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Castle Rock Of Triermain
Watson's Dodd is a fell in the English Lake District, a minor rise on the main ridge of the Helvellyn range in the Eastern Fells, but a prominent shoulder on the west side of that range. At its foot is the imposing crag of Castle Rock, on which rock climbers have developed some 60 named routes. Topography Seen from the west, Watson's Dodd is a noticeable shoulder on the Helvellyn ridge, north of Sticks Pass. The summit stands on the main ridge of the Helvellyn range at the point where the south-west ridge of Great Dodd and the north-west ridge of Stybarrow Dodd meet and merge. From this point a shoulder drops into the valley of the How Beck at Legburthwaite. This shoulder, part of the High Fells of St John's Common, is sharply defined by the deep valleys of Mill Gill to its north and Stanah Gill to its south. It slopes gently to around the 500 m contour, and then drops more steeply into the valley over a number of rocky crags. Just before reaching the valley, part of this ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Dodd
Great Dodd (meaning: ''big round hill'') is a mountain or fell in the English Lake District. It stands on the main ridge of the Helvellyn range, a line of mountains which runs in a north-south direction between the lakes of Thirlmere and Ullswater in the east of the Lake District. Great Dodd, with a height of 857 m is the highest of the fells in this range to the north of Sticks Pass. Walkers may approach Great Dodd from either High Row near Dockray to the east, or from Legburthwaite to the west – or along the main ridge track from either north or south. Scramblers with climbing skills may be attracted to three gill climbs on the western side of the mountain. The summit of Great Dodd is a smooth, grassy, rounded dome, like its two southern neighbours, Watson's Dodd and Stybarrow Dodd. Together, these three are sometimes called ‘The Three Dodds’. These three are made of volcanic rocks of the Borrowdale Volcanic Group, and the tops of all three are covered by the sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Bridal Of Triermain
''The Bridal of Triermain'' is a narrative poem in three cantos by Walter Scott, published anonymously in 1813. It is written in a flexible metre of four and three stress lines. Set in Cumberland, it recounts the exploits of a knight as he seeks to rescue a beautiful maiden, Gyneth, the illegitimate daughter of King Arthur, doomed by Merlin 500 years previously to an enchanted sleep inside a magic castle. Background In 1809 Scott included in an article 'The Inferno of Altisidora' for ''The Edinburgh Annual Review'' three short imitations, of Crabbe, Moore, and himself. The last of these was entitled 'The Vision of Triermain' and consisted of an early version of the first eight stanzas of what was to become ''The Bridal of Triermain''. While he was composing '' Rokeby'' in the autumn of 1812 Scott took some time to extend the fragment to three cantos, planning to publish it anonymously to test the critics, especially Francis Jeffrey, though in the event Jeffrey did not review ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Group (stratigraphy)
In geology, a group is a lithostratigraphic unit consisting of a series of related formations that have been classified together to form a group. Formations are the fundamental unit of stratigraphy. Groups may sometimes be combined into supergroups. Groups are useful for showing relationships between formations, and they are also useful for small-scale mapping or for studying the stratigraphy of large regions. Geologists exploring a new area have sometimes defined groups when they believe the strata within the groups can be divided into formations during subsequent investigations of the area. It is possible for only some of the strata making up a group to be divided into formations. An example of a group is the Glen Canyon Group, which includes (in ascending order) the Wingate Sandstone, the Moenave Formation, the Kayenta Formation, and the Navajo Sandstone. Each of the formations can be distinguished from its neighbor by its lithology, but all were deposited in the same vast ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official period of the Paleozoic Era by the International Union of Geological Sciences, Intern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Borrowdale Volcanic Group
The Borrowdale Volcanic Group is a group of igneous rock formations named after the Borrowdale area of the Lake District, in England. They are Caradocian (late Ordovician) in age (roughly 450 million years old). It is thought that they represent the remains of a volcanic island arc, approximately similar to the island arcs of the west Pacific today. This developed as oceanic crust to the (present) north-west and was forced by crustal movement under a continental land-mass to the present south-east. Such forcing under, as two plates meet, is termed subduction. This land-mass has been named Avalonia by geologists. It is now incorporated into England and Wales and a sliver of North America. Geology At that time the rocks that now comprise most of Scotland (and part of the northern Irish landmass) were not attached to Avalonia. They were separated by an ocean, called the Iapetus Ocean by geologists. The line of joining, or suture, is approximately under the Solway Firth and Cheviot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Western Fells
The North Western Fells are a group of hills in the English Lake District. Including such favourites as Catbells and Grisedale Pike, they occupy an oval area beneath the Buttermere and Borrowdale valley systems. The North Western Fells are characterised by soaring east-west ridges and an absence of mountain tarns. Partition of the Lakeland Fells The Lake District is a National Park in the north west of the country which, in addition to its lakes, contains a complex range of hills. These are known locally 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. In doing so the compilers frequently divide the range into smaller areas to aid their description. The most influential of all such authors 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] |
Western Fells
The Western Fells are a group of hills in the English Lake District. Centred on Great Gable they occupy a triangular area between Buttermere and Wasdale. The Western Fells are characterised by high ridges and an abundance of naked rock. Partition of the Lakeland Fells The Lake District is a National Park in the north west of the country which, in addition to its lakes, contains a complex range of hills. These are known locally 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. In doing so the compilers frequently divide the range into smaller areas to aid their description. The most influential of all such authors was Alfred Wainwright whose ''Pictorial Guide to the Lakeland Fells'' series has sold in excess of 2 million copies, being in print continuously since the first volume was published in 1952. Wainwright divided the fells into seven geographical areas, each surrounded b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Fells
The Central Fells are a group of hills in the English Lake District. Reaching their highest point at High Raise (2,500 ft or 762 metres), they occupy a broad area to the east of Borrowdale. The Central Fells are generally lower than the surrounding hills, the Lake District's dome-like structure having a slight dip in the middle. The range extends from the boggy ridge between Derwentwater and Thirlmere in the north, to the rock peaks of the Langdale Pikes in the south. Partition of the Lakeland fells The Lake District is a National Park in the north-west of the country which, in addition to its lakes, 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. In doing so the compilers frequently divide the range into smaller areas to aid their description. The most influential of all such authors was Alfred Wainwright, who ... [...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] |
Watson's Dodd - Summit
Watsons () is a Hong Kong health care and beauty care chain store in Asia and Europe. It is the flagship health and beauty brand of the A.S. Watson Group, which is majority owned by CK Hutchison Holdings. It operates near 8,000 stores and 1,500 pharmacies in 14 Asian and European markets, including Hong Kong, Indonesia, Macau, mainland China, Malaysia, the Philippines, Singapore, Taiwan, Thailand, Turkey, United Arab Emirates, Ukraine, Russia and Vietnam. History Founding and move to Hong Kong Dr. Thomas Boswell Watson (1815–1860), from Scotland, was the first member of the Watson family to arrive in the Far East, where in 1845 he set up a private practice in Macau. p. 221 After selling his practice to a fellow doctor, he moved to Hong Kong in 1856 where he became part owner of the Hong Kong Dispensary, an offshoot of the Canton Dispensary which operated from 1828 to 1858. Known as the "Big Medicine Shop" (; Cantonese: ''Dai Yeuk Fong''), the dispensary's main customer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
April Fools' Day
April Fools' Day or All Fools' Day is an annual custom on 1 April consisting of practical jokes and hoaxes. Jokesters often expose their actions by shouting "April Fools!" at the recipient. Mass media can be involved in these pranks, which may be revealed as such the following day. The custom of setting aside a day for playing harmless pranks upon one's neighbour has been relatively common in the world historically. Origins Although the origins of April Fools’ is unknown, there are many theories surrounding it. A disputed association between 1 April and foolishness is in Geoffrey Chaucer's '' The Canterbury Tales'' (1392). In the " Nun's Priest's Tale", a vain cock Chauntecleer is tricked by a fox on "Since March began thirty days and two," i.e. 32 days since March began, which is 1 April. However, it is not clear that Chaucer was referencing 1 April since the text of the "Nun's Priest's Tale" also states that the story takes place on the day when the sun is "in the sign ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peel Tower
Peel towers (also spelt pele) are small fortified keeps or tower houses, built along the English and Scottish borders in the Scottish Marches and North of England, mainly between the mid-14th century and about 1600. They were free-standing with defence being a prime consideration of their design with "confirmation of status and prestige" also playing a role. They also functioned as watch towers where signal fires could be lit by the garrison to warn of approaching danger. The FISH Vocabulary ''Monument Types Thesaurus'' lists "pele" alongside "bastle", "fortified manor house" and "tower house" under the broader term "fortified house". Pevsner defines a peel as simply a stone tower. Outside of this, "peel" or "pele" can also be used in related contexts, for example a "pele" or "barmkin" (in Ireland a bawn) was an enclosure where livestock were herded in times of danger. The rustling of livestock was an inevitable part of Border raids, and often their main purpose. In th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
