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Geology Of Suffolk
The geology of Suffolk in eastern England largely consists of a rolling chalk plain overlain in the east by Neogene clays, sands and gravels and isolated areas of Palaeocene sands. A variety of superficial deposits originating in the last couple of million years overlie this 'solid geology'. Cretaceous The oldest rocks exposed at the surface in Suffolk are the mudstones and sandstones of the Gault and Upper Greensand formations which are to be found only in the extreme northwest of the county west of Lakenheath. Overlying these deposits and to their east are the rocks of the Chalk which are divided into the lower i.e. older Grey Chalk and the upper i.e. younger White Chalk. Palaeogene There are isolated pockets of Palaeocene sands and clays north of Ipswich and between there and Sudbury to the west. The clays of the early Eocene Harwich Formation are widespread in the southeast of the county between Sudbury and Orford Ness. Neogene From Bury St Edmunds and Sudbury east ... [...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] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing a faunal interchange between the two reg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Suffolk
Geography (from Greek: , ''geographia''. Combination of Greek words ‘Geo’ (The Earth) and ‘Graphien’ (to describe), literally "earth description") is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of Earth. The first recorded use of the word γεωγραφία was as a title of a book by Greek scholar Eratosthenes (276–194 BC). Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be. While geography is specific to Earth, many concepts can be applied more broadly to other celestial bodies in the field of planetary science. One such concept, the first law of geography, proposed by Waldo Tobler, is "everything is related to everything else, but near things are more related than distant things." Geography has been called "the world discipline" and "the bridge between the human and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Broads
This article describes the geology of the Broads, an area of East Anglia in eastern England characterised by rivers, marshes and shallow lakes (‘broads’). The Broads is designated as a protected landscape with ‘ status equivalent to a national park’. The area is underlain by a suite of generally flat-lying sedimentary rock types of which the most recent are those of Neogene age. Almost entirely covered by more recent superficial deposits, they are exposed at the surface to a very limited extent or else are known from boreholes or quarry workings. Overlying these across much the larger part of the 'national park' are silts and clays of Flandrian age, which together with peat deposits form the broad flats of the Waveney, Yare, Bure and Thurne valleys. Extraction of the peat in historic times, and subsequent flooding of the workings, has resulted in the pattern of broads for which the area is widely known. Older subsurface rocks Borehole, seismic and other geophysical surv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of England
The geology of England is mainly sedimentary. The youngest rocks are in the south east around London, progressing in age in a north westerly direction.Southampton University retrieved 21/1/07 The marks the division between younger, softer and low-lying rocks in the south east and the generally older and harder rocks of the north and west which give rise to higher relief in those regions. The geology of England is recognisable in the landscape of its , the building materials of its towns and its regional |
Geology Of The United Kingdom
The geology of Great Britain is renowned for its diversity. As a result of its eventful geological history, Great Britain shows a rich variety of landscapes across the constituent countries of England, Wales and Scotland. Rocks of almost all geological ages are represented at outcrop, from the Archaean onwards. Overview Seismographical research shows that the crust of the Earth below Great Britain is from 27 to 35 km (17 to 22 miles) thick. The oldest surface rocks are found in north west Scotland and are more than half as old as the planet. These rocks are thought to underlie much of Great Britain (although boreholes have only penetrated the first few kilometres), but next appear extensively at the surface in Brittany and the Channel Islands. The youngest rocks are found in south east England. Bedrock and past volcanism The bedrock geology consists of a complex mix of generally older metamorphic rocks overlain by varying sequences of sedimentary rocks into both of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Gipping
The River Gipping is the source river for the River Orwell in the county of Suffolk in East Anglia, England, which is named from the village of Gipping, and which gave its name to the former Gipping Rural District. The name is unrelated to the name of Ipswich. although the County Town takes its name from Gippeswic. It rises near Mendlesham Green and flows in a south-westerly direction to reach Stowmarket. From there it flows towards the south or south east, passing through Needham Market and a number of villages to reach Ipswich, where it becomes the Orwell. The river has supplied power to a number of watermills, several of which are still standing. None is operational, although the mill at Baylham retains most of its machinery, and is the only complete mill on the river. There is evidence that the river was used for navigation in the thirteenth and seventeenth centuries, but in 1790 the Ipswich and Stowmarket Navigation Act 1790 was obtained to enable the river to be im ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Waveney
The River Waveney is a river which forms the boundary between Suffolk and Norfolk, England, for much of its length within The Broads. The "ey" part of the name means "river" thus the name is tautological. Course The source of the River Waveney is a ditch on the east side of the B1113 road between the villages of Redgrave, Suffolk and South Lopham, Norfolk. The ditch on the other side of the road is the source of the River Little Ouse which continues the county boundary and, via the Great Ouse, reaches the sea at King's Lynn. It is thus claimed that during periods of heavy rainfall Norfolk can be considered to be an island. The explanation of this oddity is that the valley in which the rivers rise was formed not by these rivers, but by water spilling from the periglacial lake known as Lake Fenland. This was a periglacial lake of the Devensian glacial period, fifteen or twenty thousand years ago. The ice sheet closed the natural drainage from the Vale of Pickering, the Humber ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Stour, Suffolk
The River Stour () is a river in East Anglia, England. It is long and forms most of the county boundary between Suffolk to the north, and Essex to the south. It rises in eastern Cambridgeshire, passes to the east of Haverhill, through Cavendish, Bures, Sudbury, Nayland, Stratford St Mary, Dedham and flows through the Dedham Vale Area of Outstanding Natural Beauty. It becomes tidal just before Manningtree in Essex and joins the North Sea at Harwich. Etymology and usage The name is of ambiguous and disputed origin. On one theory, the name ''Stour'' derives from the Celtic ''sturr'' meaning "strong". However, the river-name ''Stour'', common in England, does not occur at all in Wales; Crawford noted two tributaries of the Po River near Turin, spelled ''Stura''. In Germany the ''Stoer'' is a tributary of the River Elbe. According to ''Brewer's Britain and Ireland'' the ''Stour'' is pronounced differently in different cases: the Kentish and East Anglian Stours rhyme with ''to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orford, Suffolk
Orford is a village with historic town status in Suffolk, England, within the Suffolk Coast and Heaths AONB. It is located east of Woodbridge. History Like many Suffolk coastal towns it was of some importance as a port and fishing village in the Middle Ages. It has a mediaeval castle, built to dominate the River Ore and a Grade I listed parish church, St Bartholomew's. The castle was built as a royal castle built by Henry II in the period 1165-1173 as an assertion of monarchical power in the region. Although the castle became less important after the king's death in 1189, the importance of Orford as a port grew. By 1200 its level of trade exceeded that of nearby Ipswich. Henry III granted Orford its first charter and the town returned a member of parliament in 1298, although it did not function as a constituency throughout the 14th century. Local amenities The population of Orford greatly increases during the summer months, partly due to its flourishing sailing club. In ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aldeburgh
Aldeburgh ( ) is a coastal town in the county of Suffolk, England. Located to the north of the River Alde. Its estimated population was 2,276 in 2019. It was home to the composer Benjamin Britten and remains the centre of the international Aldeburgh Festival of arts at nearby Snape Maltings, which was founded by Britten in 1948.Aldeburgh Town Council Retrieved 9 January 2016.Archives Hub Retrieved 7 March 2019. It also hosts an annual poetry festival and several food festivals and other events. Aldeburgh, as a port, gained borough status in 1529 under [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Corralline Crag Formation
The Coralline Crag Formation is a geological formation in England. It is a series of marine deposits found near the North Sea coast of Suffolk and characterised by bryozoan and mollusc debris. The deposit, whose onshore occurrence is mainly restricted to the area around Aldeburgh and Orford,Suffolk Natural England. Retrieved 8 August 2016. is a series of bioclastic s and y sands with shell debris, deposited during a s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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