Английская Википедия:Alderbury-Mottisfont Syncline

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Версия от 13:02, 27 января 2024; EducationBot (обсуждение | вклад) (Новая страница: «{{Английская Википедия/Панель перехода}} {{Use dmy dates|date=April 2022}} The '''Alderbury-Mottisfont Syncline''' is an east–west trending fold in the Cretaceous chalk of Hampshire. It lies to the north of the Dean Hill Anticline and south of Salisbury Plain. ==Structure== The syncline runs west about {{convert|16|km|mi}} from the River Test near Mottisfont to the Hamps...»)
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Шаблон:Use dmy dates The Alderbury-Mottisfont Syncline is an east–west trending fold in the Cretaceous chalk of Hampshire. It lies to the north of the Dean Hill Anticline and south of Salisbury Plain.

Structure

The syncline runs west about Шаблон:Convert from the River Test near Mottisfont to the Avon at Alderbury, south-east of Salisbury.[1]

The centre of the syncline is occupied by palaeogene rocks of the Reading Formation, London Clay and Wittering Formation. To the north and south the chalk emerges.[2][3] At the western end to the south-east of Salisbury the structure is cut by the Mere Fault.[4]

See also

List of geological folds in Great Britain

References

Шаблон:Reflist


Шаблон:Regional-geology-stub