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Prince's Coverts
Prince's Coverts is an area of of managed woodland in Oxshott, Surrey, England, to which there is public access. It is owned and managed by the Crown Estate who refer to the area as Oxshott Woods. It adjoins Malden Rushett in Greater London, the Pachesham Park estate and Leatherhead Golf Course to the east. Geography Princes Coverts is 864 acres (349 hectares) of managed woodland owned by the Crown Estate. It includes, separated by roads, a minor northern woodland beyond Fairoaks Lane, ''Great Oakes'' and ''Sixty Acre Wood'', and the irregularly shaped (partly converted to other use) ''Woodlands Park'' to the south. The southernmost portion of the very long and quite narrow, almost rectangular Crown Estate has been assigned to and converted to Queen Elizabeth's Foundation for Disabled People's Training College and its Dorincourt home for the disabled, Woodlands Park Golf Course, Leatherhead, and Tyrwhitt House, a combat stress centre. While the south drains southward to Mole s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mineral Spa
Mineral spas are destination spa, spa resorts developed around naturally occurring mineral springs. Like seaside resorts, they are mainly used recreationally although they also figured prominently in traditional medicine, prescientific medicine. Origins Spas were used for millennia for their purported healing or healthful benefits to those wealthy enough or close enough to partake of their waters. This was called a mineral cure and gave let to such phrases as ''taking a cure'' and ''taking the waters''. There has always been a mixture of recreational and medicinal connotations involved, from rest and relaxation, stress relief, and convalescence to more specific notions such as humorism. These phrases are still sometimes used today as a euphemism for one trying to kick a drug dependency. In many cases, mineral spas were located in mountainous locales that gave an additional excuse to leave the drudgery of a hot house in warm weather during summer's onset and were seasonally po ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Leaflet (information)
A pamphlet is an unbound book (that is, without a hard cover or binding). Pamphlets may consist of a single sheet of paper that is printed on both sides and folded in half, in thirds, or in fourths, called a ''leaflet'' or it may consist of a few pages that are folded in half and saddle stapled at the crease to make a simple book. For the "International Standardization of Statistics Relating to Book Production and Periodicals", UNESCO defines a pamphlet as "a non-periodical printed publication of at least 5 but not more than 48 pages, exclusive of the cover pages, published in a particular country and made available to the public" and a book as "a non-periodical printed publication of at least 49 pages, exclusive of the cover pages". The UNESCO definitions are, however, only meant to be used for the particular purpose of drawing up their book production statistics. Etymology The word ''pamphlet'' for a small work (''opuscule'') issued by itself without covers came into Middl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Penge
Penge () is a suburb of South East London, England, now in the London Borough of Bromley, west of Bromley, north east of Croydon and south east of Charing Cross. History Penge was once a small hamlet, which was recorded under the name Penceat in an Anglo-Saxon deed dating from 957. Most historians believe the name of the town is derived from the Celtic word ''Penceat'', which means 'edge of wood' and refers to the fact that the surrounding area was once covered in a dense forest. The original Celtic words of which the name was composed referred to 'pen' ('head'), as in the Welsh 'pen', and 'ceat' ('wood'), similar to the Welsh 'coed', as in the name of the town of Pencoed in Wales. The largest amosite mine in the world, in South Africa, was named Penge apparently because one of the British directors thought the two areas were similar in appearance. Pensgreene and the Crooked Billet Penge was an inconspicuous area with few residents before the arrival of the railways. A trav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sydenham, London
Sydenham () is a district of south-east London, England, which is shared between the London boroughs of London Borough of Lewisham, Lewisham, London Borough of Bromley, Bromley and London Borough of Southwark, Southwark. Prior to the creation of the County of London in 1889, Sydenham was located in Kent, bordering Surrey. Historically, the area was very affluent, with the Crystal Palace being relocated to Sydenham Hill in 1854. Today, Sydenham is a diverse area, with a population of 28,378 (2011 census) and borders Forest Hill, London, Forest Hill, Dulwich, Crystal Palace, London, Crystal Palace, Penge, Beckenham, Catford and Bellingham, London, Bellingham. History Originally known as Shippenham, Sydenham began as a small settlement, a few cottages among the woods, whose inhabitants grazed their animals and collected wood. In the 1640s, springs of water in what is now Sydenham Wells Park, Wells Park were discovered to have medicinal properties, attracting crowds of people to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tulse Hill
Tulse Hill is a district in the London Borough of Lambeth in South London that sits on Brockwell Park. It is approximately five miles from Charing Cross and is bordered by Brixton, Dulwich, Herne Hill, Streatham and West Norwood. History The area known as Tulse Hill is part of the former Manor or Manors of Bodley, Upgroves and Scarlettes whose precise boundaries are now uncertain. The name of the area comes from the Tulse family who came into ownership of farmland in the area during the period of the Commonwealth in the 1650s. Sir Henry Tulse was Lord Mayor of London in 1683 and his daughter Elizabeth married Richard Onslow, 1st Baron Onslow. The land remained in Onslow ownership until 1789 when most of it was purchased by William Cole. The estate was further divided on Cole's death in 1807. The western part was left to "Mercy Cressingham, spinster" (now commemorated by the Cressingham Gardens estate in the area) and the eastern part -now mostly occupied by Brockwell Park - w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Streatham Hill
Streatham ( ) is a district in south London, England. Centred south of Charing Cross, it lies mostly within the London Borough of Lambeth, with some parts extending into the neighbouring London Borough of Wandsworth. Streatham was in Surrey before becoming part of the County of London in 1889, and then Greater London in 1965. The area is identified in the London Plan as one of 35 major centres in Greater London. History Streatham means "the hamlet on the street". The street in question, the London to Brighton Way, was the Roman road from the capital Londinium to the south coast near Portslade, today within Brighton and Hove. It is likely that the destination was a Roman port now lost to coastal erosion, which has been tentatively identified with 'Novus Portus' mentioned in Ptolemy's Geographia. The road is confusingly referred to as Stane Street (Stone Street) in some sources and diverges from the main London-Chichester road at Kennington. After the departure of the Romans ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wimbledon, London
Wimbledon () is a district and town of Southwest London, England, southwest of the centre of London at Charing Cross; it is the main commercial centre of the London Borough of Merton. Wimbledon had a population of 68,187 in 2011 which includes the electoral wards of Abbey, Dundonald, Hillside, Trinity, Village, Raynes Park and Wimbledon Park. It is home to the Wimbledon Championships and New Wimbledon Theatre, and contains Wimbledon Common, one of the largest areas of common land in London. The residential and retail area is split into two sections known as the "village" and the "town", with the High Street being the rebuilding of the original medieval village, and the "town" having first developed gradually after the building of the railway station in 1838. Wimbledon has been inhabited since at least the Iron Age when the hill fort on Wimbledon Common is thought to have been constructed. In 1086 when the Domesday Book was compiled, Wimbledon was part of the manor of Mortlake. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loam
Loam (in geology and soil science) is soil composed mostly of sand (particle size > ), silt (particle size > ), and a smaller amount of clay (particle size < ). By weight, its mineral composition is about 40–40–20% concentration of sand–silt–clay, respectively. These proportions can vary to a degree, however, and result in different types of loam soils: sandy loam, silty loam, clay loam, sandy clay loam, silty clay loam, and loam. In the , textural classification triangle, the only soil that is not predominantly sand, silt, or clay is called "loam". Loam soils generally contain more nutrients, moisture, and |
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 the North Downs is Botley Hill, Surrey ( above sea level). The ''County Top'' of Kent is Betsom's Hill ( above sea level), which is less than 1 km from Westerham Heights, Bromley, the highest point in Greater London at an elevation of . Etymology 'Downs' is from Old English ''dun'', meaning, amongst other things, "hill". The word acquired 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 to the south. Geography The narrow spine of the Hog's Back between ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
London Clay
The London Clay Formation is a marine geological formation of Ypresian (early Eocene Epoch, c. 56–49 million years ago) age which crops out in the southeast of England. The London Clay is well known for its fossil content. The fossils from the lower Eocene rocks indicate a moderately warm climate, the tropical or subtropical flora. Though sea levels changed during the deposition of the clay, the habitat was generally a lush forest – perhaps like in Indonesia or East Africa today – bordering a warm, shallow ocean. The London Clay is a stiff bluish clay which becomes brown when weathered and oxidized. Nodular lumps of pyrite are frequently found in the clay layers. Pyrite was produced by microbial activity (sulfate reducing bacteria) during clay sedimentation. Once clay is exposed to atmospheric oxygen, framboidal pyrite with a great specific surface is rapidly oxidized. Pyrite oxidation produces insoluble brown iron oxyhydroxide (FeOOH) and sulfuric acid leading to the f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gravel
Gravel is a loose aggregation of rock fragments. Gravel occurs naturally throughout the world as a result of sedimentary and erosive geologic processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm to 20–63 mm. One cubic metre of gravel typically weighs about 1,800 kg (or a cubic yard weighs about 3,000 lb). Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
