|
Tillington, West Sussex
Tillington is a village, ecclesiastical parish and civil parish in the District of Chichester in West Sussex, England, west of Petworth on the A272. The civil parish (CP) includes the hamlets of Upperton, River, and River Common. The land area of the CP is ; approximately 500 people lived in 227 households at the 2001 census. Upperton and Tillington are designated Conservation Areas. There are many old dwellings, including medieval timber-framed houses, with one third of the buildings in the parish being grade II listed. Pitshill is a Georgian mansion standing at the head of a valley between Upperton and River. All Hallows Church with its unusual Scots crown tower is a landmark when approaching from Petworth, and is floodlit at night. It was painted by J. M. W. Turner and John Constable. The church, first recorded in 1100 was mostly rebuilt and enlarged between 1807 and 1837, but retains romanesque sculpture and a plain eight-sided twelfth century stone font. Opposite the ch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United Kingdom Census 2001
A nationwide census, known as Census 2001, was conducted in the United Kingdom on Sunday, 29 April 2001. This was the 20th UK census and recorded a resident population of 58,789,194. The 2001 UK census was organised by the Office for National Statistics (ONS) in England and Wales, the General Register Office for Scotland (GROS) and the Northern Ireland Statistics and Research Agency (NISRA). Detailed results by region, council area, ward and output area are available from their respective websites. Organisation Similar to previous UK censuses, the 2001 census was organised by the three statistical agencies, ONS, GROS, and NISRA, and coordinated at the national level by the Office for National Statistics. The Orders in Council to conduct the census, specifying the people and information to be included in the census, were made under the authority of the Census Act 1920 in Great Britain, and the Census Act (Northern Ireland) 1969 in Northern Ireland. In England and Wales these re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Easebourne
Easebourne () is a village, Anglican parish and civil parish in the Chichester District of West Sussex, England. It is half a mile (0.8 km) north of Midhurst, across the River Rother on the A272 and A286 roads. The parish includes the hamlet of Henley to the north. In the 2001 census there were 708 households with a total population of 1,717 of whom 785 were economically active. History Easebourne (''Eseburne'') was listed in the Domesday Book of 1086 as an ancient Hundred, an extensive area reaching as far afield as Graffham and Cocking to the south, Stedham to the west and Tillington to the east, as well as two hamlets that were not parishes: Todham to the southeast and Buddington to the west; in total it included 12 settlements containing 276 households. In 1861, the population was 859, and the area of the parish . Governance An electoral ward of the same name exists. This ward includes Lodsworth and at the 2011 census had a population of 2,492. Amenities There i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fallow Deer
''Dama'' is a genus of deer in the subfamily Cervinae, commonly referred to as fallow deer. Name The name fallow is derived from the deer's pale brown colour. The Latin word ''dāma'' or ''damma'', used for roe deer, gazelles, and antelopes, lies at the root of the modern scientific name, as well as the German ''Damhirsch'', French ''daim'', Dutch ''damhert'', and Italian ''daino''. In Croatian and Serbian, the name for the fallow deer is ''jelen lopatar'' ("shovel deer"), due to the form of its antlers. The Modern Hebrew name of the fallow deer is ''yachmur'' (יחמור). Taxonomy and evolution The genus includes two extant species: Extant species Some taxonomists include the Persian fallow deer as a subspecies In biological classification, subspecies is a rank below species, used for populations that live in different areas and vary in size, shape, or other physical characteristics (morphology), but that can successfully interbreed. Not all species ... (''D. d. me ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
European Badger
The European badger (''Meles meles''), also known as the Eurasian badger, is a badger species in the family Mustelidae native to almost all of Europe. It is classified as least concern on the IUCN Red List as it has a wide range and a large stable population size, and is thought to be increasing in some regions. Several subspecies are recognized with the nominate subspecies (''M. m. meles'') predominating in most of Europe. In Europe, where no other badger species commonly occurs, it is generally just called the "badger". The European badger is a powerfully built, black, white, brown, and grey animal with a small head, a stocky body, small, black eyes, and short tail. Its weight varies, being 7–13 kg (15–29 lb) in spring, but building up to 15–17 kg (33–37 lb) in autumn before the winter sleep period. It is nocturnal and is a social, burrowing animal that sleeps during the day in one of several setts in its territorial range. These burrows have multipl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deer Park (England)
In medieval and Early Modern England, Wales and Ireland, a deer park () was an enclosed area containing deer. It was bounded by a ditch and bank with a wooden park pale on top of the bank, or by a stone or brick wall. The ditch was on the inside increasing the effective height. Some parks had deer " leaps", where there was an external ramp and the inner ditch was constructed on a grander scale, thus allowing deer to enter the park but preventing them from leaving. History Some deer parks were established in the Anglo-Saxon era and are mentioned in Anglo-Saxon Charters; these were often called ''hays'' (from Old English ''heġe'' (“hedge, fence”) and ''ġehæġ'' (“an enclosed piece of land”). After the Norman conquest of England in 1066 William the Conqueror seized existing game reserves. Deer parks flourished and proliferated under the Normans, forming a forerunner of the deer parks that became popular among England's landed gentry. The Domesday Book of 1086 record ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lampyris Noctiluca
''Lampyris noctiluca'', the common glow-worm of Europe (see also "glowworm"), is the type species of beetle in the genus ''Lampyris'' and the family Lampyridae. ''Lampyris noctiluca'' presents a conspicuous sexual dimorphism. The males are winged, with brown elytra, a clearer pronotum and a large brown spot in the middle, while females are larviforme, wings are missing and they are often twice the size of the males (up to in length). These beetles use their bioluminescence to attract mates. The adult females are mostly famed for their glow, although all stages of their life cycle are capable of glowing. In Britain, this species is fairly common compared to its cousin '' Phosphaenus hemipterus'' – the lesser glow worm – which is very rare. Distribution The range of this beetle stretches from Portugal and Ireland in the west, right across Europe, Africa and Asia to China in the east. It also survives further north than any other firefly, almost reaching the Arctic Circle. I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Early Purple Orchid
''Orchis mascula'', the early-purple orchid, early spring orchis, is a species of flowering plant in the orchid family, Orchidaceae. Description ''Orchis mascula'' is a perennial herbaceous plant with stems up to high, green at the base and purple on the apex. The root system consists of two tubers, rounded or ellipsoid. The leaves, grouped at the base of the stem, are oblong-lanceolate, pale green, sometimes with brownish-purple speckles. The inflorescence is long and it is composed of 6 to 20 flowers gathered in dense cylindrical spikes. The flower size is about and the color varies from pinkish-purple to purple. The lateral sepals are ovate-lanceolate and erect, the median one, together with the petals, is smaller and cover the gynostegium. The labellum is three-lobed and convex, with crenulated margins and the basal part clearer and dotted with purple-brown spots. The spur is cylindrical or clavate, horizontal or ascending. The gynostegium is short, with reddish-green ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greensand
Greensand or green sand is a sand or sandstone which has a greenish color. This term is specifically applied to shallow marine sediment that contains noticeable quantities of rounded greenish grains. These grains are called ''glauconies'' and consist of a mixture of mixed-layer clay minerals, such as smectite and glauconite. Greensand is also loosely applied to any glauconitic sediment. Formation 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 the late-Cretaceous deposits of New Jersey. Occurrence 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 h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Rother (Western)
The River Rother flows from Empshott in Hampshire, England, to Stopham in West Sussex, where it joins the River Arun. At long, most of the river lies within West Sussex except for the first which lie in Hampshire. The upper river, from its source to Midhurst, has been used to power watermills, with the earliest recorded use being in 1086, when the Domesday survey was conducted. Although none are still operational, many of the buildings which housed the mills still exist, and in some cases, still retain their milling machinery. This upper section is also noted for a number of early bridges, which have survived since their construction in the fifteenth, sixteenth and seventeenth centuries. The lower river, from Midhurst to its junction with the River Arun, has been used for navigation. Boats used the section from the Arun to Fittleworth following improvements made to the Arun in 1615, and after the Arun Navigation was completed in 1790, the Earl of Egremont made the river na ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ironstone
Ironstone is a sedimentary rock, either deposited directly as a ferruginous sediment or created by chemical replacement, that contains a substantial proportion of an iron ore compound from which iron (Fe) can be smelted commercially. Not to be confused with native or telluric iron, which is very rare and found in metallic form, the term ''ironstone'' is customarily restricted to hard, coarsely banded, non-banded, and non-cherty sedimentary rocks of post-Precambrian age. The Precambrian deposits, which have a different origin, are generally known as banded iron formations. The iron minerals comprising ironstones can consist either of oxides, i.e. limonite, hematite, and magnetite; carbonates, i.e. siderite; silicates, i.e. chamosite; or some combination of these minerals.U.S. Bureau of Mines Staff (1996) ''Dictionary of Mining, Mineral, & Related Terms.'' Report SP-96-1, U.S. Department of Interior, U.S. Bureau of Mines, Washington, D.C.Neuendorf, K. K. E., J. P. Mehl Jr., and J. A. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Escarpment
An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations. The terms ''scarp'' and ''scarp face'' are often used interchangeably with ''escarpment''. Some sources differentiate the two terms, with ''escarpment'' referring to the margin between two landforms, and ''scarp'' referring to a cliff or a steep slope. In this usage an escarpment is a ridge which has a gentle slope on one side and a steep scarp on the other side. More loosely, the term ''scarp'' also describes a zone between a coastal lowland and a continental plateau which shows a marked, abrupt change in elevation caused by coastal erosion at the base of the plateau. Formation and description Scarps are generally formed by one of two processes: either by differential erosion of sedimentary rocks, or by movement of the Earth's crust at a geologic fault. The first process is the more common type: the escarpment is a t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
