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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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ... [...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 Basin, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cawston, Norfolk
Cawston is a village and civil parish in the Broadland district of Norfolk, England. The village is approximately north of Norwich on the B1145 road, a route which runs between King's Lynn and Mundesley. Nearby towns are Reepham and Aylsham. History Cawston's name is of Anglo-Saxon origin and derives from the Old English for Kalfr's farmstead or settlement. In the Domesday Book, 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 and William de Warenne. Cawston was the scene of Norfolk's last duel, which occurred illegally in August of 1698 between Sir Henry Hobart of Blickling Hall and Oliver Le Neve of Great Witchingham. The duel was fought with swords and resulted in 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. Geography In the 2011 Census, Cawston w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sheringham
Sheringham (; population 7,367) is an English seaside town within the county of Norfolk, United Kingdom.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
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Loddon, Norfolk
Loddon is a small 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 A ... [...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 Formation (geology), 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. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay particles, but become hard, brittle and non–plastic upon drying or firing. 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. Clay is the oldest 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 dated to around 14,000 BC, and clay tablets were the first known writing medium. Clay is used in many modern industrial processes, such as paper making, cement production, and chemical filtering. Between one-half and two-thirds of the world's population live or work in buildings made with clay, often ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). 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'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. 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 isotope Carbon-13, 13C in the atmosphere was exceptionally low in comparison with the more common isotope Carbon-12, 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Popigai impact structure, Siberia and in what is now ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeogene
The Paleogene ( ; also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago ( Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of the Cretaceous–Paleogene extinction event that ended the preceding C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neogene
The Neogene ( ), informally Upper Tertiary or Late Tertiary, 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 Mya. 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). During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. The first humans (''Homo habilis'') appeared in Africa near the end of the period. Some continental movements took place, the most significant event being the connection of North and South America at the Isthmus of Panama, late in the Pliocene. This cut off the warm ocean currents from the Pacific to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Suffolk
Suffolk () is a ceremonial county of England in East Anglia. It borders Norfolk to the north, Cambridgeshire to the west and Essex to the south; the North Sea lies to the east. The county town is Ipswich; other important towns include Lowestoft, Bury St Edmunds, Newmarket, and Felixstowe which has one of the largest container ports in Europe. The county is low-lying but can be quite hilly, especially towards the west. It is also known for its extensive farming and has largely arable land with the wetlands of the Broads in the north. The Suffolk Coast & Heaths and Dedham Vale are both nationally designated Areas of Outstanding Natural Beauty. History Administration The Anglo-Saxon settlement of Suffolk, and East Anglia generally, occurred on a large scale, possibly following a period of depopulation by the previous inhabitants, the Romanised descendants of the Iceni. By the fifth century, they had established control of the region. The Anglo-Saxon inhabitants later b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hockwold Cum Wilton
Hockwold cum Wilton (''"Hock/mallow wood and willow-tree farm/settlement"'') is 10 miles west of Thetford, Norfolk, England and is in the borough of King's Lynn and West Norfolk. It is located near several USAF airbases, notably RAF Lakenheath and RAF Mildenhall. It is situated on the boundary between the geographical areas of the Breckland – a region of sandy heathland now largely forested – and the flat, low-lying Fens, with some characteristics of both. The village is the location of the primary campus of Iceni Academy. Previously this was Hockwold Primary School. The village has two churches ( St Peter's, now redundant and cared for by the Churches Conservation Trust, and St James') and a Methodist chapel. History An important Roman hoard of silver tableware and coins was found in Hockwold in 1962. It is now part of the Roman-British collections at the British Museum. Originally, the village was located next to the river. However, after the Black Death infected the vi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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