The Yorkshire Dales are an upland area of the Pennines in England. Most of the area is in the county of North Yorkshire, but it extends into Cumbria and a small part of Lancashire. It was historically entirely within Yorkshire. The majority of the Dales are part of the Yorkshire Dales National Park, created in 1954. The exception is the area around Nidderdale, which forms the separate Nidderdale Area of Outstanding Natural Beauty.
The mountains of Whernside, Ingleborough and Pen-y-ghent are collectively known as the Three Peaks. The peaks, which form part of the Pennine range, encircle the head of the valley of the River Ribble in the Yorkshire Dales National Park in the North of England.
The River Swale in Yorkshire, England, is a major tributary of the River Ure, which becomes the River Ouse, that empties into the North Sea via the Humber Estuary. The river gives its name to Swaledale, the valley through which it flows.
Ingleton is a village and civil parish in the Craven district of North Yorkshire, England. The village is 19 miles (30 km) from Kendal and 17 miles (28 km) from Lancaster on the western side of the Pennines. It is 9.3 miles (15 km) from Settle. The River Doe and the River Twiss meet to form the source of the River Greta, a tributary of the River Lune. The village is on the A65 road and at the head of the A687. The B6255 takes the south bank of the River Doe to Ribblehead and Hawes. All that remains of the railway in the village is the landmark Ingleton Viaduct. Arthur Conan Doyle was a regular visitor to the area and was married locally, as his mother lived at Masongill from 1882 to 1917. It has been claimed that there is evidence that the inspiration for the name Sherlock Holmes came from here.
Hardraw Force is a waterfall on Hardraw Beck in Hardraw Scar, a wooded ravine just outside the hamlet of Hardraw, 0.9 miles (1.5 km) north of the town of Hawes, Wensleydale, in the Yorkshire Dales. The Pennine Way long distance footpath passes close by.
Kisdon Force is a series of waterfalls on the River Swale in Swaledale, England. The falls are situated within the Yorkshire Dales National Park in the county of North Yorkshire, 500 metres downstream from the small hamlet of Keld at grid reference NY898010.
Kisdon, also called Kisdon Hill, is a fell situated in upper Swaledale in the Yorkshire Dales National Park in North Yorkshire, England.
East Gill Force is a waterfall in Swaledale, 330 yards (300 m) east of the hamlet of Keld, in the Yorkshire Dales National Park, North Yorkshire, England. The falls are located on East Gill at grid reference NY896012, just before its confluence with the River Swale at the point where the Pennine Way and the Coast to Coast Walk intersect. The falls are a popular spot for visitors, not just long-distance walkers but also families and picnickers because of the proximity of the road. East Gill Force has two main torrents: the upper falls have an impressive 15-foot (4.5 m) drop whilst the lower section is a series of stepped cascades that fall 9.8 feet (3 m) as East Gill enters the River Swale.
Wain Wath Force is a waterfall on the River Swale in the Yorkshire Dales National Park, North Yorkshire, England. The falls are at grid reference NY883015, 0.6 miles (1 km) upstream from the hamlet of Keld which has three other waterfalls in its vicinity. The names of waterfalls in the north of England often contain "force" after the Old Norse word foss, which means "waterfall".
The River Doe is a river in North Yorkshire, England. The river's source is near God's Bridge close to the settlement of Chapel-le-Dale and flows through Twisleton in a south-westerly direction to Ingleton, where it meets the River Twiss to form the River Greta. The river forms part of the River Lune system that flows into the Irish Sea.
Ingleton Waterfalls Trail is a well-known circular trail beginning and ending in the village of Ingleton in the English county of North Yorkshire, now maintained by the Ingleton Scenery Company. It is claimed that the trail, some 8 kilometres (5 mi) long, and with a vertical rise of 169 m (554 feet) has some of the most spectacular waterfall and woodland scenery in the north of England. It is on private land and an entrance fee is charged.
Scar End is a settlement on the side of Twisleton Scar in the English county of North Yorkshire.
The Craven Fault System is the name applied by geologists to the group of crustal faults in the Pennines that form the southern edge of the Askrigg Block and which partly bounds the Craven Basin. Sections of the system's component faults which include the North, Middle and South Craven faults and the Feizor Fault are evident at the surface in the form of degraded faults scarps where Carboniferous Limestone abuts millstone grit. The fault system is approximately coincident with the southwestern edge of the Yorkshire Dales National Park and the northeastern edge of the Bowland Fells.
Kingsdale is a valley on the western edge of the Yorkshire Dales National Park in northern England. The name Kingsdale derives from a combination of Old Norse and Old English which means The valley where the cows were kept. Humans were active in Kingsdale from 6,700 BC onwards. Evidence of fire-pits used by hunter-gatherers have been found in the dale.
Weathercote Cave is a natural solutional cave in Chapel-le-Dale, North Yorkshire, England. It has been renowned as a natural curiosity since the eighteenth century, and was accessible to paying visitors until 1971. The entrance is a large shaft about 20 metres (66 ft) deep, dominated by a waterfall entering at one end. It lies within the designated Ingleborough Site of Special Scientific Interest.
Yordas Cave is a solutional cave in Kingsdale, North Yorkshire, England. It has been renowned since the eighteenth century as a natural curiosity, and was a show cave during the nineteenth century. It is now a popular destination for cavers, walkers, and outdoor activity groups.
Swinsto Cave is a limestone cave in West Kingsdale, North Yorkshire, England. It leads into Kingsdale Master Cave and it is popular with cavers as it is possible to descend by abseiling down the pitches, retrieving the rope each time, and exiting through Valley Entrance of Kingsdale Master Cave at the base of the hill. It is part of a 27-kilometre (17 mi) long cave system that drains both flanks of Kingsdale.
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. It is noted for its karst landscape which includes extensive areas of limestone pavement and large numbers of caves including Britain's longest cave network.
Chapel-le-Dale is west-facing valley in the Yorkshire Dales, England. The U-shaped valley of Chapel-le-Dale is one of the few which drain westwards towards the Irish Sea, however, the river that flows through the valley has several names with the Environment Agency and the Ordnance Survey listing it as the River Doe. However, some older texts insist the name of the watercourse through the dale is the River Greta, which runs from a point below the hamlet of Chapel-le-Dale, and onwards past Ingleton. The dale is sparsely populated with only one settlement, the hamlet of Chapel-le-Dale, which has a small chapel.
River Twiss,Raven Ray footbridge. To the north the limestone slopes of Keld Head Scars rise to the summit of Gragareth
Manor Bridge over River Twiss
Cuckoo Island in the River Twiss
River Twiss seen from the road bridge in Ingleton
Pecca Falls, River Twiss, near Ingleton
Thornton Force, River Twiss, Ingleton
