4.5
(2156)
15,519
등산객
433
하이킹
Komoot에 등록된 스넬스톤 내 트레일 및 경로 컬렉션 중에서 하이킹과 워킹을 가장 멋지게 즐길 수 있는 곳을 알려드릴게요. 아래에서 각 경로의 상세 정보를 모두 확인한 후, 스넬스톤 속 자연에서 즐거운 시간을 누려보세요.
마지막 업데이트: 2월 24, 2026
5.0
(3)
16
등산객
11.3km
03:00
110m
110m
보통 하이킹. 좋은 체력 필요. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
4.0
(3)
9
등산객
6.71km
01:43
30m
30m
초급용 하이킹. 모든 체력 수준에 적합. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
무료 회원 가입
5.0
(1)
8
등산객
9.12km
02:24
80m
80m
보통 하이킹. 좋은 체력 필요. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
5.0
(1)
4
등산객
10.7km
02:51
120m
120m
보통 하이킹. 좋은 체력 필요. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
10
등산객
7.22km
01:56
90m
90m
초급용 하이킹. 모든 체력 수준에 적합. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
더 다양한 경로와 다른 탐험가들의 추천을 살펴보세요.
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이미 komoot 계정이 있나요?
투어 추천은 다른 사람들이 komoot에서 완료한 수천 개의 활동을 바탕으로 구성되어 있습니다.
Beautiful tunnel which is very photogenic from Ashbourne end
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The Ashbourne Tunnel runs below the town of Ashbourne itself, and serves as the begining – or, alternatively, the ending – of the Tissington Trail: a 13-mile hike, much of which comprises of disused railway lines, connecting the towns of Ashbourne and Parsley Hay. Recently renovated with speakers that transmit authentic steam-powered engine noise, Ashbourne Tunnel is a highly evocative experience that is sure to transport visitors back to the age of industry. Ashbourne was first included in the North Staffordshire Railway line in 1852, as the trade of limestone grew around the town. At the end of the 19th century, this line was taken over by the London & South Western line, who were seeking a line south of Buxton, and connected Ashbourne to the junction at Parsley Hay. This saw the construction of the Ashbourne Tunnel, which was first opened in 1899.
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Okeover Mill is a former water mill. Early C18 with later alterations and additions. Coursed limestone rubble with ashlar quoins and dressings, and red brick additions; clay tile roof; brick ridge stack.
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Okeover Hall is a privately owned Grade II* listed country house in Okeover, Staffordshire, England. It is the family seat of the Okeover family, who have been in residence since the reign of William Rufus. The house lies close to the border between Staffordshire and Derbyshire, which lies on the far side of the small River Dove. The Hall is not open to the public.
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St John the Baptist's Church is an Anglican church in the village of Mayfield, Staffordshire, England. It is a Grade I listed building. The core is a Norman church; it was extended in the early 14th century, and the tower built in 1515. There was a church in the village in Saxon times; the Domesday book, of 1086, recorded that there was a priest in the village, one of 25 recorded for Staffordshire. A simple rectangular stone building replaced the Saxon church about 1125. The south doorway (inside the later porch), with a well-preserved Norman arch, dates from this time. The nave, of three bays, is mainly Norman.
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Mayfield Yarns is a synthetic yarn manufacturer based in Mayfield, Staffordshire, with over 80 years of experience in the industry. The company is located in the Mayfield Mill, which has a long history of textile production dating back to 1795. In 1795 A cotton mill was built on an industrial site but in 1806 a fire destroyed much of the mill. It was rebuilt with a cast iron framework and brick vaulted ceilings. Brothers Joseph and George Simpson rebuilt and enlarged the mill in 1866. Mr C.H. Cowlishaw, a solicitor from Uttoxeter, purchased the mill in 1932 but sold it again two years later to William Tatton & Co. of Leek, and manufacturing switched to silk. In 1980 Mayfield Yarns began manufacturing and supplying synthetic yarns in the mill.
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The River Dove is the principal river of the southwestern Peak District, in the Midlands of England, and is around 45 miles (72 km) in length. It rises on Axe Edge Moor near Buxton and flows generally south to its confluence with the River Trent at Newton Solney. From there, its waters reach the North Sea via the Humber Estuary. For almost its entire course it forms the boundary between the counties of Staffordshire (to the west) and Derbyshire (to the east). The river meanders past Longnor and Hartington and cuts through a set of deep limestone gorges, Beresford Dale, Wolfscote Dale, Milldale and Dovedale
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