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마지막 업데이트: 3월 3, 2026
하이라이트 • 구조물
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There is a lovely little weir on the River Chess here that's worth stopping by. Also, on the same pond, you will see stepping stones (called Steps of Heaven by some) if you'd like to walk across! A good few years ago, I used to live in the street right next to these ponds, so I can vouch for the fact that this is a great place to spend some time at, particularly in the summer.
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There is a lovely little weir on the River Chess here that's worth stopping by. Also, on the same pond, you will see stepping stones (called Steps of Heaven by some) if you'd like to walk across! A good few years ago, I used to live in the street right next to these ponds, so I can vouch for the fact that this is a great place to spend some time at, particularly in the summer.
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its ok but muddy to get in and out of if you want to dip your feet during a hike
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Legend has it that whoever walks on these steps without falling will be blessed with eternal life.
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Located just outside Cholesbury village, Cholesbury Camp was once an important fort. It was built between the 6th Century BC and 1st Century AD, but the exact date of its construction is unknown. The Iron Age Hill Fort is well-preserved. Today, you can visit the 15-acre camp and see the oval-shaped area with its ramparts. Cholesbury Camp is a scheduled ancient monument.
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Archaeological Surveys undertaken in Park Wood have revealed a fascinating past for this quiet area of deciduous woodland. Lynchets and banks within the woods give evidence of ancient field systems which may date back to the late Iron Age/early Roman period (or they may be medieval). In the beech woodland opposite the pond is evidence of a late thirteenth/early fourteenth homestead in the woodlands and in Tudor times (1485 – 1603) the woodland was a deer park. Much of Park Wood was converted to beech woodland from the late 18th until the early 20th century to cater for the High Wycombe furniture industry. Associated features include sawpits, tracks and charcoal burning platforms. https://www.nationaltrust.org.uk/chilterns-countryside/trails/bradenham-beech-woods-and-bunkers-trail
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Like other major valleys or gaps in the Chilterns that run approximately North-South, the Bradenham valley was predominantly formed during Pleistocene Epoch (the Ice Ages), between 2.5 million and 10,000 years ago. Like most other Chiltern valleys, it is now a dry valley because the underlying chalk is permeable to water. During the Ice Age, in permafrost conditions, water could not pass through the frozen ground. Seasonal thawing, particularly of the ice sheets to the north, would have released large amounts of water, which would have cut down into the chalk to create the present “fossil” valley. https://www.nationaltrust.org.uk/chilterns-countryside/trails/bradenham-beech-woods-and-bunkers-trail
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Bluebells are well-known for forming carpets of bright blue flowers beneath our oak and beech woodlands in the late spring. At this time of year, they can also be found along hedgerows and in woodland clearings. Their spectacular floral displays are exclusive to northern Europe, with Britain containing more than half of the world’s population of bluebells. Bluebells, which are inedible members of the asparagus family of plants, are perennial bulbous herbs with flowering stems to about 50cm tall. They spend most of the year as bulbs underground and emerge to flower from mid-April onwards, although they are usually at their peak in the first two weeks of May, depending on the spring weather. Up to twenty sweetly-scented flowers are borne on a flower stalk which droops to one side. The flowers are bell-shaped and although they are usually blue, they can be white or rarely pink. https://www.nationaltrust.org.uk/chilterns-countryside/features/discover-bluebells-in-the-chiltern-countryside
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