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Blea Rigg
Blea Rigg is a fell in the English Lake District, lying between the valleys of Easedale and Great Langdale. One of the Central Fells, it is a broad plateau with a succession of rocky tops. Many routes of ascent are possible, beginning either from Grasmere or Great Langdale, though the paths are often poorly marked and hard to follow. Topography The main spine of the Central Fells runs north to south from the Vale of Keswick to its greatest elevation at High Raise. A long ridge runs out eastward from here, so that the range as a whole resembles the letter 'L'. This eastward ridge begins as Blea Rigg and then continues over Silver How and Loughrigg Fell, before petering out near the head of Windermere. Blea Rigg is a broad plateau, around a mile wide and two miles long, climbing roughly east to west. It connects via a narrower section between Stickle and Codale Tarns to Sergeant Man and ultimately High Raise in the west. Stickle Tarn is the larger of the two waterbodies, a 50&n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harrison Stickle
Harrison Stickle is a fell in the central part of the English Lake District, situated above Great Langdale. The fell is one of the three (although the number is debated) fells which make up the picturesque Langdale Pikes, the others being Pike of Stickle and Loft Crag. Together they make up one of the most picturesque, and probably the best-known, mountain groups in the District. A "stickle" is a hill with a prominent rocky top. Topography The Langdale Pikes form a raised rocky parapet around the southern and eastern edges of a high tableland centred upon Thunacar Knott. Harrison Stickle is the high point of this system and its crags fall south and east from the summit, presenting an arresting view from the valley floor 2,000 ft below, or from further afield. To the north, the main ridge of the central fells passes over Thunacar Knott before climbing to High Raise. The craggy eastern face of this ridge continues north as far as Harrison's near neighbour, Pavey Ark, visua ... [...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] |
Southern Fells
Image:Annotated Scafell range.jpg, 300px, The Scafells rect 23 372 252 419 Slight Side, Slight Side (762 m) rect 173 794 560 834 Sca Fell, Scafell East Buttress rect 707 787 893 861 Esk Pike, Esk Pike or Crag (885 m) rect 245 303 409 358 Sca Fell, Sca Fell (964 m) rect 408 238 637 280 Mickledore, Mickledore (c. 840 m) rect 544 174 826 213 Scafell Pike, South Summit (<978 m) rect 706 310 928 355 Scafell Pike, Scafell Pike (978 m) rect 870 238 1108 286 Broad Crag, Broad Crag (934 m) rect 1043 308 1198 360 Ill Crag, Ill Crag (935 m) rect 1238 311 1446 351 Great End, Great End (910 m) rect 0 0 1444 1085 #top, Click hyperlink or button to expand desc none The Southern Fells are a group of hills in the England, English Lake District. Including Scafell Pike, the highest peak in England, they occupy a broad area to the south of Great Langdale, Borrowdale and Wasdale. High and rocky towards the centre of the Lake District, the Southern Fells progressively take on a moorland c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Fells
The Eastern Fells are a group of hills in the English Lake District. Centred on Helvellyn they primarily comprise a north–south ridge running between Ullswater and Lakeland's Central Valley. Partition of the Lakeland fells The Lake District is a National Park in the north west of the country and in addition to its lakes it contains a complex range of hills. These are locally known as fells and range from low hills to the highest ground in England. Hundreds of tops exist and many writers have attempted to draw up definitive lists of fells and divided the range into areas to aid their description. The most influential of all such writers was Alfred Wainwright whose ''Pictorial Guide to the Lakeland Fells'' series has sold in excess of 2 million copies, [...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] |
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 (village)
Grasmere is a village and tourist destination in Cumbria, England, in the centre of the Lake District, named after its adjacent lake. It has links with the Lake Poets: William and Dorothy Wordsworth lived in Grasmere for 14 years and called it "the loveliest spot that man hath ever found."A Farewell Retrieved 2 December 2013 Grasmere lies within the historic county of . In 1961, the civil parish had a population of 1,029. That of the and Grasmere ward was 4,475 in the 2011 ... [...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] |
Alfred Wainwright
Alfred Wainwright MBE (17 January 1907 – 20 January 1991), who preferred to be known as A. Wainwright or A.W., was a British fellwalker, guidebook author and illustrator. His seven-volume ''Pictorial Guide to the Lakeland Fells'', published between 1955 and 1966 and consisting entirely of reproductions of his manuscript, has become the standard reference work to 214 of the fells of the English Lake District. Among his 40-odd other books is the first guide to the Coast to Coast Walk, a 182-mile long-distance footpath devised by Wainwright which remains popular today. Life Alfred Wainwright was born in Blackburn, Lancashire, into a family which was relatively poor, mostly because of his stonemason father's alcoholism. He did very well at school (first in nearly every subject) although he left at the age of 13. While most of his classmates were obliged to find employment in the local mills, Wainwright started work as an office boy in Blackburn Borough Engineer's Department. He ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sergeant Man
Sergeant Man is a fell in the English Lake District. It is properly a secondary summit of High Raise, but is given a separate chapter by Alfred Wainwright in his third Pictorial Guide nonetheless, as it "is so prominent an object and offers so compelling a challenge". Its rocky cone is indeed in great contrast to the grassy dome of High Raise. Topography Sergeant Man lies a third of a mile to the south east of the parent fell and is the pivotal point for a complex system of ridges radiating eastward from High Raise. Sergeant Man is not actually visible from the peak of High Raise and Sergeant Man only comes into view as you gently descend from High Raise. South east, passing between Codale and Stickle Tarns is the broad spur leading to Blea Rigg, Silver How and Loughrigg. Sitting above Codale Tarn is the rocky subsidiary top of Codale Head — a grandchild of High Raise. From here further ridges run east to Tarn Crag and north east to Calf Crag and the circuit of Greenburn. S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Windermere
Windermere (sometimes tautology (language), tautologically called Windermere Lake to distinguish it from the nearby town of Windermere, Cumbria (town), Windermere) is the largest natural lake in England. More than 11 miles (18 km) in length, and almost 1 mile (1.5 km) at its widest, it is a ribbon lake formed in a glacial trough after the retreat of ice at the start of the current interglacial period. It has been one of the country's most popular places for holidays and summer homes since the arrival of the Kendal and Windermere Railway's branch line in 1847. Forming part of the border between the historic counties of Lancashire and Westmorland, Windermere is today within the administrative county of Cumbria and the Lake District National Park. Etymology The word 'Windermere' is thought to translate as "'Winand or Vinand's lake'... The specific has usually been identified with an Old Swedish personal name 'Vinandr', genitive singular 'Vinandar'"... although "the pers ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
