Newick And Chailey Station
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Newick And Chailey Station
Newick is a village, civil parish and electoral ward in the Lewes District of East Sussex, England. It is located on the A272 road east of Haywards Heath. The parish church, St. Mary's, dates mainly from the Victorian era, but still has a Norman window. Zion Chapel, a Strict Baptist chapel, was built in 1834 and converted to flats in 2001. Newick Evangelical Free Church, originally a mission hall, opened in 1892. The village is home to three pubs (''The Crown Inn'', ''The Royal Oak'', and ''The Bull Inn''), one restaurant (Newick Tandoori), a butcher, a baker, a pharmacy, as well as a number of other businesses. There is also a primary school, a health centre, a village hall known originally as the 'Derek Hall', and a post office. Like many other places in Sussex, Newick holds an annual Bonfire Night celebration on the Saturday before Lewes Bonfire Night. Many of the local bonfire societies join the procession. History Newick was a dispersed settlement until the Second Wo ...
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Lewes (UK Parliament Constituency)
Lewes is a constituency in East Sussex represented in the House of Commons of the UK Parliament since 2015 by Maria Caulfield, a Conservative. Constituency profile The constituency is centred on the town of Lewes. However, the constituency also covers most of the Lewes district, including the coastal towns of Seaford and Newhaven, which are rural and semi-rural and all in outer parts of the London Commuter Belt, though with a high number of people who have retired from across the country. The constituency excludes Peacehaven and Telscombe which since 1997 have been in Brighton, Kemptown, and includes part of neighbouring Wealden District. Electoral Calculus categorises the constituency as "Centrist", indicating average levels of education and wealth and moderate support for Brexit. Boundaries 1885–1918: The Borough of Brighton, the Sessional Divisions of Hove and Worthing, and parts of the Sessional Divisions of Lewes and Steyning. 1918–1950: The Borough of Lewes, th ...
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Ox-eye Daisy
''Leucanthemum vulgare'', commonly known as the ox-eye daisy, oxeye daisy, dog daisy, marguerite (french: Marguerite commune, "common marguerite") and other common names, is a widespread flowering plant native to Europe and the temperate regions of Asia, and an introduced plant to North America, Australia and New Zealand. Description ''L. vulgare'' is a perennial herb that grows to a height of and has a creeping underground rhizome. The lower parts of the stem are hairy, sometimes densely hairy but more or less glabrous in the upper parts. The largest leaves are at the base of the plant and are long, about wide and have a petiole. These leaves have up to 15 teeth, or lobes or both on the edges. The leaves decrease in size up the stem, the upper leaves up to long, lack a petiole and are deeply toothed. The plant bears up to three "flowers" like those of a typical daisy. Each is a "head" or capitulum wide. Each head has between fifteen and forty white "petals" (ray florets) ...
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Betony
Betony is a common name for a plant which may refer to: *''Stachys'', a genus of plants containing several species commonly known as betony in Europe **'' Stachys officinalis'', a historically important medicinal plant *''Pedicularis ''Pedicularis'' is a genus of perennial green root parasite plants currently placed in the family Orobanchaceae (the genus previously having been placed in Scrophulariaceae ''sensu lato''). Description Between 350 and 600 species are accep ...
'', a genus of plants containing several species commonly known as betony in North America {{plant common name ...
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Chalybeate
Chalybeate () waters, also known as ferruginous waters, are mineral spring waters containing salts of iron. Name The word ''chalybeate'' is derived from the Latin word for steel, , which follows from the Greek word . is the singular form of or Chalybes, who were a people living on Mount Ida in north Asia Minor and who were expert in iron working. ''Ferruginous'' () comes from the Latin word 'of a rusty colour', from 'iron rust', from 'iron'. History Early in the 17th century, chalybeate water was said to have health-giving properties and many people once promoted its qualities. Dudley North, 3rd Baron North, discovered the chalybeate spring at Tunbridge Wells in 1606. His eldest son's physician said the waters contained "vitriol" and the waters of Tunbridge Wells could cure: the colic, the melancholy, and the vapours; it made the lean fat, the fat lean; it killed flat worms in the belly, loosened the clammy humours of the body, and dried the over-moist brain. He also ...
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Weald Clay
Weald Clay or the Weald Clay Formation is a Lower Cretaceous sedimentary rock unit underlying areas of South East England, between the North and South Downs, in an area called the Weald Basin. It is the uppermost unit of the Wealden Group of rocks within the Weald Basin, and the upper portion of the unit is equivalent in age to the exposed portion of the Wessex Formation on the Isle of Wight. It predominantly consists of thinly bedded mudstone. The un-weathered form is blue/grey, and the yellow/orange is the weathered form, it is used in brickmaking. The formation was deposited in lagoonal, lacustrine and alluvial conditions that varied from freshwater to brackish. The clay alternates with other subordinate lithologies, notably hard red-weathering beds of ironstone, limestone (Sussex Marble) and sandstones, notably including the calcareous sandstone unit referred to as the Horsham Stone. It has a gradual, conformable contact with the underlying Tunbridge Wells Sand Formation, a ...
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Wealden Group
The Wealden Group, occasionally also referred to as the Wealden Supergroup, is a group (a sequence of rock strata) in the lithostratigraphy of southern England. The Wealden group consists of paralic to continental (freshwater) facies sedimentary rocks of Berriasian to Aptian age and thus forms part of the English Lower Cretaceous. It is composed of alternating sands and clays. The sandy units were deposited in a flood plain of braided rivers, the clays mostly in a lagoonal coastal plain.Jackson (2008) The Wealden Group can be found in almost all Early Cretaceous basins of England: its outcrops curve from the Wessex Basin in the south to the Cleveland Basin in the northeast. It is not found in northwest England and Wales, areas which were at the time tectonic highs where no deposition took place. The same is true for the London Platform around London and Essex. Offshore, the Wealden Group can reach a thickness of 700 metres. The terms ''Wealden'' and ''Wealden facies'' are also ...
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Chailey
Chailey is a village and civil parish in the Lewes District of East Sussex, England. It is located 7 miles north of Lewes, on the A272 road from Winchester to Canterbury. The Prime Meridian passes just to the east of Chailey. The parish consists of the settlements: South Chailey (which also incorporates South Common), South Street, Chailey (also known as Chailey Green) and North Chailey (which incorporates the North Common). The parish church is dedicated to St. Peter and is recorded as having been built in 1256. Recently a special service was held to commemorate its 750 years. At one time Chailey had more churches than pubs. The churches being ''St Peter's'', ''St Martin's'' (within Chailey Heritage), ''Chailey Free Church'', ''St John's'' (now housing in South Common), and ''St Mary's'' (now housing in North Common), and the pubs being the ''King's Head'', ''Five Bells'', ''Horns Lodge'' and the ''Swan House''. In addition it is believed another chapel was sited near the Bluebe ...
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Barcombe
Barcombe is an East Sussex village and civil parish in the Lewes District of East Sussex. The parish has four settlements: old Barcombe (), the oldest settlement in the parish with the parish church; Barcombe Cross (), the more populous settlement and main hub with the amenities and services; the hamlet of Spithurst () in the north east and Town Littleworth () in the north west. Barcombe was recorded in the ''Domesday Book'' as "Berchamp". The origins of the place name 'Barcombe' may have derived from two sources: the Saxon 'Berecampe', meaning 'barley land' and the Latin loan word 'campus', a field. Barcombe is particularly noted to Sussex residents and tourists for 'Barcombe Mills', a reference to an old water-mill complex on the River Ouse at the base of the hill/plateau on which Barcombe Cross sits. The mills burnt down before the Second World War, but Barcombe Mills is still a popular Sunday outing for townsfolk from Lewes and Brighton. History Roman settlements Ther ...
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Fletching
Fletching is the fin-shaped aerodynamic stabilization device attached on arrows, bolts, darts, or javelins, and are typically made from light semi-flexible materials such as feathers or bark. Each piece of such fin is a fletch, also known as a flight or feather. A fletcher is a person who attaches fletchings to the shaft of arrows. The word is related to the French word , meaning 'arrow', via the ultimate root of Old Frankish . Description As a noun, ''fletching'' refers collectively to the fins or vanes, each of which individually is known as a fletch. Traditionally, the fletching consists of three matched half-feathers attached near the back of the arrow or shaft of the dart that are equally spaced around its circumference. Four fletchings have also been used. In English archery, the male feather, from a cock, is used on the outside of the arrow, while the other two stabilizing feathers are from a female, or hen. Traditional archery lore about feather curvature is that a ...
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River Ouse, Sussex
The Ouse ( ) is a 35 mile (56 kilometre) long river in the English county, counties of West Sussex, West and East Sussex. It rises near Lower Beeding in West Sussex, and flows eastwards and then southwards to reach the sea at Newhaven, East Sussex, Newhaven. It skirts Haywards Heath and passes through Lewes. It forms the main spine of an extensive network of smaller streams, of which the River Uck is the main tributary. As it nears the coast it passes through the Lewes and Laughton Levels, an area of flat, low-lying land that borders the river and another tributary, the Glynde Reach. It was a large tidal inlet at the time of the Domesday book in 1086, but over the following centuries, some attempts were made to reclaim some of the valley floor for agriculture, by building embankments, but the drainage was hampered by the buildup of a large shingle bar which formed across the mouth of the river by longshore drift. In 1539, a new channel for the entrance to the river was cut thro ...
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George V Of The United Kingdom
George V (George Frederick Ernest Albert; 3 June 1865 – 20 January 1936) was King of the United Kingdom and the British Dominions, and Emperor of India, from 6 May 1910 until his death in 1936. Born during the reign of his grandmother Queen Victoria, George was the second son of Albert Edward, Prince of Wales, and was third in the line of succession to the British throne behind his father and his elder brother, Prince Albert Victor. From 1877 to 1892, George served in the Royal Navy, until the unexpected death of his elder brother in early 1892 put him directly in line for the throne. On Victoria's death in 1901, George's father ascended the throne as Edward VII, and George was created Prince of Wales. He became king-emperor on his father's death in 1910. George's reign saw the rise of socialism, communism, fascism, Irish republicanism, and the Indian independence movement, all of which radically changed the political landscape of the British Empire, which itself reache ...
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List Of King George V Playing Fields In East Sussex
References {{King George V Fields in the United Kingdom Sussex, East King G King G King is the title given to a male monarch in a variety of contexts. The female equivalent is queen, which title is also given to the consort of a king. *In the context of prehistory, antiquity and contemporary indigenous peoples, the tit ... Lists of buildings and structures in East Sussex ...
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