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엘믈리 로벳

가장 멋진 명소 20곳


엘믈리 로벳에는 둘러볼 만한 장소가 많답니다. 하이킹 또는 사이클링을 좋아한다면 엘믈리 로벳에 숨겨진 20
가지 보석을 만날 수 있을 거예요. 이 지역의 주요 명소를 살펴보면서 다음 모험을 계획해보세요.

마지막 업데이트: 2월 26, 2026

뷰들리 브리지

하이라이트 • 카페

Great little town to grab a Tea and some cake

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Burlish Top 자연 보호구역

하이라이트 • 자연

An important area of lowland heath, Burlish Top Nature Reserve is 86 acres (35 ha) and a lovely place to ramble around. Grassland, oak and birch scrub provide a vital …

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최고의 싱글 트랙, 봉우리 및 다양한 흥미로운 야외 장소에 대한 추천을 받아보세요.

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타드비그 잠금장치

하이라이트 • 자전거 도로

Make sure you've got the right tyres on your bike. I was riding my tourer and the tyres needed to be a bit more aggressive for the muddy tow path.

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채드슬리 우드 국립 자연 보호구역

하이라이트 • 자연 기념물

Chaddesley Woods were probably mentioned in the Domesday Book as the ‘wood of two leagues’ and we think that parts of the site have been wooded since the Ice Age …

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리프게이트 옛 철도 노선

하이라이트 • 트레일

The ‘Old Railway Line’ cuts through the red sandstone bedrock. These sandstones are Triassic in age, belonging to the ‘Sherwood Sandstone Group’ of rocks.

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커뮤니티 팁

Clive G
2월 8, 2026, Burlish Top Nature Reserve

One of the highlights of this part of the Geopark Way, rather better than walking through Stourport.

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AnNa
6월 22, 2025, Tardebigge Locks

John Corbett Way

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Marc
5월 10, 2025, Tardebigge Locks

Watch out for walkers around some of the locks. Few blind corners.

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Incredibly muddy - wear wellies!

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The nature reserve is approximately 35 hectares (86 acres) in size. The dominant habitat is heath and acid grassland, surrounded by oak and birch scrub. The acid grassland has been surveyed by many professional bodies, and Natural England rated it as the best quality acid grassland in the county. Wildlife on the site is typical for what you would expect on a heathland site, while reptiles are scarce due to the levels of disturbance from the public; however common lizard, grass snake and slow worm have been seen. There are many notable species of solitary bee and wasp which make use of the bare sandy soil, as do unusual heathland specialists, the green tiger beetle. The open areas are also utilised by a variety of ground feeding birds such as green woodpecker and as nesting sites for rarities like woodlark. There are a few small pools on site; one in particular supports a good breeding population of smooth newt, common frog, various dragonflies, damselflies and great diving beetle. Although traditionally a heath, this has given way in the main to gorse and broom scrub. There has been an increase in the density of rare grey hair grass after scrub clearance carried out in previous years. The area has an interesting history, with the site being used as a World War II American Army training and hospital camp. All that remains from those days are concrete paths, and some foundations from the original buildings. Much of this has been highlighted along a way marked ‘History’ trail. The website 'Burlish Camp' has more on the history of the site. In addition to the history trail, there are 3 other trails around the site, including 2 easy going routes, which take advantage of the sites historical concrete tracks, and a heathland circular, which also incorporates much of the Rifle Range SSSI. Source: Wyre Forest District Council

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The ‘Old Railway Line’ cuts through the red sandstone bedrock. These sandstones are Triassic in age, belonging to the ‘Sherwood Sandstone Group’ of rocks. The Sherwood Sandstone Group, the older Permian-aged Bridgnorth Sandstone and the younger Triassic-aged Mercia Mudstone Group have one thing in common; they were deposited in a vast rift basin, called the Worcester Basin. The Worcester Basin was north-south orientated and formed during the Permian period. Its western edge, in the Geopark area, followed the line of a major fault-line, the East Malvern Fault. In the present day this fault line is most clearly marked by the Malvern, Suckley and Abberley Hills. The eastern edge of the Basin followed the line of another major fault-line, the Inkberrow Fault. Into this basin a great variety of different sedimentary rocks were deposited and formed. Some were windblown deposits, others were despotised by streams and rivers, evaporate deposits also formed in lakes and the other significant deposit was alluvial fans that formed along the edge of the basin. Each of the rocks represents the changing environments experienced in the basin through the passage of time. The rocks seen along the ‘Old Railway Line’ belong to the Wildmoor Sandstone Formation, part of the Sherwood Sandstone Group of rocks. They are around 220 million years ago and comprises soft, weakly cemented, pale red-brown, micaceous, sandstones. The well-rounded, evenly sized grains suggest reworking of windblown sands that were deposited the Worcester Basin during the Permian period. Source: geopark.org

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Bewdley was once an important inland port, connecting Shrewsbury with the Midlands and the seaports of Gloucester and Bristol. Originally the quays were shorter and had slipways between them. In time, as more landing space was needed, the quayside walls were joined into one continuous length. The larger boats, known as Severn Trows, carried local goods such as rope and charcoal, metal goods from Birmingham and Staffordshire pottery to the south. They returned laden with woollen cloth, wine, spirits, tobacco, sugar, spices, citrus fruit and dried fish to be sold in market towns across the West Midlands and Welsh borders. This civic space was developed when the Environment Agency built the Town's new flood defences, and incorporates work by artist Elizabeth-Jane Grose. On the lower quayside you can find flowing words relating to the river and the vessels that worked on it. On the upper quayside have a look for the 'cargo-plates' recording forty of the common and less common exports and imports to the Port of Bewdley. Source: Environment Agency

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Bewdley Bridge over the Severn was built in 1798 by Thomas Telford. It was erected to replace the 1483 medieval bridge that was swept away in the floods of 1795.

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