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Yeolmbridge
Yeolmbridge is a village in Cornwall (but within the boundaries of the historic county of Devon), two and a half miles north of Launceston. Yeolm Bridge The village takes its name from the bridge, Yeolm Bridge which crosses the River Ottery and is Grade I listed and a Scheduled Ancient Monument. Built about 1350, it is considered the oldest surviving and best built of medieval Cornish bridges. In 1951 Nikolaus Pevsner described it as Cornwall's "most ambitious" bridge. Quarry Yeolmbridge Quarry SSSI is 250 m to the east of the village. The quarry is designated a Site of Special Scientific Interest and a Geological Conservation Review (GCR) site, as the type–locality of the Yeolmbridge Formation; a black shale which shows the Devonian–Carboniferous boundary around 359 million years ago with a sequence of fossils. Notable people *Joan Rendell Joan Rendell MBE (1921 – 4 May 2010) was an English historian, writer (mainly on Cornish subjects), and phillumenist. Li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Ottery
The River Ottery ( kw, Otri) is a small river in northeast Cornwall, United Kingdom. The river is about long from its source southeast of Otterham to its confluence with the River Tamar at Nether Bridge, northeast of Launceston. The headwaters of the River Ottery are within the civil parish of Otterham but formerly came under the parish of Forrabury and Minster. In 1311, the rector of that parish wrote: "..the river Ottery takes its rise in this parish and flows to Canworthy Water and so by Yeolmbridge to the river Tamar." Hydrology and course With its tributaries, the River Ottery forms a major sub-catchment of the Tamar system, draining of north Cornwall. The River Ottery's catchment area is within the Carboniferous geological formation known as the Culm Measures which stretches from Dartmoor to north Devon and across northeast Cornwall as far west as Bodmin Moor. The infant river initially flows north until it reaches the hamlet of Trengune. From here it adopts an e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Werrington, Cornwall
Werrington ( kw, Trewolvredow) is a civil parish and former manor now in Cornwall, England, United Kingdom. Prior to boundary changes it straddled the Tamar and lay within the county of Devon. The portion on the west side was transferred to Cornwall in 1966.Pevsner, Nikolaus & Cherry, Bridget, The Buildings of England: Devon, London, 2004, p.896 It is situated to the west of the Tamar, the traditional boundary between Devon and Cornwall, and north of Launceston. Geography White's ''Devonshire Directory'' (1850) described the parish of Werrington as being near the River Tamar and the Bude Canal and having an area of c. 5,000 acres. Yeolmbridge, Druxton and Eggbeer were then within the parish which was included in Black Torrington Hundred. Druxton Bridge is a Grade II* listed 16th century road bridge. Manor The descent of the manor of Werrington was as follows: Crown Before the Norman Conquest of 1066, the manor of Werrington, in the hundred of Black Torrington, was the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Joan Rendell
Joan Rendell MBE (1921 – 4 May 2010) was an English historian, writer (mainly on Cornish subjects), and phillumenist. Life Rendell was born in Plymouth, Devon, in 1921. She was the daughter of Gervase Rendell, born 1879 in Eastry, Kent. For most of her life her home was at Werrington, Cornwall. She was the author of more than 30 books, mainly on Cornish subjects. In September 1980 she was made a Bard of Gorsedh Kernow, taking the name ''Scryfer Weryn'' (Writer of Werrington). She was also an avid collector of matchbox covers and had an estimated collection of 300,000. Another interest was corn dolly making, on which she also wrote a book. Rendell died in a fire at her bungalow in Yeolmbridge, near Launceston, Cornwall, on 4 May 2010. Awards Rendell was awarded the MBE in 1958, for raising £100,000 in National Savings stamps. She went on to be national chairman of the National Savings Bank. In 1977 she was awarded the Queen's Silver Jubilee Medal.Notes in ''Superstitio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Launceston, Cornwall
Launceston ( or , locally or , kw, Lannstevan; rarely spelled Lanson as a local abbreviation) is a town, ancient borough, and civil parish in Cornwall, England, United Kingdom. It is west of the middle stage of the River Tamar, which constitutes almost the entire border between Cornwall and Devon. The landscape of the town is generally steep particularly at a sharp south-western knoll topped by Launceston Castle. These gradients fall down to the River Kensey and smaller tributaries. The town centre itself is bypassed and is no longer physically a main thoroughfare. The A388 still runs through the town close to the centre. The town remains figuratively the "gateway to Cornwall", due to having the A30, one of the two dual carriageways into the county, pass directly next to the town. The other dual carriageway and alternative main point of entry is the A38 at Saltash over the Tamar Bridge and was completed in 1962. There are smaller points of entry to Cornwall on minor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geological Conservation Review
The Geological Conservation Review (GCR) is produced by the UK's Joint Nature Conservation Committee and is designed to identify those sites of national and international importance needed to show all the key scientific elements of the geological and geomorphological features of Britain. These sites display sediments, rocks, minerals, fossils, and features of the landscape that make a special contribution to an understanding and appreciation of Earth science and the geological history of Britain, which stretches back more than three billion years. The intention of the project, which was devised in 1974 by George Black and William Wimbledon working for the Governmental advisory agency, the Nature Conservancy Council (NCC), was activated in 1977. It aimed to provide the scientific rationale and information base for the conservation of geological SSSIs (Sites of Special Scientific Interest, protected under British law (latterly the Wildlife and Countryside Act 1981, as amended 1995). ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Villages In Cornwall
A village is a clustered human settlement or community, larger than a hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a church. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural England
Natural England is a non-departmental public body in the United Kingdom sponsored by the Department for Environment, Food and Rural Affairs. It is responsible for ensuring that England's natural environment, including its land, flora and fauna, freshwater and marine environments, geology and soils, are protected and improved. It also has a responsibility to help people enjoy, understand and access the natural environment. Natural England focuses its activities and resources on four strategic outcomes: * a healthy natural environment * enjoyment of the natural environment * sustainable use of the natural environment * a secure environmental future Roles and responsibilities As a non-departmental public body (NDPB), Natural England is independent of government. However, the Secretary of State for Environment, Food & Rural Affairs has the legal power to issue guidance to Natural England on various matters, a constraint that was not placed on its predecessor NDPBs. Its powers inc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Type Locality (geology)
Type locality, also called type area, is the locality where a particular rock type, stratigraphic unit or mineral species is first identified. If the stratigraphic unit in a locality is layered, it is called a stratotype, whereas the standard of reference for unlayered rocks is the type locality. The term is similar to the term type site in archaeology or the term type specimen in biology. Examples of geological type localities Rocks and minerals * Aragonite: Molina de Aragón, Guadalajara, Spain * Autunite: Autun, France * Benmoreite: Ben More (Mull), Scotland * Blairmorite: Blairmore, Alberta, Canada * Boninite: Bonin Islands, Japan * Comendite: Comende, San Pietro Island, Sardinia * Cummingtonite: Cummington, Massachusetts * Dunite: Dun Mountain, New Zealand. * Essexite: Essex County, Massachusetts, US * Fayalite: Horta, Fayal Island, Azores, Portugal * Harzburgite: Bad Harzburg, Germany * Icelandite: Thingmuli (Þingmúli), Iceland * Ijolite: Iivaara, Kuusamo, Finl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nikolaus Pevsner
Sir Nikolaus Bernhard Leon Pevsner (30 January 1902 – 18 August 1983) was a German-British art historian and architectural historian best known for his monumental 46-volume series of county-by-county guides, ''The Buildings of England'' (1951–74). Life Nikolaus Pevsner was born in Leipzig, Saxony, the son of Anna and her husband Hugo Pevsner, a Russian-Jewish fur merchant. He attended St. Thomas School, Leipzig, and went on to study at several universities, Munich, Berlin, and Frankfurt am Main, before being awarded a doctorate by Leipzig in 1924 for a thesis on the Baroque architecture of Leipzig. In 1923, he married Carola ("Lola") Kurlbaum, the daughter of distinguished Leipzig lawyer Alfred Kurlbaum. He worked as an assistant keeper at the Dresden Gallery between 1924 and 1928. He converted from Judaism to Lutheranism early in his life. During this period he became interested in establishing the supremacy of German modernist architecture after becoming aware of Le ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
