The Chiltern Hills are formed by an outcrop of chalk, overlain by clay-with-flints, on the north-western side of the London basin, which stretch across southern England from the Goring Gap in Oxfordshire to near Hitchin in Hertfordshire. The chalk strata have been tilted to create a dip slope that falls gently towards the south-east. To the north-west, the hills end abruptly at a steep escarpment, which overlooks the Vale of Aylesbury.
nationaltrust.org.uk/chilterns-countryside/features/the-geology-beneath-the-chilterns-countryside

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Elevation 160 m

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Location: Bradenham, Wycombe, Buckinghamshire, South East England, England, United Kingdom

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