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High Rigg
High Rigg is a small fell located in the English Lake District, approximately three miles southeast of the town of Keswick. It occupies an unusual position, surrounded on all sides by higher fells but not connected by any obvious ridge. This separation from its fellows ensures that it is a Marilyn (a hill with topographic prominence of at least 150m). Topography High Rigg is strictly the continuation of the ridge running up the western shore of Thirlmere, whose high point is Raven Crag. This forms the watershed between the Shoulthwaite and Thirlmere/ Vale of St John systems. The depression between High Rigg and Raven Crag to the south — at only around — is at Smaithwaite, just south of the A591 Keswick to Ambleside road. High Rigg resembles a model of the Lakeland Fells in miniature, complete with crags, intermediate tops, tarns and even a 'pass' crossing the ridge halfway along, complete with church. The northern and southern aspects of the fell are largely grassed and ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Low Rigg
Low Rigg is a small hill located in the English Lake District a few miles east of the town of Keswick and slightly to the north of its larger neighbour High Rigg. It is a hill of modest elevation, being of insufficient size to merit inclusion in the famous Lake District guides produced by Alfred Wainwright. However, its position affords excellent views of the surrounding mountains such as Blencathra and Clough Head. Geologically, Low Rigg is a lens-shaped laccolith consisting of an intrusion of a fine-grained granite. The hill may be climbed in a short walk from either the Naddle Valley or St John's in the Vale St John’s in the Vale is a glacial valley in the Lake District National Park, Cumbria, England. Within the vale are a number of farms and small settlements, in addition to several disused quarry and mining works. St John’s Beck meanders nort .... Low Rigg also possesses a feature not present on its larger neighbour, a body of water of reasonable size known as Tew ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tarn (lake)
A tarn (or corrie loch) is a Proglacial lake, proglacial mountain lake, pond or pool, formed in a cirque excavated by a glacier. A moraine may form a natural dam below a tarn. Etymology The word is toponymy, derived from the Old Norse word ''tjörn'' ("a small mountain lake without tributaries") meaning pond. In parts of Northern England - predominantly Cumbria but also areas of North Lancashire and North Yorkshire - 'tarn' is widely used as the name for small lakes or ponds, regardless of their location and origin (e.g. Talkin Tarn, Urswick Tarn, Malham Tarn). Similarly, in Scandinavian languages, a ''tjern'' or ''tjørn'' (both Norwegian) or ''tjärn'' or ''tärn'' (both Swedish) is a small natural lake, often in a forest or with vegetation closely surrounding it or growing into the tarn. The specific technical use for a body of water in a glacial corrie comes from high number of tarns found in corries in the Lake District, an upland area in Cumbria. Nonetheless, there are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pictorial Guide To The Lakeland Fells
''A Pictorial Guide to the Lakeland Fells'' is a series of seven books by A. Wainwright, detailing the fells (the local word for hills and mountains) of the Lake District in northwest England. Written over a period of 13 years from 1952, they consist entirely of reproductions of Wainwright's manuscript, hand-produced in pen and ink with no typeset material. The series has been in print almost continuously since it was first published between 1955 and 1966, with more than 2 million copies sold. It is still regarded by many walkers as the definitive guide to the Lakeland mountains. The 214 fells described in the seven volumes have become known as the Wainwrights. the LDWA register of those who have climbed all the fells listed 674 names. The Wainwright Society maintains a "register of current Society members who have climbed all 214 fells". First editions The first five books were originally published by Wainwright's friend, Henry Marshall, Chief Librarian of Kendal and West ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scafell
Scafell ( or ; also spelled Sca Fell, previously Scawfell) is a mountain in the English Lake District, part of the Southern Fells. Its height of makes it the second-highest mountain in England after its neighbour Scafell Pike, from which it is separated by Mickledore col. Topography Scafell stands between Wasdale in the west and upper Eskdale to the east. The highest part of the fell is a ridge running south from Mickledore as far as Slight Side, which is counted as a separate fell by most guidebooks.Richards, Mark: ''Mid-Western Fells'': Collins (2004): Despite regarding Slight Side as a separate entity, Wainwright included the wide upland area beyond it to the south west as a part of Scafell. More modern guides have partitioned the plateau off as a further independent top, Great How. The opposing flanks of Scafell are entirely different in character. To the south, monotonous smooth slopes, stony and lacking vegetation at higher levels, run down toward Burnmoor and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bleaberry Fell
Bleaberry Fell is a fell in the Lake District in Cumbria, England, with a height of 590 metres (1,936 feet). It stands on the main watershed between Borrowdale and Thirlmere and can be climbed from either flank. Walla Crag is a subsidiary top of Bleaberry Fell. Topography Situated in the central area of the national park, four kilometres ( miles) south of Keswick, Bleaberry Fell is the northernmost top on the ridge that separates the valleys containing the lakes of Derwent Water (Borrowdale) and Thirlmere. This ridge, which also contains the fells of High Seat and High Tove, is notoriously boggy underfoot, but Bleaberry Fell is mostly dry and the heather-covered summit gives an excellent all-round vista. To the east the fell has the rock faces of Iron Crag and Goat Crags as it falls away towards the Thirlmere valley. Ascents The fell is usually climbed from the car park in Great Wood in Borrowdale, firstly ascending Walla Crag via Cat Gill and then continuing south-e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Helvellyn Range
The Helvellyn range is the name given to a part of the Eastern Fells in the English Lake District, "fell" being the local word for "hill". The name comes from Helvellyn, the highest summit of the group. The Helvellyn range forms a ridge extending for about 10 km, at no point dropping below 600 m. The ridge runs in a north–south direction, with Patterdale on the eastern side and the Thirlmere valley to the west. The village of Threlkeld lies directly to the north, below the northernmost point on the ridge, Clough Head. Generally, the slopes above Thirlmere are steep and grassy, whilst the Patterdale side exhibits rockier features, due to cirque glaciation on the north east side of the ridge. List of peaks The majority of the peaks in the range lie directly on the north–south axis, although there are some outliers on the eastern side of the ridge. *Clough Head (726 m) *Great Dodd (856 m) * Watson's Dodd (789 m) * Stybarrow Dodd (843 m) **Green ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clough Head
Clough Head () (meaning: ''hill-top above the ravine'') is a fell, or hill, in the English Lake District. It marks the northern end of the main ridge of the Helvellyn range and is often walked as part of the ridge walk. The fell stands south of the village of Threlkeld and the A66 road, and it forms the steep eastern side of the tranquil valley of St John's in the Vale. On its western side the fell displays a dark mass of rocky crags and a deep-set rocky ravine. On the other side it has smooth grassy slopes. Beneath the north face is the steep valley or clough from which Clough Head gets its name. Also beneath the steep northern face lies the lower hill of Threlkeld Knotts, a granite hill which has been much quarried round its margin. A number of different types of rock are found on and around Clough Head, which were formed in very different circumstances. These include deep-sea sedimentation, effusive volcanic lava flows, explosive volcanism, an intrusion of granite, mineralis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blencathra
Blencathra, also known as Saddleback, is one of the most northerly hills in the English Lake District. It has six separate fell tops, of which the highest is the Hallsfell Top at 2,848 feet (868 metres). Name For many years, Ordnance Survey listed Blencathra under the alternative name of Saddleback, which was coined in reference to the shape of the mountain when seen from the east. The guidebook author Alfred Wainwright popularised the use of the older Cumbric name, which is now used almost exclusively. Ordnance Survey currently marks the summit as ‘Saddleback or Blencathra’. It is likely that the name Blencathra is derived from the Cumbric elements *''blain'' ‘top, summit’ and ''cadeir'' ‘seat, chair’, meaning ‘the summit of the seat-like mountain’. Andrew Breeze has proposed an alternative interpretation of the second element of the name, arguing that it represents a Cumbric cognate of Middle Welsh ''carthwr'' ‘working horse’. Richard Coates has sug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skiddaw
Skiddaw is a mountain in the Lake District National Park in England. Its summit is the sixth-highest in England. It lies just north of the town of Keswick, Cumbria, and dominates the skyline in this part of the northern lakes. It is the simplest of the Lake District mountains of this height to ascend (as there is a well-trodden tourist track from a car park to the north-east of Keswick, near the summit of Latrigg) and, as such, many walking guides recommend it to the occasional walker wishing to climb a mountain. This is the first summit of the fell running challenge known as the Bob Graham Round when undertaken in a clockwise direction. The mountain lends its name to the surrounding areas of Skiddaw Forest and Back o' Skidda, and to the isolated Skiddaw House, situated to the east, formerly a shooting lodge and subsequently a youth hostel. It also provides the name for the slate derived from that region: Skiddaw slate. Skiddaw slate has been used to make tuned percussi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Panorama
A panorama (formed from Greek πᾶν "all" + ὅραμα "view") is any wide-angle view or representation of a physical space, whether in painting, drawing, photography, film, seismic images, or 3D modeling. The word was originally coined in the 18th century by the English (Irish descent) painter Robert Barker to describe his panoramic paintings of Edinburgh and London. The motion-picture term ''panning'' is derived from ''panorama''. A panoramic view is also purposed for multimedia, cross-scale applications to an outline overview (from a distance) along and across repositories. This so-called "cognitive panorama" is a panoramic view over, and a combination of, cognitive spaces used to capture the larger scale. History The device of the panorama existed in painting, particularly in murals, as early as 20 A.D., in those found in Pompeii, as a means of generating an immersive "panoptic" experience of a vista. Cartographic experiments during the Enlightenment era prec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cairn
A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehistoric times, they were raised as markers, as memorials and as burial monuments (some of which contained chambers). In modern times, cairns are often raised as landmarks, especially to mark the summits of mountains. Cairns are also used as trail markers. They vary in size from small stone markers to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. A variant is the inuksuk (plural inuksuit), used by the Inuit and other peoples of the Arctic region of North America. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andesite
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of the fe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
