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London To Lewes Way
The London to Lewes Way is a long Roman road between Watling Street at Peckham and Lewes in Sussex. The road passes through Beckenham and West Wickham, then crosses the North Downs above Titsey, on the county boundary between Surrey and Kent, and is overlain by Edenbridge High Street.Ivan Donald Margary, ''Roman Ways in the Weald'' 1965 Phoenix House The road continues on this alignment onto the high ground of Ashdown Forest, where the more grassy vegetation on the silted up outer ditches contrasts very clearly with surrounding heather in aerial photographs, then descends through Piltdown to Lewes, linking with the Sussex Greensand Way at Barcombe Mills and with a network of roads at Lewes. Dating evidence First and early second century pottery fragments were found over the edge of the road near Barcombe Mills, which, together with the heavy construction and planned alignments, indicate a late 1st or early 2nd century date. Design and construction Five main alignments were ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edenbridge 6 , a neighbourhood in Toronto, Ontario, Canada, commonly referred to as Edenbridge-Humber Valley
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Edenbridge may mean: *Edenbridge (band), a symphonic metal band from Austria *Edenbridge, Kent, a town in England *Edenbridge, Saskatchewan, a former Jewish settlement in Canada *Humber Valley Village Humber Valley Village is a neighbourhood located in Toronto, Ontario, Canada. It is within the former City of Etobicoke and includes some of the most expensive real estate in the metropolitan west end. The boundaries are from Dundas Street on the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flint
Flint, occasionally flintstone, is a sedimentary cryptocrystalline form of the mineral quartz, categorized as the variety of chert that occurs in chalk or marly limestone. Flint was widely used historically to make stone tools and start fires. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones.''The Flints from Portsdown Hill'' Inside the nodule, flint is usually dark grey, black, green, white or brown in colour, and often has a glassy or waxy appearance. A thin layer on the outside of the nodules is usually different in colour, typically white and rough in texture. The nodules can often be found along s and |
River Pool (London)
The River Pool is a tributary of the River Ravensbourne. It is 5.1 km (3 miles) in length, and rises with its tributaries between Shirley and West Wickham in the London Borough of Croydon. It then flows northwards through Beckenham in the London Borough of Bromley, and Sydenham in the London Borough of Lewisham, to join the Ravensbourne in Catford. Two of its tributaries are the River Beck and the Chaffinch Brook. For much of its length the river lies in a floodplain. Land on either side is given up to sports grounds and a flood watch is kept continually on it. In New Beckenham, the River Pool Walkway, running north from Lennard Road near the Midland Bank Sports Ground and Cator Park, includes a conservation site and naturalised areas; the route is part of the National Cycle Network. At Sydenham, the section of the river that ran in a culvert under the gas works has been opened up and landscaped. In June 2009, London Mayor Boris Johnson fell into the River Pool whilst promo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
London To Lewes Way Titsey
London is the capital and largest city of England and the United Kingdom, with a population of just under 9 million. It stands on the River Thames in south-east England at the head of a estuary down to the North Sea, and has been a major settlement for two millennia. The City of London, its ancient core and financial centre, was founded by the Romans as '' Londinium'' and retains its medieval boundaries.See also: Independent city § National capitals The City of Westminster, to the west of the City of London, has for centuries hosted the national government and parliament. Since the 19th century, the name "London" has also referred to the metropolis around this core, historically split between the counties of Middlesex, Essex, Surrey, Kent, and Hertfordshire, which largely comprises Greater London, governed by the Greater London Authority.The Greater London Authority consists of the Mayor of London and the London Assembly. The London Mayor is distinguished from the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blythe Hill Fields
Blythe Hill Fields, also sometimes known as Blythe Hill is an area of elevated open land in the London Borough of Lewisham that commands panoramic views over Canary Wharf, the City, Kent and Surrey. The surrounding areas of Blythe Hill Fields involve Catford to the south and southeast, Crofton Park to the north, and Forest Hill to the north west. The land stands at an elevation of – which may be one of the reasons it escaped development – and was once part of Brockley Farm. A brickworks was also formerly on part of the site and a chimney remained there until 1938. Blythe Hill House was built to the south in 1842 and its grounds covered a large part of Blythe Hill Fields until it was demolished in 1895. The land where Blythe Hill Fields now stands was bought by London County Council and opened as a public park in 1935. Access The park can be accessed from a number of different points: * Blythe Hill Lane * Montacute Road * Codrington Hill * Brockley View. The Transport For ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nunhead Railway Station
Nunhead railway station is in the Nunhead area of the London Borough of Southwark. It is measured from . The station is managed by Thameslink. It is in Travelcard Zone 2. Services Services at Nunhead are operated by Southeastern and Thameslink using , , and EMUs. The typical off-peak service in trains per hour is: * 2 tph to * 2 tph to London Blackfriars * 2 tph to via * 2 tph to via During the peak hours, additional services between , and call at the station. In addition, the service to London Blackfriars is extended to and from via . History The Crystal Palace and South London Junction Railway from Canterbury Road Junction, near Brixton to Crystal Palace (High Level) was opened by the London, Chatham and Dover Railway (LCDR) on 1 August 1865, to take passengers to the Crystal Palace. Train services on the Crystal Palace High Level line ceased in 1917–1919 and 1944-1946 for wartime economies. The line closed to all traffic on 20 September 1954. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old Kent Road
Old Kent Road is a major thoroughfare in South East London, England, passing through the London Borough of Southwark. It was originally part of an ancient trackway that was paved by the Romans and used by the Anglo-Saxons who named it Wæcelinga Stræt (Watling Street). It is now part of the A2, a major road from London to Dover. The road was important in Roman times linking London to the coast at Richborough and Dover via Canterbury. It was a route for pilgrims in the Middle Ages as portrayed in Chaucer's Canterbury Tales, when Old Kent Road was known as Kent Street. The route was used by soldiers returning from the Battle of Agincourt. In the 16th century, St Thomas-a-Watering on Old Kent Road was a place where religious dissenters and those found guilty of treason were publicly hanged. The road was rural in nature and several coaching inns were built alongside it. In the 19th century it acquired the name Old Kent Road and several industrial premises were set up to close to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Agger (ancient Rome)
An agger (Latin) is an ancient Roman embankment or any artificial elevation. The most common agger was the ridge or embankment on which Roman roads were built to give the proper draining base. The agger was constructed by excavating the line of the road, building a firm foundation, refilling and compressing the soil, adding more soil from digging drainage ditches or fosses on one or both sides of the road, then surfacing with graded layers of stone and cobbles. The material used to build the aggers was dug from lateral ditches. Once the material was dug out of the ditches that were known as "scoop ditches", they were used as the storm drain for that road. These ditches could also be used for soldiers to hide in if they ever were under attack from enemies. On the most important road routes, the agger could be high and wide. Along less important routes the road is occasionally set directly on the levelled ground surface with stones laid to provide drainage with the lateral ditch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Grinstead
East Grinstead is a town in West Sussex, England, near the East Sussex, Surrey, and Kent borders, south of London, northeast of Brighton, and northeast of the county town of Chichester. Situated in the extreme northeast of the county, the civil parish has an area of . The population at the 2011 Census was 26,383. Nearby towns include Crawley and Horley to the west, Tunbridge Wells to the east and Redhill and Reigate to the northwest. The town is contiguous with the village of Felbridge to the northwest. Until 1974 East Grinstead was in East Sussex, before joining together with Haywards Heath and Burgess Hill as the Mid-Sussex district of West Sussex. The town is on the Greenwich Meridian. It has many historic buildings, and the Weald and Ashdown Forest lie to the south-east. Places of interest The High Street contains one of the longest continuous runs of 14th-century timber-framed buildings in England. Other notable buildings in the town include Sackville College, the san ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hartfield
Hartfield is a village and civil parish in the Wealden district of East Sussex, England. The parish also includes the settlements of Colemans Hatch, Hammerwood and Holtye, all lying on the northern edge of Ashdown Forest. Geography The main village of Hartfield lies seven miles (11.2 km) south-west of Royal Tunbridge Wells where the B2110 road between Groombridge and Forest Row meets the B2026 road between Edenbridge and Maresfield. Governance Hartfield Parish Council consists of 13 members. The population of this ward as taken at the 2011 census was 2,639. The parish settlements Hartfield is the main village in the parish. The church is dedicated to St Mary the Virgin. There are three public houses: ''Anchor Inn''; ''Gallipot Inn''; and ''Haywagon Inn''. The village street is narrow, precluding much parking although The Anchor and Haywagon Inns have private car parks for patrons only. Note that the Haywagon Inn closed in 2015 following a planning application to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wealden Iron Industry
The Wealden iron industry was located in the Weald of south-eastern England. It was formerly an important industry, producing a large proportion of the bar iron made in England in the 16th century and most British cannon until about 1770. Ironmaking in the Weald used ironstone from various clay beds, and was fuelled by charcoal made from trees in the heavily wooded landscape. The industry in the Weald declined when ironmaking began to be fuelled by coke made from coal, which does not occur accessibly in the area. Resources Iron ore in the form of siderite, commonly known as iron stone or historically as mine, occurs in patches or bands in the Cretaceous clays of the Weald. Differing qualities of ore were extracted and mixed by experienced smelters to give the best results. Sites of opencast quarries survive from the pre-Roman and Roman eras, but medieval ore extraction was mainly done by digging a series of minepits about five metres in diameter and up to twelve metres deep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
