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High Hartsop Dodd
High Hartsop Dodd is a fell in the English Lake District, an outlier of the Fairfield group in the Eastern Fells. It stands above Kirkstone Pass on the road from Ullswater to Ambleside. Topography High Hartsop Dodd is properly the north eastern ridge of Little Hart Crag, 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 ''"the appearance of an isolated mountain with a peaked summit and steep sides, a very shapely pyramid rising from the green fields."'' Alfred Wainwright: '' A Pictorial Guide to the Lakeland Fells'', Book 1: There are three Dodds when viewed from Hartsop, the others being (Low) Hartsop Dodd and Middle Dodd. The names refer to their position in the valley rather than their height. All three present an imposing pyramidal profile when seen from below, totally obscuring their parent fells. Similarly, all three appear entire ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Hart Crag
Little Hart Crag is a fell in the Lake District area of England. It stands at the head of Scandale, six kilometres north of Ambleside, at a height of 637 metres (2090 feet). It is an eastern outlier of Dove Crag in the Eastern Fells, although it does have 34 metres of prominence from that fell making it both a Hewitt and a Nuttall fell. It is frequently climbed as part of the Dovedale horseshoe, an 11 kilometre walk over the neighbouring fells of Hartsop above How, Hart Crag, Dove Crag and High Hartsop Dodd, starting and finishing at Brothers Water. Topography Little Hart Crag is composed of grassy slopes on its eastern slopes above the Scandale Pass, with the tiny Scandale Tarn tucked in a hollow in the hill. To the east it drops steeply into Caiston Glen. On its west side it is connected to Dove Crag by the boggy hollow of Bakestone Moss and to the north east a ridge falls away towards Patterdale going over High Hartsop Dodd before dropping steeply to the valley. The fe ... [...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] |
Hartsop Dodd
Hartsop Dodd is a fell in the English Lake District, standing to the south east of Brothers Water. It is a subsidiary top on the north ridge of Caudale Moor, but was given separate fell status by Wainwright in his ''Pictorial Guide to the Lakeland Fells''.Alfred Wainwright:''A Pictorial Guide to the Lakeland Fells'', Book 2: That convention is followed here. Topography A broad grassy ridge descends gently from Caudale Moor, running north from the summit plateau and topped by a stone wall. After about half a mile it narrows considerably and turns north-west for the same distance again. Finally it throws up a small grassy dome which is the summit of Hartsop Dodd. After this the ridge drops quickly to valley level between Hartsop village and Brothers Water. The western flank of the ridge stands above the high valley of Caudale, which is a feeder of Kirkstone Beck and Brothers Water. On the eastern side is Pasture Bottom, the valley of Pasture Beck. This stream joins the outflow ... [...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] |
Lead
Lead is a chemical element with the symbol Pb (from the Latin ) and atomic number 82. It is a heavy metal that is denser than most common materials. Lead is soft and malleable, and also has a relatively low melting point. When freshly cut, lead is a shiny gray with a hint of blue. It tarnishes to a dull gray color when exposed to air. Lead has the highest atomic number of any stable element and three of its isotopes are endpoints of major nuclear decay chains of heavier elements. Lead is toxic, even in small amounts, especially to children. Lead is a relatively unreactive post-transition metal. Its weak metallic character is illustrated by its amphoteric nature; lead and lead oxides react with acids and bases, and it tends to form covalent bonds. Compounds of lead are usually found in the +2 oxidation state rather than the +4 state common with lighter members of the carbon group. Exceptions are mostly limited to organolead compounds. Like the lighter members of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Geological Survey
The British Geological Survey (BGS) is a partly publicly funded body which aims to advance geoscientific knowledge of the United Kingdom landmass and its continental shelf by means of systematic surveying, monitoring and research. The BGS headquarters are in Keyworth, Nottinghamshire, England. Its other centres are located in Edinburgh, Wallingford, Cardiff and London. The current motto of the BGS is: ''Gateway to the Earth''. History and previous names The Geological Survey was founded in 1835 by the Board of Ordnance as the Ordnance Geological Survey, under Henry De la Beche. This was the world's first national geological survey. It remained a branch of the Ordnance Survey for many years. In 1965, it was merged with the Geological Museum and Overseas Geological Surveys, under the name of Institute of Geological Sciences. On 1 January 1984, the institute was renamed the British Geological Survey (and often referred to as the BGS), a name still carried today. Competenc ... [...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] |
Volcaniclastic
Volcaniclastics are geologic materials composed of broken fragments (clasts) of volcanic rock. These encompass all clastic volcanic materials, regardless of what process fragmented the rock, how it was subsequently transported, what environment it was deposited in, or whether nonvolcanic material is mingled with the volcanic clasts. The United States Geological Survey defines volcaniclastics somewhat more narrowly, to include only rock composed of volcanic rock fragments that have been transported some distance from their place of origin. In the broad sense of the term, volcaniclastics includes pyroclastic rocks such as the Bandelier Tuff; cinder cones and other tephra deposits; the basal and capping breccia that characterize ʻaʻā lava flows; and lahars and debris flows of volcanic origin.Vincent 2000, pp.27-28 Volcaniclastics make up more of the volume of many volcanoes than do lava flows. Volcaniclastics may have contributed as much as a third of all sedimentation in the geolo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dacite
Dacite () is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides. It has a fine-grained (aphanitic) to porphyritic texture and is intermediate in composition between andesite and rhyolite. It is composed predominantly of plagioclase feldspar and quartz. Dacite is relatively common, occurring in many tectonic settings. It is associated with andesite and rhyolite as part of the subalkaline volcanic rock, subalkaline tholeiite, tholeiitic and calc-alkaline magma series. Composition Dacite consists mostly of plagioclase feldspar and quartz with biotite, hornblende, and pyroxene (augite or enstatite). The quartz appears as rounded, corroded phenocrysts, or as an element of the ground-mass. The plagioclase in dacite ranges from oligoclase to andesine and labradorite. Sanidine occurs, although in small proportions, in some dacites, and when abundant gives rise to rocks that form rhyodacite, transitions to the rhyolites. The rel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brothers Water
Brothers Water is a small lake in the Hartsop valley, in the eastern region of the Lake District in England. Once called Broad Water, it lies at the northern end of Kirkstone Pass, affording views on the descent towards Patterdale. The name was changed in the 19th century after two brothers drowned there. Dorothy Wordsworth, having left William Wordsworth sitting on Cow Bridge, walked beside the lake on 16 April 1802, commented on: The lake is not among the most popular in the national park, being shallow and full of reeds. Water lilies bloom in July, providing colour. To the north-east of Brothers Water is the village of Hartsop, which has several 17th-century stone farm buildings and cottages. Some of the buildings still contain spinning-rooms where villagers would have made their own clothing, selling any surplus in the local market towns. The word Hartsop means "valley of the deer", which would have lived in the woodlands of the lower areas of the surrounding fells. A wal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Red Screes
Red Screes is a fell in the English Lake District, situated between the villages of Patterdale and Ambleside. It may be considered an outlier of the Fairfield group in the Eastern Fells, but is separated from its neighbours by low cols. This gives Red Screes an independence which is reflected in its prominence. Topography Red Screes is a ridge of high ground which runs for nearly 7 km in a north north-easterly direction from the town of Ambleside, and reaches a maximum height of 776 m. This ridge narrows at either end, giving it the shape of a long upturned boat. It is separated from neighbouring fells by Scandale Pass to the west (c.516 m) and Kirkstone Pass to the east (455 m). These two low cols mean that Red Screes is seen as an independent fell when viewed from the south of the Lake District. They also give the fell sufficient prominence to be classified as a Marilyn. There are two minor subsidiary tops: Snarker Pike (644 m) on the south ridge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scandale Pass
Hill passes of the Lake District were originally used by people in one valley travelling to another nearby without having to go many miles around a steep ridge of intervening hills. Historically, in the Lake District of northwest England, travel on foot or by pony was difficult because of the region's steep-sided valleys so tracks across the ridges were created taking the easiest route over passes – often, but not always, via a col. Since Roman times long-distance travel had tended to be along ridges. From the 19th century these passes and ridge routes were brought back into use when recreational hill walking become popular. Forty hill passes within the Lake District National Park are listed here, using criteria for selecting the major routes. Background The Lake District National Park was created in 1951 covering an area of over and, although its population is only 42,000, over 10 million visitors arrive each year, mostly attracted by the lakes and fells. Geology Abou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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