70-642: The Hog's Back is a hilly ridge, part of the North Downs in Surrey , England. It runs between Farnham in the west and Guildford in the east. Compared with the main part of the Downs to the east of it, it is a narrow elongated ridge, hence its name. Jane Austen , in a letter to her sister Cassandra dated Thursday 20 May 1813 from her brother's house in Sloane Street, wrote of her journey to London in
140-522: A curricle via "the Hog's-back" This shows that it was known as the Hog's Back by Jane Austen's time. However, the medieval name for the ridge was Guildown (recorded first in 1035 where it was the site of the abduction of Prince Alfred of Wessex by Earl Godwin and then in the Pipe Rolls for 1190 and onwards) but this name is no longer in use. However, the name Guildown is evoked by Guildown Road,
210-486: A landscape similar to that found in Normandy known as bocage . The predominant type of farming on the Downs is arable farming; this increased greatly during the 20th century. Pastoral farming also occurs but to a lesser extent. Human settlements within the Downs have generally formed in sheltered valleys and at the foot of the scarp slope (known as spring line settlements). In recent years vineyards have been planted along
280-678: A large hill which exceeds it – as such is part of the Surrey Hills Area of Outstanding Natural Beauty . The name, Seale, may derive from the Old English word for "hall" or, alternatively, for "willow" (see for example Salfords ). . Also possibly, a Viking word meaning, "to the pig", (in references to the Hog's_Back ). The Sands is not a relatively old name for any part of Seale, first recorded in Tudor period records, and derives from
350-471: A little below the high point occupied by the original carriageways, were added in the early 1970s. Roughly midway along the ridge of the Hog’s Back between Farnham and Guildford (OS grid reference SU911483), the human remains of at least six skeletons were discovered in 1935 when ground was being dug for a new water pipe. They were buried less than a yard from the then-northern edge of the road (now part of
420-534: A mansion known as Poyle Hill Lodge. This was once one of the Admiralty semaphore stations because of its high vantage point. In 1935 it became the Hog's Back Hotel, initially owned by the Guildford Friary Brewery, and it remains a hotel, now officially known as the Hog's Back Hotel and Spa, Farnham. On the south side of the Hog's Back, a little to the east of Poyle Hill, another large mansion
490-529: A mix of rubble and viscous mud, which may be washed downhill, further eroding the landscape (a process known as solifluction ). Since chalk contains a very high percentage of calcium carbonate , it can be dissolved by both groundwater and rainwater. Across much of the North Downs, the chalk dips below the London Clay at a relatively shallow angle (c. 18° near Dorking), however at the far west of
560-610: A private house. The village is well connected by roads but not rail and had approximately 50% of its working population recorded in 2011 as commuting 20–40 km, living in the rural outer Metropolitan Green Belt yet commuting to major employment areas such as London, Farnborough , Fleet and Aldershot . Specific long-distance roads are the A31 and the A331 roads (the Blackwater Valley Route) dual carriageway; along
630-399: A public place), but recently (2012–13) Guildford police and local residents are curbing these practices. Towards Guildford, on the north-east side of the Hog’s Back, lie Down Place and Blackwell Farm. The manor of Down Place was demolished in 1963, all that remains today of the estate are the stables where is established Hogs Back Books , the children’s book publisher. Once associated with
700-526: A residential road that climbs the southern side of the ridge on the southwestern fringes of Guildford. The Guild- element of Guildown is the same as that found in Guildford, meaning "gold". Various explanations have been suggested for the relationship between the names of Guildown and Guildford. Guildown may be an abbreviation of Guildford Down ("the Down by Guildford"). The Hog's Back ends at Guildford, which
770-621: A roundabout road system centred on the Friary Centre (named after the medieval Dominican Friary there) has also broken up this direct stretch of road at the point that it reaches Guildford, where it ends at the junction with the A3. When the idea of the Pilgrims' Way to Canterbury was popularised in the nineteenth century, a route over the southern slopes of the Hog's back, parallel with the ridgeway and running through Seale and Puttenham ,
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#1732797738347840-407: Is The Lyttons, a Grade II listed house which stands next to the churchyard but away from the road. This was originally an open hall house as shown by blackened rafters and the oldest parts of the fabric have been dated to the early 1500s. A brick chimney was inserted and the open hall was divided into an upper and lower storey by the insertion of an upper floor in the 1600s. The next oldest building
910-517: Is absent. The alkaline soils are thin and nutrient poor, which prevents deeper-rooted lush grasses (with a high water demand) from dominating. Each square metre of chalk downland may support up to 40 different species. This semi-natural habitat is maintained through sheep, cattle and rabbit grazing which prevents scrub encroachment. Chalk grassland to the west of the Medway Valley is dominated by upright brome and fescue , whilst grassland to
980-739: Is an early 20th-century merger of land formerly owned by the Long family, land formerly that of Seale Lodge, and agricultural and parkland formerly comprising the Great Down estate, centred on another mansion at the top of the Hog's Back, Great Down, which was demolished in the 1950s. The Hampton Estate was acquired by Eustace Thornton in 1929. He was succeeded by his son, Sir Richard Thornton, KCVO , OBE , Lord Lieutenant of Surrey 1986–1997 and then by Sir Richard's daughter and son-in-law, Bridget and Bill Biddell. The 1873, rubblestone built, stone dressed , Grade II listed building in its listed park in
1050-576: Is an independent real ale brewery based in Tongham , which is a village just below the Hog's Back. The Hog's Back Cafe is in a layby on the Guildford to Farnham (westbound) carriageway of the A31 along the Hog's Back, between the turn offs to Puttenham and Seale . It is popular with lorry drivers, who use the cafe and toilets during the day. The hillside adjacent to the A31 layby was a popular site for dogging (viewing or participating in sexual relations in
1120-524: Is considerable evidence of Mesolithic activity in the Surrey Downs through the discovery of pit-dwellings at Weston Woods near Albury and the quantity of discarded tools, microliths and other implements discovered. In about 3000 BC the emergence of Neolithic culture saw the lifestyle of the Mesolithic hunter-gatherers shift to a more sedentary and communal lifestyle that relied upon
1190-660: Is mentioned in: North Downs The North Downs are a ridge of chalk hills in south east England that stretch from Farnham in Surrey to the White Cliffs of Dover in Kent . Much of the North Downs comprises two Areas of Outstanding Natural Beauty (AONBs): the Surrey Hills and the Kent Downs . The North Downs Way National Trail runs along the North Downs from Farnham to Dover . The highest point in
1260-459: Is nearby East End Farm, another Grade II listed building which dates from the later part of the 1500s: about 1560-1580 compared with the Lyttons' dating of circa 1520-1550. Adjacent to the church are 17th and 18th century joined buildings, known as Manor Farm, converted into craft shops and a tea room. Manor Farm Cottages, and Seale Lodge Cottages stand opposite the church, clustered around
1330-632: Is now demolished and its lands subdivided in the twentieth century – an interior from Poyle Park is on display in the Museum of London . Hampton Lodge (below) was originally a hunting lodge, occupied by the wealthy Long family. In the 19th century, it passed through a female line into the hands of a branch of the Howard family of the Dukes of Norfolk (and Earls of Surrey) who took up residence and enlarged their estate by acquisition until it became, from about 1918,
1400-624: Is on the northern side of the same hill. East of the Medway Valley the Downs become broader and flatter, extending as far as the Isle of Thanet . The ridge of the North Downs is intersected by the valleys of a series of rivers: the Wey , Mole , Darent , Medway and Stour . These drain much of the Weald to the south. The western rivers are tributaries of the Thames ; they have carved steep valleys through
1470-663: Is the point where the River Wey cuts through the North Downs. Alternatively, both Guildown and Guildford may derive independently from a gold-coloured feature; either the yellow flowers of the marsh marigold or the gold-coloured (sandy) soil of the hillside. The Hog's Back has a minimum prominence (drop) of 55 metres (180 ft), reaching 154 m (505 ft) above sea level, the 24th highest hill in Surrey. Along its course are half panoramas north and south separated by less than 100 m (330 ft) viewable from paths alongside
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#17327977383471540-417: Is the surface representation of a monoclinal fold , where once horizontal chalk beds have been folded into steeply sloping layers. Across much of the North Downs, the angle of the chalk as it disappears below the surface is relatively shallow (c. 18° near Dorking ), however at the Hog's Back, local faulting has produced a much steeper angle (up to 55°). To the north of the ridge lies the London Clay , and to
1610-475: Is very little archaeological evidence in support, it has been suggested that a Roman road ran from London to Winchester and that, at this point, it passed, either over the Hog's Back or perhaps a little to the north (e.g. Roman Surrey , David Bird, 2004). Research on this is continuing. According to the Victoria County History of Surrey (volume 3, published 1911, p 374, s.v. Wanborough ),
1680-455: The Devil's Punchbowl . The road along the Hog's Back is ancient, since its raised position offered travellers a vantage point and also kept them above the thick ancient woodland of the valleys on either side. It was part of the ancient ridgeway which runs from Wiltshire down to the east coast of Kent. It was also part of the road from London to Winchester (as it still is). Although there
1750-560: The Hog's Back . Much chalk grassland and ancient woodland on the Downs is open-access, and there are also many historic sites such as Kit's Coty House (near Maidstone) and Dover Castle . The topography of the North Downs means there are relatively few summits with topographic prominence . Below is a list of summits on the North Downs which are more than 180 metres in height with 30 metres of topographic prominence (a commonly used threshold in Britain). The summits are arranged in order along
1820-645: The Bishops of Winchester "for three lives" from 1839 (although they sold this interest in 1856). From the Tudor period , as evidenced by memorials in Seale church, the main landowner was the Woodroffe family (of whom two, David and Nicholas, father and son, were Sheriffs of London in 1554 and 1573 respectively), and later, by descent through a female line, the Chester family. They were seated at Poyle, Tongham , on
1890-643: The Cretaceous, the sea covering the south of England began to retreat and the land was pushed higher. The Weald (the area covering modern day south Surrey, south Kent and north Sussex) was lifted by the same geological processes that created the Alps , resulting in an anticline which stretched across the English Channel to the Artois region of northern France. Initially an island, this dome-like structure
1960-416: The Downs has been greatly shaped by man. There has been deforestation of the Downs for centuries. The woodland that remains today is largely located where deforestation has been inhibited by steep slopes or by the layer of clay with flints, which is difficult to plough. Because of the many small farms that have survived on the Downs, a network of narrow lanes and minor roads has developed. This has resulted in
2030-508: The Elder in 909 AD) (Latin vii dica ); and also in a feoffment defining the Shoelands estate in about 1210 (Latin “Seuedic” ); and also in the plea rolls of the 1263 Surrey Eyre, noting the hanging of one Robert de la Felde of Send at (Latin) “Seinedik” , translated Sendike or Seven Ditches. On the north side of the Hog's Back near the turn off to the village of Seale formerly stood
2100-519: The Kent–Surrey border, often reaching heights in excess of 200 m (660 ft) above sea level at the crest of the escarpment. The highest point is Botley Hill in Surrey at 269 m (883 ft). The County top of Kent at Betsom's Hill , with a height of 251 m (823 ft), is nearby, and the highest point in Greater London , Westerham Heights , at 245 m (804 ft),
2170-479: The North Downs is Botley Hill , Surrey (270 m (890 ft) above sea level). The County Top of Kent is Betsom's Hill (251 m (823 ft) above sea level), which is less than 1 km from Westerham Heights , Bromley , the highest point in Greater London at an elevation of 245 m (804 ft). 'Downs' is from Old English dun , meaning, amongst other things, "hill". The word acquired
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2240-465: The Stour Valley is the only British site for the black-veined moth . Other notable moth species that occur on the North Downs include the fiery clearwing moth and the straw belle moth . On the summit of the cliffs between Deal and Folkestone the early spider orchid occurs in large numbers, as well as the rare oxtongue broomrape . Naturally exposed chalk is rare inland with the exception of
2310-570: The UK. Although its spread is often considered undesirable, scrub provides valuable habitat for a range of invertebrates, including the Roman snail , rufous grasshopper and the dark green fritillary . In Surrey, superficial deposits from the Quaternary are found overlying the chalk. These sands and gravels indicate the position of a former sea shore. Where these deposits occur, they are thin and
2380-613: The broad eastern part in Kent, by further river valleys such as that of the Little Stour . Leith Hill (the highest point in Surrey) is sometimes incorrectly referred to as part of the North Downs, but it is located on the parallel Greensand Ridge and does not consist of chalk. The Downland of the North Downs consists of distinct lithostratigraphic units (the types of strata, the names of which are always capitalised): Following
2450-454: The central grass verge between the two carriageways). One of them was buried prone and another showed signs of having originally been bound or trussed, and scholars now believe that they were criminals buried here after execution at different times over an extended period (Reynolds in 2005; Briggs in 2010). Their burial place was at the meeting point of the parishes of Wanborough , Seale (originally Farnham ) and Puttenham , which were each in
2520-485: The chalk also comes to the surface in the same areas (e.g. Headley Heath on the north east side of Box Hill), allowing acid-loving plants to thrive alongside those that prefer alkaline conditions , producing the rare chalk heath habitat. Worked flints and human and animal remains dating from the Lower Paleolithic , about 400,000 years ago, were discovered at Barnfield Pit near Swanscombe ; this provides
2590-446: The chalk and provide natural corridor routes. In addition to existing rivers, the Downs are crossed by a number of wind gaps – prehistoric river valleys no longer occupied by rivers – including those at Farnham , Betchworth , Caterham , Lyminge and Hawkinge . Except for the river valleys and wind gaps, the crest of the escarpment is almost continuous along its length. The dip slope is dissected by many small dry valleys , and in
2660-431: The craft shop/tea room. These date to the early 18th century. Beside them is Stable Cottage of later that century. Most of the non-forested, agricultural land in Seale is appurtenant to (attached to or let by the owners of) Hampton Lodge, a Grade II listed Regency period mansion of c.1810. The tall two-storey house is Stuccoed brick to its façade with mansard slate roofs and some fishscale banding. This estate
2730-478: The different hundreds of Woking , Farnham and Godalming respectively. It is suggested by Rob Briggs that an elevated site at the junction of different hundreds and parishes was probably a site of general assembly and he identifies it with the place name Seven Ditches, found in the charter of King Caedwalla of Wessex confirming Farnham to the Bishop of Winchester (following the original grant by King Edward
2800-433: The earliest evidence of human occupation in the North Downs. It is suggested that human activity at that time coincided with intermittent warm phases during the last glacial period and that continuous occupation of the Downs did not occur until warming after the glaciation. Flint axes have also been found on river terraces at Farnham, on Walton and Banstead Heaths and on the crest of the escarpment above Folkestone. There
2870-534: The east is dominated by tor-grass . Owing to the close proximity of the North Downs to the European continent, the warm climate and the south-facing escarpment, several plant species survive on the chalk grassland which are scarce or not found elsewhere in the British Isles. The nationally rare late spider orchid is limited within the British Isles to chalk grassland between Folkestone and Wye . One of
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2940-426: The far south known as Heathersett, Littleworth has been attributed to R. Norman, architect. The listed park is due to its later designer, Gertrude Jekyll . James Mangles, who lived at Valewood, Haslemere, was one of the earliest rhododendron collectors and hybridisers. When James died in 1884, most of his plant collection was brought to Littleworth Cross and Harry continued hybridising and exhibiting rhododendrons, with
3010-563: The foot of the scarp slope, and this has been joined much more recently by the M20 motorway . The scarp slope has also been used for fortification; many examples of this still exist, such as Thurnham Castle and on Castle Hill, Folkestone Castle Hill near Folkestone. Many beauty spots on the North Downs are owned by the National Trust , for instance Box Hill and Langdon Cliffs . Other areas of interest are Newland's Corner , Wye Downs and
3080-516: The foot of the steep Hog's Back, is the parish church of St Laurence, Seale. 800m down the valley is a spring, whose stream leads to Cutt Mill and hence to the Wey. The land undulates, between 165m in the southwest, down to 55m in the east. The north border is the 100 to 140m crest of a long range of hills with the popular name, the Hog's Back . Seale in the Kingdom of England remained in its county but
3150-571: The help of his sister Clara. Gertrude Jekyll (1843–1932), who lived nearby at Munstead, knew the Mangles family and was visiting one afternoon in May 1889 when she was introduced to a young architect, Edwin Lutyens (1869–1944) who was designing a gardener's cottage and some garden buildings for Harry Mangles. The meeting was important for both Lutyens and Jekyll: she discovered someone with a similar love of
3220-526: The keeping of livestock and the growing of crops. There is substantial evidence of Neolithic activity within the North Downs, notably the long barrows concentrated in the Medway and Stour valleys. The Medway long barrows , which include Kit's Coty House and Coldrum Stones , are constructed of sarsen stone , locally found on Blue Bell Hill and in the valleys of the dip slope, whilst the Stour Valley long barrows are constructed of earth. The landscape of
3290-502: The largest landholding in the parish of Seale. The Hampton Estate was sold by the Howard family to the Thornton family in 1929 and remains in the hands of their descendants. Wood Lane, which runs from the nucleus of Seale up to the top of the Hog's Back, shares its name with that of the family who leased Seale Manor Farm. The village hall, near the old school, is a venue for regular events and hosts parish council meetings. The church
3360-426: The layer of clay-with-flints overlying the chalk has inhibited clearance. Where this is the case species such as pedunculate oak predominate, although much woodland has been replanted with conifer and sweet chestnut . Calcareous woodland occurs on thin soils where chalk is close to the surface. These conditions are most often found on the escarpment of the North Downs and on valley slopes, but may also occur on
3430-498: The manor as one of the first model farm in Surrey, Blackwell Farm is now a place of controversies since the University of Surrey, its owner, announced its plan to build a "Garden Neighbourhood" as part of Guildford Borough Council's local plan consultation. The Hog's Back is formed of chalk of Cretaceous age, laid down in shallow seas from the deposition of the calcium carbonate skeletons of micro-organisms . The Hog's Back
3500-472: The other side of the Hog's Back, which was originally part of the parish of Seale; their landholdings also extended south of the Hog's Back into what remained of the parish of Seale after Tongham was split off into a separate parish in 1866. As late as 1899, Henry Chester objected to being asked to give up his pew in Seale Church when a new plan was circulated by the churchwardens. The mansion at Poyle Park
3570-470: The plateau of the dip slope . Calcareous woodland is typically dominated by beech , hornbeam , yew and ash . Box Hill has one of the largest areas of native box woodland in England. One notable species characteristic of calcareous woodland is the nationally scarce lady orchid , which is found in more than 100 sites on the Kent stretch of the North Downs, but is confined to just two sites elsewhere in
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#17327977383473640-466: The quantities of Bargate sandstone and sand present in the far north-west of the Greensand Ridge especially in its high uplands, crowned here by the highest point in the parish, Crooksbury Hill. Binton Farm takes its name from a Saxon settlement of Binton, which bears the prefix of an Old English personal name and standard suffix for any settlement. At the top of a short dry valley , at
3710-410: The range, from west to east. 51°16′N 0°30′W / 51.267°N 0.500°W / 51.267; -0.500 Seale, Surrey Seale is a village in Surrey , England. Seale covers most of the civil parish of Seale and Sands and the steep slope and foot of the south side of the Hog's Back (mid-western section of the North Downs between Farnham and Guildford ) as well as
3780-402: The range, local faulting has produced a much steeper angle (up to 55°), resulting in the distinctive Hog's Back between Farnham and Guildford. The North Downs support several important habitats including chalk grassland , scrub , woodland and chalk heath . Chalk grassland is found on the steep south-facing scarp slopes and the more gently graded north-facing dip slopes, where woodland
3850-441: The ridge in the east. The North Downs cuesta has a steep south-facing scarp slope and a more gentle north-facing dip slope . Its southern boundary is defined by the low-lying Vale of Holmesdale at the foot of the escarpment, in which the underlying stratum is primarily gault clay . The northern boundary is less apparent but occurs where the chalk submerges below the more recent Paleocene deposits. The Downs are highest near
3920-542: The river cliffs formed by the River Mole on the west face of Box Hill and at Ham Bank in Norbury Park . However, quarry lakes within chalk pits provide habitats for great crested newt . The scarce musk orchid has colonised disused chalk pits near Hollingbourne in Kent. Woodland was far more extensive on the North Downs prior to human clearance 5000 to 4000 years ago. Fragments still remain particularly where
3990-525: The road over the Hog's Back was "the Via Regia of early deeds and Hundred Rolls" . What is now designated the A31 along the Hog's Back originally formed part of a road leading directly from Winchester into Guildford High Street and from there into London. However, the modern A31 adopts a slightly less direct and less steep approach to the High Street, and reorganisation of central Guildford into
4060-465: The road which runs along the Hog's Back (the A31 ). The view north includes many towns and villages, including Woking , Ash and Aldershot which on a clear day reaches to London, as far as Canary Wharf , Tower 42 , The Gherkin , Wembley Arch and Heathrow Airport . The view to the south is unspoilt and has been designated an area of outstanding natural beauty as well as a site of special scientific interest . These views extend to Hindhead and
4130-486: The sense of "elevated rolling grassland" around the 14th century. The name contains "North" to distinguish them from a similar range of hills – the South Downs – which runs roughly parallel to them but some 50 km (31 mi) to the south. The narrow spine of the Hog's Back between Farnham and Guildford forms the western extremity of the North Downs, whilst the cliffs between Folkestone and Deal terminate
4200-471: The south the clays of the Wealden Group . The chalk is more resistant to weathering than the flanking clays, leading to the ridge's prominence over the surrounding terrain. The Hog's Back gives its name to the geomorphological landform known as a Hogback , which is a long narrow ridge or series of hills with a narrow crest and steep slopes of nearly equal inclination on both flanks. The Hog's Back
4270-563: The southern slopes of the Downs, in particular the Denbies Wine Estate , Dorking , which is the largest vineyard in the country, accounting for 10% of the country's vines. The chalky soils are similar to those of the Champagne region. There is plenty of evidence of chalk extraction on the Downs, particularly along the scarp slope. Oil has been drilled at the foot of the Downs in several locations in Surrey. The Kent Coalfield
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#17327977383474340-569: The two native British sites for the nationally rare monkey orchid is on the North Downs. The nationally scarce man orchid is not uncommon on chalk grassland on the Downs in Surrey and Kent. Other scarce plant species such as early gentian , dwarf milkwort and bedstraw broomrape also occur on chalk grassland in the North Downs. Chalk grassland also supports a rich fauna, particularly insects. Notable butterfly species include Adonis blue and silver-spotted skipper , which may be found on warm, sheltered, south-facing slopes. The chalk downland above
4410-452: The vernacular architecture of south-west Surrey, who would design her new home, Munstead Wood (qv), and through her, he was introduced to many potential clients. Lutyens and Jekyll began a collaboration of building and garden design that would last until her death in 1932. Seale Lodge, built in ornate style with surrounding landholdings fell into dilapidation and was demolished c. 1970. The village school has closed and been converted into
4480-574: Was also in the hundred of Farnham . Successive bishops retained right of free warren and other manorial privileges into the 19th century. Seale's medieval parish church and rector served equally Tongham to the north until 1866, however much of the land was owned by the Bishop of Winchester who owned much of far-west Surrey since the early holder of that position Henry (of Blois) or Winchester , who used his power and status to build Farnham Castle . The manor farm, evidencing this, were tenants of
4550-405: Was built in 1873 called Great Down, attributed to Robert Kerr . This was demolished in about 1950, but the parkland and other associated buildings, such as a lodge and stables, remain. Also on the south side is Greyfriars House, a Grade II* listed Arts and Crafts style mansion built in 1896 by the renowned architect Charles Voysey . It is now a boutique wedding venue. The Hogs Back Brewery
4620-661: Was drained by the ancestors of the rivers which today cut through the North and South Downs. The dome was eroded away over the course of the Cenozoic , exposing the strata beneath and resulting in the escarpments of the Downs. Chalk is a relatively soft rock that may be eroded or weathered in a number of different ways. It is porous, absorbing up to 20% of its dry weight in water, and is therefore highly susceptible to weathering by freeze-thaw action , which may occur over repeated annual or diurnal cycles. This frost weathering produces
4690-450: Was established in the 12th century as an outpost of Waverley Abbey . The bell tower houses a peal of six bells, the oldest and largest cast in the 16th century. The church was extensively restored and enlarged in about 1860. It is served by a rector, who now also has care of the adjacent parishes of Puttenham and Wanborough . These three parishes were formally merged in 2004, although they retain their separate places of worship. Tongham
4760-401: Was established in the late 19th century after coal was found in 1890. Four successful collieries continued to be worked through much of the 20th century: Betteshanger , Snowdown , Tilmanstone and Chislet ; Bettershanger was the last to close in 1989. The east to west ridge of the Downs has provided a natural transport route for centuries. Much of the historic Pilgrims' Way still survives at
4830-540: Was incorporated in its course. In order to avoid the A31, however, the Pilgrims' Way does not run along the top of the Hog's Back. The Hog's Back stretch of the A31 is now a dual carriageway, but the two directions of the road are separated by a central area of trees, some of them very old. The original road ran along the stretch now occupied by the lanes running from Guildford to Farnham , i.e. from east to west. The other two lanes, running from west to east, which are
4900-402: Was originally part of the parish of Seale, but it became an independent parish in 1866. In the west of the parish, associated with The Sands which is immediately south-east of it, is Farnham Golf Club. The first five holes start in parkland after which there is a sudden change in scenery as the pine trees close in and the heather replaces the grass. The oldest building, apart from the church,
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