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Geology Of Norfolk
The geology of Norfolk in eastern England largely consists of late Mesozoic and Cenozoic sedimentary rocks of marine origin covered by an extensive spread of unconsolidated recent deposits. Jurassic The oldest rocks at or near the surface in Norfolk are late Jurassic mudstones and muddy limestones which underlie recent deposits in the area west of King's Lynn and Downham Market. Cretaceous Overlying the Jurassic is a Cretaceous sequence whose lowermost unit is the Wealden Group comprising mudstones, limestones, siltstones and sandstones and which extends in a band from Hunstanton southwards to south of the village of Southery. A narrow band of sandstone immediately east of this constitutes the Lower Greensand Group and beyond this, and stratigraphically above it, lie the mudstones and sandstones of the Gault and Upper Greensand formations. The Grey Chalk and the White Chalk subgroups and the Hunstanton Formation overlie the Greensand. The Chalk extends across the rest of Norfo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
England
England is a Countries of the United Kingdom, country that is part of the United Kingdom. It is located on the island of Great Britain, of which it covers about 62%, and List of islands of England, more than 100 smaller adjacent islands. It shares Anglo-Scottish border, a land border with Scotland to the north and England–Wales border, another land border with Wales to the west, and is otherwise surrounded by the North Sea to the east, the English Channel to the south, the Celtic Sea to the south-west, and the Irish Sea to the west. Continental Europe lies to the south-east, and Ireland to the west. At the 2021 United Kingdom census, 2021 census, the population was 56,490,048. London is both List of urban areas in the United Kingdom, the largest city and the Capital city, capital. The area now called England was first inhabited by modern humans during the Upper Paleolithic. It takes its name from the Angles (tribe), Angles, a Germanic peoples, Germanic tribe who settled du ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gault
The Gault Formation is a geological formation of stiff blue clay deposited in a calm, fairly deep-water marine environment during the Lower Cretaceous Period (Upper and Middle Albian). It is well exposed in the coastal cliffs at Copt Point in Folkestone, Kent, England, where it overlays the Lower Greensand formation, and underlies the Upper Greensand Formation. These represent different facies, with the sandier parts probably being deposited close to the shore and the clay in quieter water further from the source of sediment; both are believed to be shallow-water deposits. The etymology of the name is uncertain and probably of local origin. Distribution It is found in exposure on the south side of the North Downs and the north side of the South Downs. It is also to be found beneath the scarp of the Berkshire Downs, in the Vale of White Horse, in Oxfordshire, England, and on the Isle of Wight where it is known as Blue Slipper. Gault underlies the chalk beneath the London Ba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cawston, Norfolk
Cawston is a village and civil parish in the English county of Norfolk. Cawston is located 3miles south-west of Aylsham and 9miles north of Norwich. History Cawston's name is of combined Anglo-Saxon and Viking origin and derives from the Old English for a Viking named ''Kalfr's'' settlement. In the Domesday Book of 1086, Cawston was recorded as being a settlement of 26 households in the hundred of South Erpingham. In 1086, the village was divided between the estates of King William I and William de Warenne. Cawston was the scene of Norfolk's last duel, which occurred illegally in August 1698 between Sir Henry Hobart of Blickling Hall and Oliver Le Neve of Great Witchingham. The duel was fought with swords and ended with the fatal wounding of Hobart, resulting in Le Neve fleeing to the Netherlands. Today, a memorial stone to the duel is maintained by the National Trust. During the Second World War, part of Cawston Parish fell within the grounds of RAF Oulton, a satellit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sheringham
Sheringham (; population 7,367) is a seaside town and civil parish in the county of Norfolk, England.Ordnance Survey (2002). ''OS Explorer Map 252 - Norfolk Coast East''. . The motto of the town, granted in 1953 to the Sheringham Urban District Council, is ''Mare Ditat Pinusque Decorat'', Latin for "The sea enriches and the pine adorns".Town Crest and motto Retrieved 7 March 2013 History The place-name 'Sheringham' is first attested in the Domesday Book of 1086, where it appears as ''Silingeham''. It appears as ''Siringeham'' in 1174, and ''Scheringham'' in the ''Book of Fees'' (''Liber feodorum'') in 1242. The name means 'the homestead of Scira's people'. Historically, the parish of Sheringham comprised the two villages of Upper Sheringham, a farming community, and Lower Sheringham, which combined ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loddon, Norfolk
Loddon is a town and civil parish in Norfolk, England, about south-east of Norwich. The town lies on the River Chet, a tributary of the River Yare within The Broads. The name "Loddon" is thought to mean ''muddy river'' in Celtic in reference to the Chet. History Origins The earliest written mention of Loddon (Lodne) is in the will of Ælfric Modercope written in 1042 or 1043. In the will Ælfric split his land holdings in Loddon, Bergh Apton and Barton between the Bishops of Bury, Ely and St Benet of Holme. Ælfric held of land in Loddon and was by far the biggest landowner. His manor house is believed to have been close by the church overlooking the river and the fields are known as Manor Yards. The Parish Council adopted Ælfric for Loddon's town sign in 1961 and the bronze statue still stands on Farthing Green. Modern times Although Loddon and Chedgrave have been flooded many times through history, the worst or at least the best documented occasions were in August ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thames Group
The Thames Group is an Eocene lithostratigraphic group (a sequence of rock strata) which is widespread in southeast England, especially in the Hampshire Basin from Dorset through Hampshire to West Sussex and in the Isle of Wight and in the London Basin from Berkshire east through northern Hampshire, Surrey and Greater London to Essex and north Kent. It is encountered in older literature as the London Clay Group. Stratigraphy The London Clay Formation is the uppermost sub-unit of the Group. It is overlain by the lowermost units of the Bracklesham Group; these being the Bagshot Formation in the London Basin, and the Poole and Wittering formations in the Hampshire basin and English Channel. Beneath the London Clay is the Harwich Formation which itself overlies Lambeth Group strata, these being rocks of the Thanet Formation The Thanet Formation is a geological formation found in the London Basin of southeastern England. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolinite, ). Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impurities, such as a reddish or brownish colour from small amounts of iron oxide. Clays develop plasticity (physics), plasticity when wet but can be hardened through Pottery#Firing, firing. Clay is the longest-known ceramic material. Prehistoric humans discovered the useful properties of clay and used it for making pottery. Some of the earliest pottery shards have been radiocarbon dating, dated to around 14,000 BCE, and Clay tablet, clay tablets were the first known writing medium. Clay is used in many modern industrial processes, such as paper making, cement production, and chemical filtration, filtering. Between one-half and two-thirds of the world's population live or work in buildings made with clay, often baked into brick, as an essenti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene
The Eocene ( ) is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (Ma). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''Ēṓs'', 'Eos, Dawn') and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch.See: *Letter from William Whewell to Charles Lyell dated 31 January 1831 in: * From p. 55: "The period next antecedent we shall call Eocene, from ήως, aurora, and χαινος, recens, because the extremely small proportion of living species contained in these strata, indicates what may be considered the first commencement, or ''dawn'', of the existing state of the animate creation." The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isoto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeogene
The Paleogene Period ( ; also spelled Palaeogene or Palæogene) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period Ma (million years ago) to the beginning of the Neogene Period Ma. It is the first period of the Cenozoic Era, the tenth period of the Phanerozoic and is divided into the Paleocene, Eocene, and Oligocene epochs. The earlier term Tertiary Period was used to define the time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognized as a formal stratigraphic term, "Tertiary" still sometimes remains in informal use. Paleogene is often abbreviated "Pg", although the United States Geological Survey uses the abbreviation "" for the Paleogene on the Survey's geologic maps. Much of the world's modern vertebrate diversity originated in a rapid surge of diversification in the early Paleogene, as survivors of the Cretaceous–Paleogene extinction event took advantage of empty ecologica ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neogene
The Neogene ( ,) is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period million years ago. It is the second period of the Cenozoic and the eleventh period of the Phanerozoic. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene. Some geologists assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary. The term "Neogene" was coined in 1853 by the Austrian palaeontologist Moritz Hörnes (1815–1868). The earlier term Tertiary Period was used to define the span of time now covered by Paleogene and Neogene and, despite no longer being recognized as a formal stratigraphic term, "Tertiary" still sometimes remains in informal use. During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. The first human ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Suffolk
Suffolk ( ) is a ceremonial county in the East of England and East Anglia. It is bordered by Norfolk to the north, the North Sea to the east, Essex to the south, and Cambridgeshire to the west. Ipswich is the largest settlement and the county town. The county has an area of and a population of 758,556. After Ipswich (144,957) in the south, the largest towns are Lowestoft (73,800) in the north-east and Bury St Edmunds (40,664) in the west. Suffolk contains five Non-metropolitan district, local government districts, which are part of a two-tier non-metropolitan county administered by Suffolk County Council. The Suffolk coastline, which includes parts of the Suffolk & Essex Coast & Heaths National Landscape, is a complex habitat, formed by London Clay and Crag Group, crag underlain by chalk and therefore susceptible to erosion. It contains several deep Estuary, estuaries, including those of the rivers River Blyth, Suffolk, Blyth, River Deben, Deben, River Orwell, Orwell, River S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hockwold Cum Wilton
Hockwold cum Wilton is a civil parish and village in the England, English county of Norfolk. Hockwold is located west of Thetford and south-west of Norwich. History Hockwold cum Wilton's name is of Anglo-Saxon origin and derives from the Old English for the hock forest and willow-tree farmstead. In the Domesday Book of 1086, Hockwold cum Wilton is recorded as a settlement of 12 households in the Hundred (county division), hundred of Grimshoe. In 1086, the village was part of the East Anglia, East Anglian estates of William de Warenne, 1st Earl of Surrey, William de Warenne. Several Roman Empire, Roman buildings have been found in Hockwold cum Wilton including a former temple in Sawbench Woods. In 1962, a hoard of silver cups were found in the parish which are currently held by the British Museum. The only pilgrim badge of Saint Andrew to be found outside of Scotland and London was found in the parish in the 1980s. Geography According to the 2021 United Kingdom census, 2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
