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Sisland
Sisland, historically Sislanda, is a very small village, manor and parish in the county of Norfolk, England, about a mile west of Loddon. In the 2001 census, the population was 44 in 16 households. The parish covers an area of , and is approximately southeast of Norwich and west of Great Yarmouth. For the purposes of local government, it falls within the district of South Norfolk, however Sisland does have its own Parish Council. The village contains only one heritage-listed building, that being St Mary's Church, which is Grade II*. Location Sisland is located in the electoral district of Loddon which is located in the South Norfolk district of the county of Norfolk, England. Sisland lies at an average elevation of 16 meters, with a range of 11 to 21 meters, and is located 9.3 miles southeast of Norwich. Sisland borders Langley to the north, while in the north east, it borders Chedgrave, and in the north west it borders Thurton. In the west, it borders with Bergh Apton and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Norfolk
South Norfolk is a local government district in Norfolk, England. Its council is based in Long Stratton. The population of the Local Authority District was 124,012 as taken at the 2011 Census. History The district was formed on 1 April 1974 under the Local Government Act 1972, as a merger of Diss Urban District, Wymondham Urban District, Depwade Rural District, Forehoe and Henstead Rural District and Loddon Rural District. History of governance The below table outlines the composition of South Norfolk Council from 1973 to 2019. Recent elections 2019 saw the Conservatives lose five seats but retain overall control of the council. The boundaries used were new at this election and saw the Labour Party unexpectedly win a seat on the council for the first time since 2003 gaining Loddon (notionally) from the Conservatives. Liberal Democrat group leader Trevor Lewis, standing in a much changed ward, was not re-elected. /sup> Others: Independents and UKIP. Political comp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mundham
Mundham, historically Mundaham or Mundhala, is a small village and civil parish in the county of Norfolk, England. Archaeological and toponymic evidence of Mundham's existence predates its appearance in the Domesday survey of 1086, dating back to the early Anglo Saxon period. However, there has been activity in the area since the early Neolithic period, as well as a small Roman settlement which was located in the village. In the 2001 Census, the population was 168 in 63 households, this grew to 177 at the 2011 Census, however in the 2021 census, the population had dropped to 147. The parish covers an area of , and is approximately southeast of Norwich and west of Great Yarmouth. For the purposes of local government, it falls within the district of South Norfolk, however Mundham does have a Parish council responsible for local matters laid down by law, including a role in local planning, it consists of 5 councillors, and a clerk. The village contains a number of heritage-lis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Anglia
East Anglia is an area in the East of England, often defined as including the counties of Norfolk, Suffolk and Cambridgeshire. The name derives from the Anglo-Saxon kingdom of the East Angles, a people whose name originated in Anglia, in what is now Northern Germany. Area Definitions of what constitutes East Anglia vary. The Anglo-Saxon Kingdom of East Anglia, established in the 6th century, originally consisted of the modern counties of Norfolk and Suffolk and expanded west into at least part of Cambridgeshire, typically the northernmost parts known as The Fens. The modern NUTS 3 statistical unit of East Anglia comprises Norfolk, Suffolk and Cambridgeshire (including the City of Peterborough unitary authority). Those three counties have formed the Roman Catholic Diocese of East Anglia since 1976, and were the subject of a possible government devolution package in 2016. Essex has sometimes been included in definitions of East Anglia, including by the London Society o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kettleburgh
Kettleburgh is a small village and civil parish in the East Suffolk district, in the county of Suffolk. The population of this Civil Parish at the 2011 Census was 231. It is near the small towns of Wickham Market and Framlingham in the valley of the River Deben. The grade I listed church of St Andrew dates from the 14th century and was restored in 1890. The village also has a pub. Notable residents *Corrie Grant (1850-1924), journalist, barrister and Liberal Party politician who served as the Member of Parliament (MP) for the Rugby division of Warwickshire Warwickshire (; abbreviated Warks) is a county in the West Midlands region of England. The county town is Warwick, and the largest town is Nuneaton. The county is famous for being the birthplace of William Shakespeare at Stratford-upon-Avon an ... from 1900 to 1910. References Villages in Suffolk Civil parishes in Suffolk {{suffolk-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Advowson
Advowson () or patronage is the right in English law of a patron (avowee) to present to the diocesan bishop (or in some cases the ordinary if not the same person) a nominee for appointment to a vacant ecclesiastical benefice or church living, a process known as ''presentation'' (''jus praesentandi'', Latin: "the right of presenting"). The word derives, via French, from the Latin ''advocare'', from ''vocare'' "to call" plus ''ad'', "to, towards", thus a "summoning". It is the right to nominate a person to be parish priest (subject to episcopal – that is, one bishop's – approval), and each such right in each parish was mainly first held by the lord of the principal manor. Many small parishes only had one manor of the same name. Origin The creation of an advowson was a secondary development arising from the process of creating parishes across England in the 11th and 12th centuries, with their associated parish churches. A major impetus to this development was the legal exac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Henry II Of England
Henry II (5 March 1133 – 6 July 1189), also known as Henry Curtmantle (french: link=no, Court-manteau), Henry FitzEmpress, or Henry Plantagenet, was King of England from 1154 until his death in 1189, and as such, was the first Angevin king of England. King Louis VII of France made him Duke of Normandy in 1150. Henry became Count of Anjou and Maine upon the death of his father, Count Geoffrey V, in 1151. His marriage in 1152 to Eleanor of Aquitaine, former spouse of Louis VII, made him Duke of Aquitaine. He became Count of Nantes by treaty in 1158. Before he was 40, he controlled England; large parts of Wales; the eastern half of Ireland; and the western half of France, an area that was later called the Angevin Empire. At various times, Henry also partially controlled Scotland and the Duchy of Brittany. Henry became politically involved by the age of 14 in the efforts of his mother Matilda, daughter of Henry I of England, to claim the English throne, then occupied b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oceanic Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Temperate
In geography, the temperate climates of Earth occur in the middle latitudes (23.5° to 66.5° N/S of Equator), which span between the tropics and the polar regions of Earth. These zones generally have wider temperature ranges throughout the year and more distinct seasonal changes compared to tropical climates, where such variations are often small and usually only have precipitation changes. In temperate climates, not only do latitudinal positions influence temperature changes, but sea currents, prevailing wind direction, continentality (how large a landmass is) and altitude also shape temperate climates. The Köppen climate classification defines a climate as "temperate" C, when the mean temperature is above but below in the coldest month to account for the persistency of frost. However, other climate classifications set the minimum at . Zones and climates The north temperate zone extends from the Tropic of Cancer (approximately 23.5° north latitude) to the Arctic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (annum, Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphy, stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, evolution of mammals, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sand
Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural class of soil or soil type; i.e., a soil containing more than 85 percent sand-sized particles by mass. The composition of sand varies, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non-tropical coastal settings is silica (silicon dioxide, or SiO2), usually in the form of quartz. Calcium carbonate is the second most common type of sand, for example, aragonite, which has mostly been created, over the past 500million years, by various forms of life, like coral and shellfish. For example, it is the primary form of sand apparent in areas where reefs have dominated the ecosystem for millions of years like the Caribbean. Somewhat more rarely, sand may be composed of calciu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay particles, but become hard, brittle and non–plastic upon drying or firing. Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impurities, such as a reddish or brownish colour from small amounts of iron oxide. Clay is the oldest known ceramic material. Prehistoric humans discovered the useful properties of clay and used it for making pottery. Some of the earliest pottery shards have been dated to around 14,000 BC, and clay tablets were the first known writing medium. Clay is used in many modern industrial processes, such as paper making, cement production, and chemical filtering. Between one-half and two-thirds of the world's population live or work in buildings made with clay, often ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope Carbon-13, 13C in the atmosphere was exceptionally low in comparison with the more common isotope Carbon-12, 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Popigai impact structure, Siberia and in what is now ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
