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The Woburn Sands Formation is a geological formation in England. Part of the Lower Greensand Group, it is the only unit of the group where it occurs, and thus is sometimes simply referred to as the 'Lower Greensand' in these areas. It was deposited during the late Aptian to early Albian stages of the Early Cretaceous.
North and west of London – including Cambridgeshire, Bedfordshire and Buckinghamshire – it is referred to as the Woburn Sands Formation. In Oxfordshire it is known as the Faringdon Sand. In North Wiltshire as the Calne Sands Formation and in parts of Wiltshire, Oxfordshire and Buckinghamshire as the Seend Ironstone Formation.
Woburn Sands Formation; Y. Yat Rock This page was last edited on 19 July 2022, at 15:47 (UTC). Text is available under the Creative Commons Attribution ...
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Woburn Sands Formation; Y. Yoredale Series This page was last edited on 2 November 2019, at 03:20 (UTC). Text is available under the Creative Commons Attribution ...
The ecclesiastic parish of Wavendon anciently contained the hamlet of Woburn Sands (originally known as 'Hogsty End, [3] Wavendon'), which became a separate civil parish in 1907. The parishes are separated by the Marston Vale line .
Woburn Sands (/ ˈ w oʊ b ər n /) is a town that straddles the border between Buckinghamshire and Bedfordshire in England, and is part of the Milton Keynes urban area. [2] The larger part of the town is in Woburn Sands civil parish, which is in the City of Milton Keynes, [3] Smaller parts of the town are in the neighbouring parishes of Aspley Guise and Aspley Heath (in Central Bedfordshire). [1]