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Clare, Suffolk
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Clare, Suffolk : ウィキペディア英語版
Clare, Suffolk

Clare is a small town on the north bank of the River Stour in Suffolk, England. Clare is from Bury St Edmunds and from Sudbury. It lies in the "South and Heart of Suffolk".〔(South and Heart of Suffolk )〕 As a cloth town, it is one of Suffolk's "threads".〔(Suffolk's 'threads' )〕 Clare won Village of the Year in 2010〔(Suffolk Village of the Year )〕 and Anglia in Bloom award for Best Large Village 2011 for its floral displays in 2011. In March 2015 The Sunday Times and Zoopla〔Sunday Times, supplement: Best Places to Live: Rural, 1 March 2015〕 placed Clare amongst the top 50 UK rural locations, having "period properties and rich history without the chocolate-box perfection – and the coach trips". Within Suffolk Walberswick was also mentioned.
Clare and its vicinity reveals evidence of man's long habitation throughout prehistory. The historical record demonstrates a community which changes and yet persists across centuries, from the Norman Conquest through religious strife, agricultural upheaval and industrial revolution to the present day.
The town hosts Stour Valley Community School, one of the very first free schools established by the government,〔(Stour Valley Community School )〕 opened in September 2011.
As part of the Heritage Lottery Funded (Managing a Masterpiece ) scheme, in April and May 2011 (Access Cambridge Archaeology ) gave residents, school pupils and members of the public the chance to carry out their own small archaeological 'test pit' excavations throughout Clare to find out how the town developed over hundreds - even thousands - of years in the past. Early results indicate the presence of Saxon pottery across many sites - the first evidence of Clare's importance before the Normans. Further excavations within the Castle grounds took place (in 2013 ): the finding of several human remains suggest a cemetery was located there, before the castle's construction.
== Geology ==
This area of the country was formed during the Tertiary period, containing some of the youngest rock in the British Isles. Like the vast majority of Suffolk, the surface 'rock' is the very fertile boulder clay or clay loam, lying on top of layers of chalk. The landscape surrounding the Stour Valley is the result of the joint effects of past glaciation and the agricultural alteration of the land. Originally the area was under the sea; the shells of the sea creatures dropped to bed of the ocean and formed into chalk about 140 million years ago. Another mineral, silica, filled the sponges and other similar animals in the sea. As this was left behind it formed nodules of hard flint. A ridge of Cretaceous chalk left by the ancient sea juts into Suffolk from Cambridgeshire. This ridge is never more than 140 metres above sea level but it makes what is called High Suffolk. This chalk layer forms the so-called solid rock layer. This chalk was originally quarried where it came to the surface, and was either burned to produce agricultural lime or was mixed with sand, quarried locally, for mortar used in building (hence the presence of cream bricks ('Suffolk whites') for houses in the area). Chalk in the water makes it 'hard' (classified as 'very hard; 511 mg/l as calcium carbonate) according to (Anglian Water's water quality ).
During the Ice Age, the sea level was some 200 metres lower than it is today. Melt water carried debris and flowed beneath the glacier under high pressure, to produce tunnel valleys, deeply incised water routes. At Clare it is as far as 110 metres below our present sea level. The valley was subsequently filled with boulder clay and gravel. The ice sheet, which produced the chalky boulder clay, rolled upon a bed of glacial sand and gravel, and formed the flattened character of the area today.〔() Geology of Great Bradley〕
The main river running through the country park is not the Stour. This is a mill stream called the 'new cut', established to operate a mill belonging to the priory, in use in the 14th century. It is joined at the eastern end of the country park by the Chilton stream. This itself is fed by the Hawedych, and by another stream coming down from Poslingford. The smaller Stour now runs south of the country park, meandering around the priory and meadows.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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