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가장 멋진 말로우 바텀 주변 자연유산 20곳


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마지막 업데이트: 3월 3, 2026

브릭 앤 타일 웍스

하이라이트 • 역사적 장소

The Brick and Tile Works, established by Charles Cooper in the early 1800s, employed about 150 people and produced bricks, tiles, gargoyles, and pinnacles. The site, which closed in 1967, …

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파크 우드의 연못

하이라이트 • 호수

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 …

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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 …

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Cock Marsh 습지 산책로

하이라이트 • 트레일

The wetland meadows of Cock Marsh are very important for rare plant species, breeding waders and overwintering birds. Part of the site is designated as a Site of Special Scientific …

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브레이든햄 밸리

하이라이트 • 협곡

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 …

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Grace Mulligan
7월 5, 2023, The Brick and Tile Works

The Brick and Tile Works, established by Charles Cooper in the early 1800s, employed about 150 people and produced bricks, tiles, gargoyles, and pinnacles. The site, which closed in 1967, is now owned by the National Trust and features lowland ponds with diverse aquatic life and a variety of woodland birds and plants.

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The Brick & Tile Works The Brick and Tile Works was established by Charles Cooper in the early 1800s, exploiting a local deposit of Reading Clay. At its peak, the Works employed about 150 people, and cottages were built in Golden Ball Lane for the skilled craftsmen. In 1950, the Cooper family sold the Works to the Maidenhead Brick and Tile Company, and the site eventually closed in 1967. In addition to bricks and tiles, the works produced gargoyles and pinnacles, many of which can be seen in the locality today. The National Trust acquired the site in 1989. The industrial activity left a legacy of lowland ponds, inhabited by an impressive range of aquatic invertebrate fauna, including several species of dragonfly. There are also three species of newt and a wide range of woodland birds and other aquatic or semi-aquatic plants and animals.

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The wetland meadows of Cock Marsh are very important for rare plant species, breeding waders and overwintering birds. Part of the site is designated as a Site of Special Scientific Interest (SSSI). The steep chalk grassland swiftly changing into marshy, acid meadows has created an ecosystem of rare and interesting species. As part of the historic channel of the Thames, the ponds here support specialist plants like water violet, marsh arrowgrass, marsh stitchwort, marsh pennywort and water hemlock. The rare sedge Cyperus fuscus (brown galingale) is found here and in only a handful of other sites in Great Britain. It relies on cattle to tread or poach the ground on the pond edges to create the perfect habitat to grow. The cattle here work hard to help to maintain a rich botanical diversity of grassland habitat. https://www.nationaltrust.org.uk/maidenhead-and-cookham-commons/trails/cookham-and-cock-marsh-walk

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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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Edvard
4월 28, 2018, Bradenham Valley

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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