Ingleborough NNR
   HOME
*



picture info

Ingleborough NNR
Ingleborough () is the second-highest mountain in the Yorkshire Dales, England. It is one of the Yorkshire Three Peaks (the other two being Whernside and Pen-y-ghent), and is frequently climbed as part of the Three Peaks walk. A large part of Ingleborough is designated as a Site of Special Scientific Interest and National Nature Reserve and is the home of a new joint project, Wild Ingleborough, with aims to improve the landscape for wildlife and people. Name The first element of the name "Ingleborough" has been variably explained as a Scots term for 'beacon, fire', an Old Danish term meaning 'English' or a derivative of Old English ''ing'', 'peak'. The second element is derived from the Old English word ''burh'', meaning "a fortified place"; in this case, a hill fort. The summit plateau of Ingleborough is encircled by the remains of a massive stone rampart, containing the foundations of Iron Age huts. Geography Ingleborough is in the south-western corner of the Yorkshi ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Whernside
Whernside is a mountain in the Yorkshire Dales in Northern England. It is the highest of the Yorkshire Three Peaks, the other two being Ingleborough and Pen-y-ghent. It is the highest point in the ceremonial county of North YorkshireMickle Fell in southern Teesdale is the highest point within the boundaries of the historic county of Yorkshire. and the historic West Riding of Yorkshire with the summit lying on the county boundary with Cumbria. It is the fifteenth most prominent hill in England. In shape Whernside forms a long ridge, running roughly north-north-east to south-south-west. The mountain is north west of Ingleton and north of Horton-in-Ribblesdale. Name The name, first recorded in 1208 as ''Querneside'', is of Old English origin. It is derived from ''cweorn'' 'quern' or 'millstone' and ''sīde'' 'hillside', so means "hillside where millstones are found". The name is of the same origin as Great Whernside, to the east, with which it is sometimes confused. Ro ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

British Iron Age
The British Iron Age is a conventional name used in the archaeology of Great Britain, referring to the prehistoric and protohistoric phases of the Iron Age culture of the main island and the smaller islands, typically excluding prehistoric Ireland, which had an independent Iron Age culture of its own. The parallel phase of Irish archaeology is termed the Irish Iron Age. The Iron Age is not an archaeological horizon of common artefacts but is rather a locally-diverse cultural phase. The British Iron Age followed the British Bronze Age and lasted in theory from the first significant use of iron for tools and weapons in Britain to the Romanisation of the southern half of the island. The Romanised culture is termed Roman Britain and is considered to supplant the British Iron Age. The tribes living in Britain during this time are often popularly considered to be part of a broadly-Celtic culture, but in recent years, that has been disputed. At a minimum, "Celtic" is a linguistic ter ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Show Cave
A show cave—also called tourist cave, public cave, and, in the United States, commercial cave—is a cave which has been made accessible to the public for guided visits. Definition A show cave is a cave that has been made accessible to the public for guided visits, where a cave is defined as a natural occurring void beneath the surface of the earth, per the International Show Caves Association. A show cave may be managed by a government or commercial organization and made accessible to the general public, usually for an entrance fee. Unlike wild caves, they may possess regular opening hours, guided group tours, constructed trails and stairs, color artificial illumination and other lighting, musical/video/laser shows and concerts, elevators, small trains, and boats if they contain underground water features. Some caves (mainly in Asia) open to the public have temples, monasteries and religious statues or monuments. Some caves are visited by millions of tourists annually ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


White Scar Caves
White Scar Caves is a show cave in the civil parish of Ingleton, North Yorkshire, England, under Ingleborough in the Chapel-le-Dale valley of the Yorkshire Dales National Park. It is a solutional resurgence cave formed in Carboniferous limestone, some long. It was first explored in August 1923 by two amateur geologists, Christopher Long and J.H. Churchill, but further discoveries have been made since then including ''The Battlefield'', at long it is one of the largest known cave chambers in Great Britain. Originally accessed through a vertical boulder choke, an access tunnel has been cut to include it on the visitor trail. It is open as a show cave, the entrance being from the Ribblehead Ribblehead is the area of moorland at the head of the River Ribble in the area known as Ribblesdale, in the Yorkshire Dales National Park, England. Ribblehead is most notable for Ribblehead railway station and Ribblehead Viaduct on the Settl ... to Ingleton road on the west of Ing ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

River Ribble
The River Ribble runs through North Yorkshire and Lancashire in Northern England. It starts close to the Ribblehead Viaduct in North Yorkshire, and is one of the few that start in the Yorkshire Dales and flow westwards towards the Irish Sea (the Dee in Dentdale and the Twiss in Kingsdale being notable others). Etymology The name ''Ribble'' may be a Brittonic compound-formation. The second element is the noun ''*pol'', with connotations including "puddle, pond, upland-stream" (Welsh ''pwll''). The first is ''rö-'', an intensive prefix, with nouns meaning "great" (Welsh ''rhy-'', Cornish re-). Ribble may once have been known as ''*Bremetonā-'', underlying the name ''Bremetenacum'', the Roman fort at Ribchester. Involved here is the Brittonic root ''*breμ–'', meaning "roaring" (c.f. Welsh ''brefu''), as observed at the river-names Breamish in Northumberland, Braan in Scotland and Brefi in Wales. History Neolithic to Saxon finds from along the River Ribble during the ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Austwick
Austwick is a village and civil parish in the Craven district of North Yorkshire, England, about north-west of Settle. The village is on the edge of the Yorkshire Dales National Park. Before local government reorganisation in 1974, Austwick parish was within Settle Rural District which was in the County of the West Riding of Yorkshire. According to the Austwick & Lawkland Tithe Map of 21 October 1851 the parish has an area of of which around a quarter is uncut moorland. The highest point within the parish is at Lord's Seat on Simon Fell at . History The area around Austwick has been inhabited by humans for over 4,000 years. Archaeological finds in and around the village include prehistoric burial places, a large Bronze Age settlement, and even an Iron Age settlement. The area surrounding Austwick has many ancient remains including extensive walls and structures constructed of slate, limestone, and sandstone. At one time, Austwick, Clapham, Lawkland, and Newby were indepe ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Norber Erratics
The Norber erratics are one of the finest groups of glacial erratic boulders in Britain. They are found on the southern slopes of Ingleborough, close to the village of Austwick in the Yorkshire Dales. The Ordnance Survey grid reference of the boulder field is . The erratics are classic geomorphological features from the glaciation of northern England. In his chapter on the Pennines, A.E. Trueman wrote: "Particularly well known are the great perched blocks of dark grit which stand on the limestone platform at Norber near Settle." Many of the Silurian greywacke boulders at the site are perched on pedestals of limestone up to 30cm high. The boulders were probably deposited by melting ice sheets at the end of the last ice age, around 12,000 years ago. The pedestals have developed because the erratic boulders have protected the underlying limestone from solution by rainfall, giving estimates of the rate of lowering of the surrounding limestone pavement A limestone pavement is ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Simon Fell (Yorkshire Dales)
Simon Fell is a subsidiary summit on the north east ridge of Ingleborough, a mountain in the Yorkshire Dales in Northern England England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe b .... With a height of and a prominence of , it is classified as a Hewitt. Peaks of the Yorkshire Dales Hewitts of England {{Craven-geo-stub ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]