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Burnett, Somerset
Burnett is a small village within the civil parish of Compton Dando, approximately from the River Chew in the Chew Valley within the Unitary Authority of Bath and North East Somerset in Somerset, England. The nearest town is Keynsham, which lies approximately north of the village. The parish had an acreage of . It is within the Bristol/ Bath Green Belt. History The origin of the name Burnett is most likely derived from the old English word , meaning a place cleared by burning, and the earliest evidence of a settlement was in the period of the Roman occupation. Burnett later appeared in the Domesday Book of 1086 with 30 inhabitants. In 1102 the village came under the control of the powerful ecclesiastical body of Tewkesbury Abbey and the Benedictine monks stopped to worship and rest at St Michael's Church en route to Glastonbury. The manor was held by Edith of Wessex, probably from the time of her marriage to King Edward the Confessor in 1045, until her death in 1074. Along wit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Compton Dando
Compton Dando is a small village and civil parish on the River Chew in the affluent Chew Valley in England. It is in the Bath and North East Somerset council area and ceremonial county of Somerset, and lies from Bristol, from Bath, and from Keynsham. The parish includes the villages of Chelwood, Burnett, Chewton Keynsham, Queen Charlton and Woollard, and has a population of 589. History It is on the route of the ancient Wansdyke, and lies on the Monarch's Way long-distance footpath. According to Robinson it is listed in the 1086 Domesday Book as ''Comtuna''. A compton was originally a 'valley enclosure'. In 1297 the name Dando was added after Godfrey or Geofrey de Anno. The parish of Compton Dando was part of the Keynsham Hundred, The village was held by Alexander de Alno in the 12th century. Governance The parish council has responsibility for local issues, including setting an annual precept (local rate) to cover the council’s operating costs and producin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Whitson
John Whitson (c. 1558 – 1629) was an English merchant and politician who sat in the House of Commons at various times between 1605 and 1626. He also founded Redmaids School for girls. Later it became Redmaids High School for Girls when it joined Redland high a school founded by nuns in the 19th century. It also had a junior school founded. Life Whitson grew up in Clearwell in the Forest of Dean, and came to Bristol to start his career. Apprenticed to Nicholas Cutt, a member of the Society of Merchant Venturers in 1570, he lived in a house on Corn Street.McGrath, P, ''John Whitson and the Merchant Community of Bristol'', The University of Bristol, 1970 Cutt died in 1582, and it is presumed Whitson continued to work for his widow, Bridget, whom he married in 1585. They had their first child 8 months later. Following the wedding, John Whitson became a wealthy merchant in his own right. Whitson was a merchant and alderman of Bristol. He was Sheriff in 1589 and became Lord Mayo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South West England
South West England, or the South West of England, is one of nine official regions of England. It consists of the counties of Bristol, Cornwall (including the Isles of Scilly), Dorset, Devon, Gloucestershire, Somerset and Wiltshire. Cities and large towns in the region include Bath, Somerset, Bath, Bristol, Bournemouth, Cheltenham, Exeter, Gloucester, Plymouth and Swindon. It is geographically the largest of the nine regions of England covering , but the third-least populous, with approximately five million residents. The region includes the West Country and much of the ancient kingdom of Wessex. It includes two entire national parks of England and Wales, national parks, Dartmoor and Exmoor (a small part of the New Forest is also within the region); and four List of World Heritage Sites in the United Kingdom, World Heritage Sites: Stonehenge, the Cornwall and West Devon Mining Landscape, the Jurassic Coast and the Bath, Somerset, City of Bath. The northern part of Gloucestershi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coal
Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is formed when dead plant matter decays into peat and is converted into coal by the heat and pressure of deep burial over millions of years. Vast deposits of coal originate in former wetlands called coal forests that covered much of the Earth's tropical land areas during the late Carboniferous ( Pennsylvanian) and Permian times. Many significant coal deposits are younger than this and originate from the Mesozoic and Cenozoic eras. Coal is used primarily as a fuel. While coal has been known and used for thousands of years, its usage was limited until the Industrial Revolution. With the invention of the steam engine, coal consumption increased. In 2020, coal supplied about a quarter of the world's primary energy and over a third of its electricity. Some iron ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pensford
Pensford is the largest village in the civil parish of Publow in Somerset, England. It lies in the Chew Valley, approximately south of Bristol, west of Bath and north of Wells. It is on the A37 road from Bristol to Shepton Mallet. Pensford was identified as being of special architectural and historic interest and was designated as a Conservation Area in May 1988. History The name Pensford is in all likelihood derived from Brythonic ''Penffordd'', meaning roughly 'top of the road' or 'the highest or furthest point of the road'. Alternatively, it may mean 'The animal pens by the ford' from the Old English ''pens'' and ''ford''. The parish of Pensford was part of the Keynsham Hundred, During the 14th to 16th centuries Pensford was a cloth centre based on local wool. On 24 June 1685 rebel forces camped at Pensford during the Monmouth Rebellion. During the 19th and 20th centuries the main industry was coal mining, with Pensford and the surrounding area forming a major ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mercia Mudstone
The Mercia Mudstone Group is an early Triassic lithostratigraphic group (a sequence of rock strata) which is widespread in Britain, especially in the English Midlands – the name is derived from the ancient kingdom of Mercia which corresponds to that area. It is frequently encountered in older literature as the Keuper Marl or Keuper Marl Series. The Mercia Mudstone Group is now divided into five formations recognised and mappable across its entire outcrop and subcrop. The formations are a mix of mudstones, siltstones, sandstones and halites. Historically this sequence of rocks has been subdivided in different ways with different names in each of the basinal areas in which it is found. Increasing knowledge of the sequences and the more recent development of seamless electronic mapping by the British Geological Survey (BGS) necessitated a reappraisal of these divisions. A report published by BGS in 2008 recommended the abandonment of previous divisions and naming schemes in favour o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
White Lias
The Lilstock Formation is a geologic formation in England. It preserves bivalve, insect and other invertebrate fossils, as well as fossil fish of '' Agkistracanthus mitgelensis'' and the basal theropod dinosaur '' Newtonsaurus cambrensis'' dating back to the Rhaetian of the Triassic period. White Lias The White lias is a rare, fine-grained form of limestone from the late Triassic period, occurring only in certain parts of Somerset and infrequently in Warwickshire. It gets the name ‘lias’ from the quarrymen's dialect for ‘layers’, referring to its natural state when quarried. White lias is part of the Langport Member of the Lilstock Formation, a multi-layered bed of stone formed from shale and limestone. At its base is a bone-bed yielding ancient marine, reptilian and ammonite fossils. White lias varies in colour from white-cream to pale grey and is traditionally used for building and flooring. Evidence of its use can be seen in manor houses, churches and cathedral ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blue Lias
The Blue Lias is a geological formation in southern, eastern and western England and parts of South Wales, part of the Lias Group. The Blue Lias consists of a sequence of limestone and shale layers, laid down in latest Triassic and early Jurassic times, between 195 and 200 million years ago. The Blue Lias is famous for its fossils, especially ammonites. Its age corresponds to the Rhaetian to lower Sinemurian stages of the geological timescale, thus fully including the Hettangian stage. It is the lowest of the three divisions of the Lower Jurassic period and, as such, is also given the name ''Lower Lias''. Stratigraphically it can be subdivided into three members: the Wilmcote Limestone, Saltford Shale and Rugby Limestone. Lithology and facies The Blue Lias comprises decimetre scale alternations of argillaceous limestone and mudstone. These alternations are caused by short-term climatic variations during the Early Jurassic attributed to orbital forcing (Milankovitch cycles). Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lias Group
The Lias Group or Lias is a lithostratigraphic unit (a sequence of rock strata) found in a large area of western Europe, including the British Isles, the North Sea, the Low Countries and the north of Germany. It consists of marine limestones, shales, marls and clays. ''Lias'' is a Middle English term for hard limestone, used in this specific sense by geologists since 1833. In the past, geologists used ''Lias'' not only for the sequence of rock layers, but also for the timespan during which they were formed. It was thus an alternative name for the Early Jurassic epoch of the geologic timescale. It is now more specifically known that the Lias is Rhaetian to Toarcian in age (over a period of 20 million years between ) and thus also includes a part of the Triassic. The use of the name "Lias" for a unit of time is therefore slowly disappearing. Subdivisions In southern England, the Lias Group is often divided into Lower, Middle and Upper subgroups. In Southern England the Lias is d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
