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Low Pike
Low Pike is a small fell in the English Lake District. It has a modest height of 508 m (1,667 ft) and is situated three kilometres north of Ambleside. Low Pike is well seen from the streets of the town as the first prominent fell on the ridge which continues northwards for a further four kilometres to Fairfield. This ridge is part of the Fairfield horseshoe walk and Low Pike is most commonly ascended as part of this. Topography Despite its modest height, Alfred Wainwright gave Low Pike a separate chapter in his ''Pictorial Guide to the Lakeland Fells'' because "it is sufficiently elevated above the deep valleys of Scandale and Rydale to give an impression of loftiness which exaggerates its modest altitude." Bill Birkett also mentions the fell in his “Complete Lakeland Fells”, but its altitude is not sufficient to be noted on any other mountain lists. Geology The crest of the ridge consists of the dacitic welded lapilli-tuff of the Lincomb Tarns Formation. And ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Pike (Scandale)
High Pike is a fell in the English Lake District, located five kilometres north of Ambleside. Situated in the Eastern Fells, it can be confused with another Lake District High Pike in the Northern Fells. High Pike reaches a height of . It is sometimes referred to as Scandale Fell, although this name really only applies to the high ground at the head of Scandale. Topography When viewed from the south around High Sweden bridge near Ambleside, High Pike has the look of a remote peak standing alone with cliffs falling away from the summit on its eastern side. However, in reality it is just a slight rise on the long southern ridge of Dove Crag with only about five metres of prominence which prevents it even qualifying as a “Nuttall”; nevertheless both Alfred Wainwright and Bill Birkett mention the fell in their books on the Lakeland Fells. Geology The crest of the ridge consists of the volcaniclastic laminated claystone and siltstone of the Esk Pike Formation. Beneath is the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dove Crag
Dove Crag is a fell in the English Lake District. Situated in the Eastern Fells of the national park, seven kilometres south-south-west of Glenridding, it reaches a height of 792 metres (2,598 feet). The fell is often climbed as part of the Fairfield horseshoe walk but a direct ascent from Patterdale is required to show the fell's full potential, displaying the impressive crags just to the north east of the summit. The highest point was originally unnamed on maps, being just a minor top, but over the years the summit has adopted the name of Dove Crag by mutual accord.. Wainwright's Pictorial Guides One of Dove Crag's claims to fame is that it was the first chapter ever written by Alfred Wainwright for his Pictorial Guide to the Lakeland Fells. He wrote the Dove Crag chapter on 9 November 1952 as he started Book One, after ascending the fell from Ambleside in the previous weeks, making notes and taking photographs. It would take Wainwright a further 14 years to finish the complet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lapilli
Lapilli is a size classification of tephra, which is material that falls out of the air during a volcanic eruption or during some meteorite impacts. ''Lapilli'' (singular: ''lapillus'') is Latin for "little stones". By definition lapilli range from in diameter. A pyroclastic particle greater than 64 mm in diameter is known as a volcanic bomb when molten, or a volcanic block when solid. Pyroclastic material with particles less than 2 mm in diameter is referred to as volcanic ash. Formation Lapilli are spheroid-, teardrop-, dumbbell- or button-shaped droplets of molten or semi-molten lava ejected from a volcanic eruption that fall to earth while still at least partially molten. These granules are not accretionary, but instead the direct result of liquid rock cooling as it travels through the air. Lapilli tuffs are a very common form of volcanic rock typical of rhyolite, andesite and dacite pyroclastic eruptions, where thick layers of lapilli can be deposited during a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Furness Fells
The Furness Fells are a multitude of hills and mountains in the Furness region of Cumbria, England. Historically part of Lancashire, the Furness Fells or High Furness is the name given to the upland part of Furness, that is, that part of Furness lying north of the line between Ulverston and Ireleth. The hills lie largely within the English Lake District. The term ''Furness Fells'' is also sometimes used as a synonym with ''Coniston Fells'', perhaps partly as a result of the placing of the words "Furness Fells" on some Ordnance Survey 1:250 000 maps. The Coniston Fells properly form only part of the Furness Fells, albeit with all the highest mountains; other fells in Furness are of lower altitude. The Coniston Fells form part of the Southern Fells of the Lake District as defined by Alfred Wainwright. Coniston Fells The Coniston Fells are separated from the Scafell and Bowfell massif to their north by Wrynose Pass, and are surrounded on all other sides by lower ground. Coniston ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Langdale
Great Langdale is a valley in the Lake District National Park in North West England, the epithet Great distinguishing it from the neighbouring valley of Little Langdale. Langdale is also the name of a valley in the Howgill Fells, elsewhere in Cumbria. It is a popular location for hikers, climbers, fell-runners, and other outdoor enthusiasts who are attracted by the many fells ringing the head of the valley. Among the best-known features of Great Langdale are the Langdale Pikes, a group of peaks on the northern side of the dale. England's highest mountain, Scafell Pike, can be climbed by a route from Langdale. Langdale has views of, in particular, Dungeon Ghyll Force waterfall, Harrison Stickle, and Pike of Stickle. Great Langdale was an important site during the Neolithic period for producing stone axes and was also one of the centres of the Lakeland slate industry. History Great Langdale is known to archaeologists as the source of a particular type of Neolithic polished ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heron Pike
Heron Pike is a fell in the English Lake District, two kilometres east of Grasmere. It is part of the Fairfield group in the Eastern Fells. It should not be confused with the Heron Pike that forms part of Sheffield Pike, although it appears that, by coincidence, both Heron Pikes are exactly the same height. Topography Not a fell of great significance, Heron Pike is a slight grassy rise on the long southern ridge of its parent fell Fairfield. Just cresting the 2,000 foot mark at 612 m (2,008 ft), it is mostly climbed as part of the Fairfield horseshoe walk and it lies between the adjoining fells of Nab Scar and Great Rigg. Heron Pike’s eastern side features Erne Crag and Blind Cove as it falls away quite steeply towards Rydal Beck. At the base of Erne Crag is an old quarry, the mouth of a cavern quite easy to locate.Richards, Mark: ''Near Eastern Fells'': Collins (2003): The fell's western flank drops towards Grasmere and has the small Alcock Tarn on its low ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Rigg
Great Rigg is a fell in the English Lake District, 7 kilometres (4½ miles) north-west of Ambleside and reaching a height of 766 metres (2,513 feet). It is most often climbed as part of the Fairfield horseshoe, a 16-km circular walk which starts and finishes in Ambleside. The fell's name originates from the Old English "Rigg", meaning a bumpy or knobbly ridge. Topography Great Rigg is mostly without merit, being just an undulation on one of Fairfield's southern ridges; with 31 metres of prominence it just qualifies as a Hewitt. It is best seen from the south-west near Grasmere where from that angle its summit seems to dominate the valley. The fell is rocky on its eastern side as Stone Cove drops to Rydal Beck; on its western flank it is mostly grassy as it falls away to Tongue Gill; to the north and south are ridges which continue to other fells, with Fairfield being 1.5 kilometres (0.9 miles) away to the north while Heron Pike lies 2.5 kilometres (1.6 miles) to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hart Crag
Hart Crag is a fell in the English Lake District, being one of the Fairfield group of hills in the Eastern Fells. Topography The fell stands on the ridge running south east from Fairfield to Dove Crag, at the point where a long subsidiary spur sweeps off to the north east. This is Hartsop above How and, although in reality part of Hart Crag, was treated as a separate fell by Alfred Wainwright in his ''Pictorial Guide to the Lakeland Fells''. That convention is also followed here. Being at the meeting point of three ridges, Hart Crag also has a share in three valleys. Despite forming a part of the headwall in each case, the fell is not the true head of any of them. West of the summit runs the long and unfrequented valley of Rydal Beck. This flows almost due south for 3 miles, finally emptying into the River Rothay at Rydal village. The slopes of Rydal Head below Hart Crag are steep, but reasonably free of outcropping rock. To the north of Hart Crag is Link Cove. This is a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old Norse Language
Old Norse, Old Nordic, or Old Scandinavian, is a stage of development of North Germanic languages, North Germanic dialects before their final divergence into separate Nordic languages. Old Norse was spoken by inhabitants of Scandinavia and their Viking expansion, overseas settlements and chronologically coincides with the Viking Age, the Christianization of Scandinavia and the consolidation of Scandinavian kingdoms from about the 7th to the 15th centuries. The Proto-Norse language developed into Old Norse by the 8th century, and Old Norse began to develop into the modern North Germanic languages in the mid-to-late 14th century, ending the language phase known as Old Norse. These dates, however, are not absolute, since written Old Norse is found well into the 15th century. Old Norse was divided into three dialects: Old West Norse, ''Old West Norse'' or ''Old West Nordic'' (often referred to as ''Old Norse''), Old East Norse, ''Old East Norse'' or ''Old East Nordic'', and ''Ol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scandinavia
Scandinavia; Sámi languages: /. ( ) is a subregion#Europe, subregion in Northern Europe, with strong historical, cultural, and linguistic ties between its constituent peoples. In English usage, ''Scandinavia'' most commonly refers to Denmark, Norway, and Sweden. It can sometimes also refer more narrowly to the Scandinavian Peninsula (which excludes Denmark but includes part of Finland), or more broadly to include all of Finland, Iceland, and the Faroe Islands. The geography of the region is varied, from the Norwegian fjords in the west and Scandinavian mountains covering parts of Norway and Sweden, to the low and flat areas of Denmark in the south, as well as archipelagos and lakes in the east. Most of the population in the region live in the more temperate southern regions, with the northern parts having long, cold, winters. The region became notable during the Viking Age, when Scandinavian peoples participated in large scale raiding, conquest, colonization and trading mostl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Packhorse Bridge
A packhorse bridge is a bridge intended to carry packhorses (horses loaded with sidebags or panniers) across a river or stream. Typically a packhorse bridge consists of one or more narrow (one horse wide) masonry arches, and has low Parapet#Bridge parapets, parapets so as not to interfere with the panniers borne by the horses. Multi-arched examples sometimes have triangular Starling (structure), cutwaters that are extended upward to form pedestrian refuges. Packhorse bridges were often built on the trade routes (often called packhorse routes) that formed major transport arteries across Europe and Great Britain until the coming of the toll road, turnpike roads and canals in the 18th century. Before the road-building efforts of Napoleon, all Principal passes of the Alps, crossings of the Alps were on packhorse trails. Travellers' carriages were dismantled and transported over the mountain passes by ponies and mule, mule trains. Definition In the British Isles at least, the definitio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dry-stone Wall
Dry stone, sometimes called drystack or, in Scotland, drystane, is a building method by which structures are constructed from stones without any mortar to bind them together. Dry stone structures are stable because of their construction method, which is characterized by the presence of a load-bearing façade of carefully selected interlocking stones. Dry stone construction is best known in the context of stone walls, traditionally used for the boundaries of fields and churchyards, or as retaining walls for terracing, but dry stone sculptures, buildings, bridges, and other structures also exist. The term tends not to be used for the many historic styles which used precisely-shaped stone, but did not use mortar, for example the Greek temple and Inca architecture. The art of dry stone walling was inscribed in 2018 on the UNESCO representative list of the intangible cultural heritage of humanity, for dry stone walls in countries such as France, Greece, Italy, Slovenia, Cro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
