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Thornton Force
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 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. Beginnings Following a number of articles in the ''Lancaster Guardian'' and other newspapers about the scenery in and around Ingleton, public interest led to the creation of the trail in an area which was previously hidden from view. Paths and bridges were built and the trail opened on Good Friday, 11 April 1885. The presence of Ingleton railway station played a major role in the early success of the trail, attracting visitors from Bradford, Manchester and Leeds. Geology Ingleton lies on the North and South Craven fault, exposing Carboniferous ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ingleton, North Yorkshire
Ingleton is a village and civil parish in the Craven district of North Yorkshire, England. The village is from Kendal and from Lancaster on the western side of the Pennines. It is 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.OS map 98, Wensleydale and Upper Wharfdale. Arthur Conan Doyle was a regular visitor to the area and was married locally, as his mother lived at Masongill from 1882 to 1917 (see notable people). It has been claimed that there is evidence that the inspiration for the name Sherlock Holmes came from here. Whernside, north-north-east of the village, one of the Yorkshire Three Peaks, is the highest point in the parish at . There are major quarries within the paris ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official period of the Paleozoic Era by the International Union of Geological Sciences, Intern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Site Of Special Scientific Interest
A Site of Special Scientific Interest (SSSI) in Great Britain or an Area of Special Scientific Interest (ASSI) in the Isle of Man and Northern Ireland is a conservation designation denoting a protected area in the United Kingdom and Isle of Man. SSSI/ASSIs are the basic building block of site-based nature conservation legislation and most other legal nature/geological conservation designations in the United Kingdom are based upon them, including national nature reserves, Ramsar sites, Special Protection Areas, and Special Areas of Conservation. The acronym "SSSI" is often pronounced "triple-S I". Selection and conservation Sites notified for their biological interest are known as Biological SSSIs (or ASSIs), and those notified for geological or physiographic interest are Geological SSSIs (or ASSIs). Sites may be divided into management units, with some areas including units that are noted for both biological and geological interest. Biological Biological SSSI/ASSIs may ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
English Nature
English Nature was the United Kingdom government agency that promoted the conservation of wildlife, geology and wild places throughout England between 1990 and 2006. It was a non-departmental public body funded by the Department for Environment, Food and Rural Affairs (DEFRA) and gave statutory advice, grants and issued licences. The Nature Conservancy Council (NCC) (formerly the Nature Conservancy) was established by the National Parks and Access to the Countryside Act 1949 to cover nature conservation issues across the whole of Great Britain. The NCC was split into four by the Environmental Protection Act 1990—its English duties being given to English Nature. In Scotland, its functions were merged with those of the Countryside Commission for Scotland to form Scottish Natural Heritage, and similarly in Wales there was a merger to form the Countryside Council for Wales. A much smaller body, the Joint Nature Conservation Committee (JNCC), supported all three agencies. The Engl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Lune
The River Lune (archaically sometimes Loyne) is a river in length in Cumbria and Lancashire, England. Etymology Several elucidations for the origin of the name ''Lune'' exist. Firstly, it may be that the name is Brittonic in genesis and derived from ''*lǭn'' meaning "full, abundant", or "healthy, pure" (c.f. Old Irish ''slán'', Welsh ''llawn''). Secondly, ''Lune'' may represent Old English ''Ēa Lōn'' (''ēa'' = "river") as a phonetic adaptation of a Romano-British name referring to a Romano-British god Ialonus who was worshipped in the area. Springs The river begins as a stream at Newbiggin, in the parish of Ravenstonedale, Cumbria, at St. Helen's Well (elevation of above sea level) and some neighbouring springs. On the first two miles of its course, it is joined by four streams, two of them as short as itself, but two much longer. These are the Bessy Beck (short), the Dry Beck of 4.9 kilometres' (three miles) length at from St. Helen's Well, the Sandwath Beck (s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Greta (Lune)
The River Greta is a river flowing through Lancashire and North Yorkshire in the north of England. The river is formed by the confluence of the River Twiss and the River Doe at Ingleton. From Ingleton, the Greta travels westwards through Burton-in-Lonsdale and, over the border in Lancashire, Cantsfield and Wrayton, passing Thurland Castle, where the Greta flows into the River Lune The River Lune (archaically sometimes Loyne) is a river in length in Cumbria and Lancashire, England. Etymology Several elucidations for the origin of the name ''Lune'' exist. Firstly, it may be that the name is Brittonic in genesis and der .... References Rivers of Lancashire Rivers of North Yorkshire Rivers of Lancaster 1Greta {{England-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chapel-le-Dale
Chapel-le-Dale is a hamlet in the civil parish of Ingleton, North Yorkshire, England. It is in the Yorkshire Dales and was previously in the West Riding of Yorkshire. History The hamlet is situated on the B6255 road between Ingleton and Ribblehead near to the Ribblehead Viaduct. The name derives from Old French and literally means ''Chapel in the valley''. It was first recorded as ''Chappell ith Dale'' in 1677. Historically, the hamlet, and its parish, were both in the Wapentake of Ewcross and up until 1974, they were in the West Riding of Yorkshire. The hamlet is in close proximity to Ingleborough and Whernside and there are several potholes in the vicinity, the best known being Great Douk Cave. There is a pub in the village, ''The Old Hill Inn'', which is used as a starting and ending point for various walks on Whernside or Ingleborough. The source of the River Doe is nearby. There is a church in the hamlet (The Church of St Leonard) which is now a grade II listed buildin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Doe
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. Course The source of the river is found at a place named God's Bridge where Chapel Beck disappears underground and the Doe begins. The river flows south west, fed by a number of small unnamed springs on the valley sides. The first named tributary is Light Water Spring which feeds north west into the river near a disused quarry. Near Twisleton Dale House, the river can be crossed by some stepping stones at a fording point as well as some later near the disused granite quarry. Further down stream near Twisleton Hall there are another set of stepping stones at a fording point just above Beezley Falls. After flowing under a footbridge, there ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scar End
Scar End is a settlement on the side of Twisleton Scar in the English county of North Yorkshire. This Scar itself is the end of a spur running westwards from Whernside, one of the Three Peaks, towards Ingleton, North Yorkshire, and the beds of limestone project to a height of above sea level. Looking out towards the west from Twisleton Scar is Ingleton, to the South, is Ingleborough, and to the north is the view up the Kingsdale valley. The settlement consists of a handful of buildings, one of which is Twisleton Hall. The road into the settlement leaves the old Roman Road from Ingleton (Oddies Lane) into Chapel-le-Dale. Visitors walking the Ingleton Waterfalls Trail 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 long, and wi ... will approach Scar End by walking along Twisleton Lane. Twisl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wish Tree
A wish tree is a tree, usually distinguished by species, location or appearance, which is used as an object of wishes and offerings. Such trees are identified as possessing a special religious or spiritual value. Postulants make votive offerings in hopes of having a wish granted, or a prayer answered, from a nature spirit, saint or goddess, depending on the local tradition. Practices Coin trees One form of votive offering is the token offering of a coin. Coin trees are found in parts of Scotland, Northern England, and Wales. Folklorist Ceri Houlbrook observed actions at a coin tree in Aira Force, Cumbria, noting that a succession of at least twelve families passed by the site and decided to hammer coins into it using a piece of limestone lying around; she commented that this custom appeared to offer "little variation: it is imitative, formulaic, homogeneous". In 2019 the National Trust for Scotland said 'For many years people have hammered coins into tree stumps and trunks as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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