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Geological notes and local details for 1:10 000 sheet TM 35 SE (Snape) : part of 1:50 000 sheets 190 (Eye) and 208 (Woodbridge)

机译:1:10 000张Tm 35 sE(斯内普)的地质记录和当地详情:1:50 000张190(眼睛)和208张(伍德布里奇)的一部分

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摘要

This report describes the geology of the 1:10 000 sheet TM 35 NE whichudis included in the Eye (190) and Woodbridge (208) geological maps.udThe area was f i r s t surveyed by W Whitaker and W H Dalton as part ofudthe Old Series One-Inch sheet 50 SE published in 1883. The primaryudsix-inch survey of the Snape area was made by J A Zalasiewicz inud1982-3 under the direction of D r W A Read as Programme Manager.udUncoloured dyeline copies of the map can be obtained from the BritishudGeological Survey, Keyworth.udThe sheet area lies some 10 Km north-east of Woodbridge, Suffolk.udMost of the ground is broadly f l a t and lies a t c 20-25 m OD. It isudunderlain largely by Boulder Clay and given over to arable farming.udBoulder Clay is absent from the south-east of the area, where a broadudoutcrop of Kesgrave Sands and Gravels largely coincides withudconiferous forest.udThe south-eastwards flowing River Alde and its tributaries haveudincised wide valleys in the central and northern parts of the area.udKesgrave Sands and Gravels and the underlying Chillesford Sand cropudout in the valley sides, together with irregular masses ofudFluvio-Glacial Sand and Gravel and Boulder Clay. The wide f l a t valleyudfloors are underlain by freshwater and estuarine alluvium, and areudgiven over to arable farming with some pasture.udThe major settlement is Snape, where The Maltings is now a well-knownudconcert hall. There are two smaller settlements, Tunstall andudBlaxhall, and a number of scattered farmsteads.
机译:该报告描述了1:35 000 TM 35 NE片的地质情况,这包括在Eye(190)和Woodbridge(208)地质图中。 ud该地区最早由W Whitaker和WH Dalton作为 udthe的一部分进行了勘测。旧系列一英寸纸页50 SE于1883年出版。斯内普地区的主要 udsix英寸勘测由JA Zalasiewicz在 ud1982-3中进行,由D r WA Read作为计划经理进行。 ud该地图可从英国 ud地质调查局Keyworth处获得。 ud地表区域位于萨福克州伍德布里奇(Woodbridge)东北约10公里。 ud大部分地面较平坦,外径约为20-25 m。该地区大部分由博尔德·克莱(Boulder Clay)种植,并移交给可耕种。向东流动的阿尔德河及其支流在该地区的中部和北部使宽阔的山谷消失。还有砾石和巨石粘土。宽阔的谷底/地面被淡水和河口冲积层所覆盖,并被认为可以耕种一些牧场。有两个较小的定居点Tunstall和 udBlaxhall,以及许多分散的农庄。

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    Zalasiewicz J.A.;

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  • 年度 1988
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  • 原文格式 PDF
  • 正文语种 {"code":"en","name":"English","id":9}
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