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The Wolds
The Wolds is a term used in England to describe a range of hills which consists of open country overlying a base of limestone or chalk. Geography The Wolds comprise a series of low hills and steep valleys that are in the main underlain by calcareous (chalk and limestone) and sandstone rock, laid down in the Cretaceous and Jurassic periods. One exception to this is the North Leicestershire /South Nottinghamshire Wolds, which are underlain by sometimes chalky glacial till ('Oadby Till'). The characteristic open valleys of the Wolds were created during the last glacial period through the action of glaciation and meltwater. The chalk that underlies the Chalk Wolds Landscape Character Type extends from the Yorkshire Wolds to the south coast of England, in East Sussex and in Dorset. Geologically, the Lincolnshire Wolds is a continuation of the Yorkshire Wolds which runs through the East Riding of Yorkshire; the point at which the ranges of hill crosses the Humber is known as the Humber G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Head Of Swindale, On The Wolds Way - Geograph
A head is the part of an organism which usually includes the ears, brain, forehead, cheeks, chin, eyes, nose, and mouth, each of which aid in various sensory functions such as sight, hearing, smell, and taste. Some very simple animals may not have a head, but many bilaterally symmetric forms do, regardless of size. Heads develop in animals by an evolutionary trend known as cephalization. In bilaterally symmetrical animals, nervous tissue concentrate at the anterior region, forming structures responsible for information processing. Through biological evolution, sense organs and feeding structures also concentrate into the anterior region; these collectively form the head. Human head The human head is an anatomical unit that consists of the skull, hyoid bone and cervical vertebrae. The term "skull" collectively denotes the mandible (lower jaw bone) and the cranium (upper portion of the skull that houses the brain). Sculptures of human heads are generally based on a ske ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humber Gap
The Humber Gap is a term for the geographic gap between the roughly north–south running line of hills formed by the Yorkshire Wolds and the Lincolnshire Wolds, formed by the west–east running Humber Estuary. In the geological past the gap has formed part of an ice barrier due to glaciers during the ice age resulting in damming and formation of a 'Humber Lake', and also forms a geological division. In modern times the gap has formed a natural choice for transport routes, such as the railways. The Humber Bridge also crosses the Humber close to the gap. See also *Humberhead Levels: very heavily silted area formed west of the gap as a result of the damming of the gap, and subsequent lake formation *North Ferriby and South Ferriby South Ferriby is a village in North Lincolnshire, England. It is situated on the south bank of the Humber Estuary and west from the Humber Bridge. North Ferriby is directly opposite on the Estuary's north bank. Village population was 651 in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wessex
la, Regnum Occidentalium Saxonum , conventional_long_name = Kingdom of the West Saxons , common_name = Wessex , image_map = Southern British Isles 9th century.svg , map_caption = Southern Britain in the ninth century , event_start = Established , year_start = 519 , event_end = English unification , year_end = 12 July 927 , event1 = , date_event1 = , event_pre = Settlement , date_pre = 5th–6th century , event_post = Norman conquest , date_post = 14 October 1066 , border_s2 = no , common_languages = Old English *West Saxon dialect British Latin , religion = PaganismChristianity , leader1 = Cerdic (first) , leader2 = Ine , leader3 = Ecgberht , leader4 = Alfred the Great , leader5 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Weald
The Weald () is an area of South East England between the parallel chalk escarpments of the North and the South Downs. It crosses the counties of Hampshire, Surrey, Sussex and Kent. It has three separate parts: the sandstone "High Weald" in the centre; the clay "Low Weald" periphery; and the Greensand Ridge, which stretches around the north and west of the Weald and includes its highest points. The Weald once was covered with forest, and its name, Old English in origin, signifies "woodland". The term is still used today, as scattered farms and villages sometimes refer to the Weald in their names. Etymology The name "Weald" is derived from the Old English ', meaning "forest" (cognate of German ''Wald'', but unrelated to English "wood", which has a different origin). This comes from a Germanic root of the same meaning, and ultimately from Indo-European. ''Weald'' is specifically a West Saxon form; '' wold'' is the Anglian form of the word. The Middle English form of the word i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alfred Tennyson
Alfred Tennyson, 1st Baron Tennyson (6 August 1809 – 6 October 1892) was an English poet. He was the Poet Laureate during much of Queen Victoria's reign. In 1829, Tennyson was awarded the Chancellor's Gold Medal at Cambridge for one of his first pieces, "Timbuktu". He published his first solo collection of poems, ''Poems, Chiefly Lyrical'', in 1830. "Claribel" and "Mariana", which remain some of Tennyson's most celebrated poems, were included in this volume. Although described by some critics as overly sentimental, his verse soon proved popular and brought Tennyson to the attention of well-known writers of the day, including Samuel Taylor Coleridge. Tennyson's early poetry, with its medievalism and powerful visual imagery, was a major influence on the Pre-Raphaelite Brotherhood. Tennyson also excelled at short lyrics, such as "Break, Break, Break", "The Charge of the Light Brigade", "Tears, Idle Tears", and "Crossing the Bar". Much of his verse was based on classical mythol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Lady Of Shalott
"The Lady of Shalott" is a lyrical ballad by the 19th-century English poet Alfred Tennyson and one of his best-known works. Inspired by the 13th-century Italian short prose text '' Donna di Scalotta'', the poem tells the tragic story of Elaine of Astolat, a young noblewoman stranded in a tower up the river from Camelot. Tennyson wrote two versions of the poem, one published in 1833, of 20 stanzas, the other in 1842, of 19 stanzas, and returned to the story in "Lancelot and Elaine". The vivid medieval romanticism and enigmatic symbolism of "The Lady of Shalott" inspired many painters, especially the Pre-Raphaelites and their followers, as well as other authors and artists. Background Like Tennyson's other early works, such as "Sir Galahad", the poem recasts Arthurian subject matter loosely based on medieval sources. It is inspired by the legend of Elaine of Astolat, as recounted in a 13th-century Italian ''novellina'' titled '' La Damigella di Scalot'', or ''Donna di Scalot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Winifred Holtby
Winifred Holtby (23 June 1898 – 29 September 1935) was an English novelist and journalist, now best known for her novel '' South Riding'', which was posthumously published in 1936. Biography Holtby was born to a prosperous farming family in the village of Rudston, East Riding of Yorkshire. Her father was David Holtby and her mother, Alice, was afterwards the first alderwoman on the East Riding County Council. Holtby was educated at home by a governess and then at Queen Margaret's School in Scarborough. Although she passed the entrance exam for Somerville College, Oxford, in 1917, she chose to join the Women's Army Auxiliary Corps (WAAC) in early 1918 but soon after she arrived in France, the First World War came to an end and she returned home. During this period, Holtby met Harry Pearson, the only man who stimulated romantic feelings in her, due primarily to his tales of the suffering soldiers endured during the war. In 1919, she returned to study at the University of Oxf ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cotswolds
The Cotswolds (, ) is a region in central-southwest England, along a range of rolling hills that rise from the meadows of the upper Thames to an escarpment above the Severn Valley and Evesham Vale. The area is defined by the bedrock of Jurassic limestone that creates a type of grassland habitat rare in the UK and that is quarried for the golden-coloured Cotswold stone. The predominantly rural landscape contains stone-built villages, towns, and stately homes and gardens featuring the local stone. Designated as an Area of Outstanding Natural Beauty (AONB) in 1966, the Cotswolds covers making it the largest AONB. It is the third largest protected landscape in England after the Lake District and Yorkshire Dales national parks. Its boundaries are roughly across and long, stretching southwest from just south of Stratford-upon-Avon to just south of Bath near Radstock. It lies across the boundaries of several English counties; mainly Gloucestershire and Oxfordshire, and parts ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anglian Dialects
Old English (, ), or Anglo-Saxon, is the earliest recorded form of the English language, spoken in England and southern and eastern Scotland in the early Middle Ages. It was brought to Great Britain by Anglo-Saxon settlers in the mid-5th century, and the first Old English literary works date from the mid-7th century. After the Norman conquest of 1066, English was replaced, for a time, by Anglo-Norman (a relative of French) as the language of the upper classes. This is regarded as marking the end of the Old English era, since during this period the English language was heavily influenced by Anglo-Norman, developing into a phase known now as Middle English in England and Early Scots in Scotland. Old English developed from a set of Anglo-Frisian or Ingvaeonic dialects originally spoken by Germanic tribes traditionally known as the Angles, Saxons and Jutes. As the Germanic settlers became dominant in England, their language replaced the languages of Roman Britain: Common Brit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old English
Old English (, ), or Anglo-Saxon, is the earliest recorded form of the English language, spoken in England and southern and eastern Scotland in the early Middle Ages. It was brought to Great Britain by Anglo-Saxon settlement of Britain, Anglo-Saxon settlers in the mid-5th century, and the first Old English literature, Old English literary works date from the mid-7th century. After the Norman conquest of 1066, English was replaced, for a time, by Anglo-Norman language, Anglo-Norman (a langues d'oïl, relative of French) as the language of the upper classes. This is regarded as marking the end of the Old English era, since during this period the English language was heavily influenced by Anglo-Norman, developing into a phase known now as Middle English in England and Early Scots in Scotland. Old English developed from a set of Anglo-Frisian languages, Anglo-Frisian or Ingvaeonic dialects originally spoken by Germanic peoples, Germanic tribes traditionally known as the Angles, Sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Riding Of Yorkshire
The East Riding of Yorkshire, or simply East Riding or East Yorkshire, is a ceremonial county and unitary authority area in the Yorkshire and the Humber region of England. It borders North Yorkshire to the north and west, South Yorkshire to the south-west, and Lincolnshire to the south. The coastal towns of Bridlington, Hornsea and Withernsea are popular with tourists, the town of Howden contains Howden Minster, Market Weighton, Pocklington, Brough, Hedon and Driffield are market towns with markets held throughout the year and Hessle and Goole are important port towns for the county. The port city of Kingston upon Hull is an economic, transport and tourism centre which also receives much sea freight from around the world. The current East Riding of Yorkshire came into existence in 1996 after the abolition of the County of Humberside. The county's administration is in the ancient market town of Beverley. The landscape is mainly rural, consisting of rolling hills, valley ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
