devon in the Blackdown and Haldon hills. The soil of the greensand

1640-522: Was designated as an Area of Outstanding Natural Beauty (AONB). The western edge of the Chilterns is notable for ancient strip parishes , elongated parishes with villages in the flatter land below the escarpment, and woodland and summer pastures in the higher land. The hills have been used for their natural resources for millennia . The chalk has been quarried for the manufacture of cement, and flint for local building material. Beechwoods supplied furniture makers with quality hardwood . The area

1681-455: Was once (and still is to a lesser degree) renowned for its chair-making industry, centred on the towns of Chesham and High Wycombe (the nickname of Wycombe Wanderers Football Club is the Chairboys). Water was and remains a scarce resource in the Chilterns. Historically it was drawn from the aquifer via ponds , deep wells , occasional springs or bournes and chalk streams and rivers. The River Chess directly supplies watercress beds. Today

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