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Stone Arthur
Stone Arthur is a fell in the English Lake District, an outlier of the Fairfield group in the Eastern Fells. It stands above Grasmere village. Topography Stone Arthur is properly the south western ridge of Great Rigg, but was given the status of a separate fell by Alfred Wainwright in his '' Pictorial Guide to the Lakeland Fells'' and that convention is followed here. His decision was based on it having a summit tor with''"a short wall of rock like a ruined castle."''. Alfred Wainwright: '' A Pictorial Guide to the Lakeland Fells'', Book 1: This outcrop appears particularly impressive from Grasmere village, from where the higher fells are hidden. From the top of Great Rigg the main ridge ploughs on due south, descending over the tops of Heron Pike and Nab Scar and carrying the ever popular Fairfield horseshoe walk. A second shorter ridge descends steadily to the south west over gradually roughening ground, until after three quarters of a mile a rock outcrop is thrust up. Th ... [...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] |
Tor (rock Formation)
A tor, which is also known by geomorphologists as either a castle koppie or kopje, is a large, free-standing rock outcrop that rises abruptly from the surrounding smooth and gentle slopes of a rounded hill summit or ridge crest. In the South West of England, the term is commonly also used for the hills themselves – particularly the high points of Dartmoor in Devon and Bodmin Moor in Cornwall.Ehlen, J. (2004) ''Tor'' in Goudie, A., ed., pp. 1054-1056. ''Encyclopedia of Geomorphology.'' Routledge. London, England. Etymology Although English topographical names often have a Celtic etymology, the Oxford English Dictionary lists no cognates to the Old English word in either the Breton or Cornish languages (the Scottish Gaelic ''tòrr'' is thought to derive from the Old English word). It is therefore accepted that the English word ''Tor'' derives from the Old Welsh word ''tẁrr'' or ''twr'', meaning a cluster or heap. Formation Tors are landforms created by the erosion and weath ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Breccia
Breccia () is a rock composed of large angular broken fragments of minerals or rocks cemented together by a fine-grained matrix. The word has its origins in the Italian language, in which it means "rubble". A breccia may have a variety of different origins, as indicated by the named types including sedimentary breccia, tectonic breccia, igneous breccia, impact breccia, and hydrothermal breccia. A megabreccia is a breccia composed of very large rock fragments, sometimes kilometers across, which can be formed by landslides, impact events, or caldera collapse. Types Breccia is composed of coarse rock fragments held together by cement or a fine-grained matrix. Like conglomerate, breccia contains at least 30 percent of gravel-sized particles (particles over 2mm in size), but it is distinguished from conglomerate because the rock fragments have sharp edges that have not been worn down. These indicate that the gravel was deposited very close to its source area, since otherwise th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grasmere (lake)
Grasmere is one of the smaller lakes of the English Lake District, in the county of Cumbria. It gives its name to the village of Grasmere, famously associated with the poet William Wordsworth, which lies immediately to the north of the lake.Parker, 2004, pages 34-36 The lake is 1680 yd (1540 m) long and 700 yd (640 m) wide, covering an area of 0.24 mi² (0.62 km²). It has a maximum depth of 70 ft (21m) and an elevation above sea level of 208 ft (62 m). The lake is both fed and drained by the River Rothay, which flows through the village before entering the lake, and then exits downstream into nearby Rydal Water, beyond which it continues into Windermere.Parker, 2004, page 90 The waters of the lake are leased by the Lowther Estate to the National Trust. The waters are navigable, with private boats allowed and rowing boats for hire, but powered boats are prohibited. The lake contains a single island, known as ''Grasmere Island'' or simply ''The Island''. In ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Rothay
The Rothay is a spate river of the Lake District in north-west England. Its name comes from Old Norse and translates literally as ''the red one''. This has come to mean ''trout river''. It rises close to Rough Crag above Dunmail Raise at a point about 1542 feet (470 m) above sea level (). Its catchment area covers Grasmere Common including Easedale Tarn, the southern flanks of Fairfield, and several of the fells to the east of Dunmail Raise, including Great Rigg, Rydal Fell, Scandale Fell and Heron Pike. From its source the Rothay descends through the valley of Greenburn Bottom to the hamlet of Helmside not far from the main A591 road over Dunmail Raise. Just north of the village of Grasmere the river subsumes Easedale Gill and Sour Milk Gill, the latter flowing out of Easedale Tarn. In the village the river flows close to the churchyard where the poet Wordsworth is buried. The Rothay then flows into the head of the lake of Grasmere (elevation 208 feet/63 m). As we ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seat Sandal
Seat Sandal is a fell in the English Lake District, situated four kilometres (2½ miles) north of the village of Grasmere from where it is very well seen. Nevertheless, it tends to be overshadowed by its more illustrious neighbours in the Eastern Fells, Helvellyn and Fairfield. Name The unusual name comes from the Old Norse language, '' " Sandulfr " '' being an Old Norse personal name. The name element '' ' Seat ' '' is from Old Norse '' ' sæter ' ''. Toponym * Sandulfr's sæter * Sandal's high summer pasture. Examples of place names with a similar etymology might include : * Seatoller , Borrowdale, Lake District : (Seat..oller ) '' " Óláfr’s sæter " '' * Seatallan , Wasdale, Lake District : (Seat..allan ) '' " Aleyn's sæter " '' The remains of structures have been found on Seat Sandal that are assumed to have been summer shielings (high altitude dwellings ) where people stayed during the summer months in order to watch over the animals. Both Seat Sanda ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fairfield Horseshoe
Fairfield Horseshoe is a classic circular hillwalking ridge walk route starting from Rydal or Ambleside in the English Lake District that takes in all the fells that surround the valley of the Rydal Beck. The round The walk is extremely popular and follows well defined paths throughout with no real difficulties; however, care should be taken on the summit of Fairfield in poor visibility as the plateau of that mountain is very flat and can be quite confusing, with the danger of steep drops to the north and west. The eastern side of the horseshoe from Low Sweden Bridge near Ambleside to the slopes of Hart Crag follows a high dry stone wall, covering some six kilometres, making navigation simple even in poor weather conditions. One of Wainwright’s favourite ridge walks, the round was described by him as “a great horseshoe of grassy slopes below a consistently high skyline, simple in design and impressive in altitude”. Contrary to his normal practice, Wainwright recommended ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nab Scar
Nab Scar is a fell in the English Lake District, an outlier of the Fairfield group in the Eastern Fells. It stands above Rydal Water. Topography Nab Scar is properly the steep terminal face of the southern ridge of Heron Pike, but the name is also given to the whole of the ridge south of Lord Crag. Alfred Wainwright gave it the status of a separate fell in his ''Pictorial Guide to the Lakeland Fells'' and that convention is followed here. The popular Fairfield horseshoe ridge walk either begins or ends with Nab Scar, consensus never having been achieved on the "correct" direction of travel. This route also takes in the additional Wainwrights of Heron Pike, Great Rigg, Fairfield, Hart Crag, Dove Crag, High Pike and Low Pike in a circuit of Rydale. From the double summit of Heron Pike, a grassy ridge descends south westerly, gradually narrowing until a rougher section falls more steeply at Lord Crag. Beyond here it levels out, curving back a little to the east and pass ... [...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] |
A 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] |
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] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
