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The Yorkshire Dales National Park is a 2,178 km 2 (841 sq mi) national park in England which covers most of the Yorkshire Dales, the Howgill Fells, and the Orton Fells. The Nidderdale area of the Yorkshire Dales is not within the national park, and has instead been designated a national landscape.
The majority of the dales are within the Yorkshire Dales National Park, created in 1954. [1] The exception is the area around Nidderdale, which forms the separate Nidderdale Area of Outstanding Natural Beauty. The landscape of the Yorkshire Dales consists of sheltered glacial valleys separated by exposed moorland. [2]
Teesdale and its side dales, historically in the North Riding of Yorkshire, and sometimes considered part of the Yorkshire Dales, [2] [3] are in the North Pennines AONB. On 1 August 2016, the area of the National Park was increased by nearly a quarter, with an extra 161 square miles (417 square kilometres) of upland landscape given protected ...
Gunnerside is a village in North Yorkshire, England. It is situated in Swaledale, on the B6270 road, 3 miles (5 km) east of Muker and 6 miles (10 km) west of Grinton. [1] [2] The village lies between the River Swale and its tributary, Gunnerside Beck, and is within the Yorkshire Dales National Park.
The 1958 nuclear monitoring post in the Yorkshire Dales is one of 1,500 built across the UK. ... The 1958 Royal Observer Corps monitoring post in the Yorkshire Dales National Park was acquired for ...
The majority of the dale is within the Yorkshire Dales National Park; the part below East Witton is within the national landscape of Nidderdale. Addlebrough, at 481 metres (1,578 feet), dominates the landscape of the upper dale, and Penhill, at 526 metres (1,726 feet), is prominent in the lower dale.
Malham Cove is a large curved limestone formation 0.6 miles (1 km) north of the village of Malham, North Yorkshire, England. It was formed by a waterfall carrying meltwater from glaciers at the end of the last Ice Age more than 12,000 years ago. Today it is a well-known beauty spot and rock climbing crag within the Yorkshire Dales National Park.
The geology of the Yorkshire Dales National Park in northern England largely consists of a sequence of sedimentary rocks of Ordovician to Permian age. The core area of the Yorkshire Dales is formed from a layer-cake of limestones, sandstones and mudstones laid down during the Carboniferous period.