|
Hove, Sussex
Hove ( ) is a seaside resort in East Sussex, England. Alongside Brighton, it is one of the two main parts of the city of Brighton and Hove. Originally a fishing village surrounded by open farmland, it grew rapidly in the 19th century in response to the development of its eastern neighbour Brighton; by the Victorian era it was a fully developed town with borough status. Neighbouring parishes such as Aldrington and Hangleton were annexed in the late 19th and early 20th centuries. The neighbouring urban district of Portslade was merged with Hove in 1974. In 1997, as part of local government reform, the borough merged with Brighton to form the Borough of Brighton and Hove; this unitary authority was granted city status in 2000. Name and etymology Old spellings of Hove include Hou (Domesday Book, 1086), la Houue (1288), Huua (13th century), Houve (13th and 14th centuries), Huve (14th and 15th centuries), Hova (16th century) and Hoova (1675). The etymology was disputed at length du ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hove (UK Parliament Constituency)
Hove and Portslade is a borough constituency in East Sussex represented in the House of Commons of the UK Parliament since 2015 by Peter Kyle of the Labour Party, who currently serves as Secretary of State for Science, Innovation and Technology in the government of Keir Starmer. It was previously called Hove. Further to the 2023 Periodic Review of Westminster constituencies, enacted by the Parliamentary Constituencies Order 2023, there were no changes to the constituency boundaries, but it was renamed from the 2024 general election. Before it was renamed, it had the joint shortest name of any constituency of the UK Parliament, with 4 letters, the same as Bath. Boundaries 1950–1983: The County Borough of Hove, and the Urban District of Portslade-by-Sea. 1983–2010: The Borough of Hove. 2010–2023: The City of Brighton and Hove wards of Brunswick and Adelaide, Central Hove, Goldsmid, Hangleton and Knoll, Hove Park, North Portslade, South Portslade, Westbourne, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bronze Age
The Bronze Age () was a historical period characterised principally by the use of bronze tools and the development of complex urban societies, as well as the adoption of writing in some areas. The Bronze Age is the middle principal period of the three-age system, following the Stone Age and preceding the Iron Age. Conceived as a global era, the Bronze Age follows the Neolithic, with a transition period between the two known as the Chalcolithic. The final decades of the Bronze Age in the Mediterranean basin are often characterised as a period of widespread societal collapse known as the Late Bronze Age collapse (), although its severity and scope are debated among scholars. An ancient civilisation is deemed to be part of the Bronze Age if it either produced bronze by smelting its own copper and alloying it with tin, arsenic, or other metals, or traded other items for bronze from producing areas elsewhere. Bronze Age cultures were the first to History of writing, develop writin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shingle Beach
A shingle beach, also known as either a cobble beach or gravel beach, is a commonly narrow beach that is composed of coarse, loose, well-rounded, and waterworn gravel, called ''shingle''. The gravel (shingle) typically consists of smooth, spheroidal to flattened, pebbles, cobbles, and sometimes small boulders, generally in the size range. Shingle beaches typically have a steep slope on both their landward and seaward sides. Shingle beaches form in wave-dominated locations where resistant bedrock cliffs provide gravel-sized rock debris. They are also found in high latitudes and temperate shores where the erosion of Quaternary glacial deposits provide gravel-size rock fragments. This term is most widely used in Great Britain.Neuendorf, Klaus K.E. Mehl, James P., Jr. Jackson, Julia A., 2011. ''Glossary of Geology'' (5th Edition). American Geosciences Institute. Narayana, A. C., 2016. ''Coastal landforms''. in Kennish, M.J., ed., pp. 143–157, ''Encyclopedia of Estuaries''. Spr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Storm Beach
A storm beach is a beach affected by particularly fierce wind wave, waves, usually with a very long fetch (geography), fetch. The resultant landform is often a very steep beach (up to 45°) composed of rounded Cobble (geology), cobbles, shingle beach, shingle and occasionally sand. The stones usually have an obvious Grade (slope), grading of pebbles, from large to small, with the larger diameter stones typically arrayed at the highest beach elevations. It may also contain many small parts of shipwrecked boats. Examples A noted textbook example is the long Chesil Beach in Dorset, one of three major shingle structures in Britain. It also connects the Isle of Portland to the mainland at Abbotsbury, west of the resort of Weymouth, Dorset, Weymouth. Other examples appear in the Shetland Islands, Shetland and Orkney Islands, as well as the Scotland, Scottish mainland at Caithness. The beaches of Lakshdweep Islands are also storm beaches. Gallery File:Storm Beach - geograph.org.uk - ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brickearth
Brickearth is a term originally used to describe Superficial deposits, superficial windblown deposits found in southern England. The term has been employed in English-speaking regions to describe similar deposits. Brickearths are periglacial loess, a wind-blown dust deposited under extremely cold, dry, peri- or postglacial conditions. The name arises from its early use in making house bricks, its composition being suitable for brick-making without additional material being added; unlike clay, its bricks can be hardened (fused) at lower temperatures, including in wood-fired kilns. The brickearth is normally represented on 1:50,000 solid and drift edition geological maps. In the River Thames, Thames valley, in broad patches brickearth overlies fluvial terrace gravel; it has been reclassified on later maps as the "Langley, Slough, Langley Silt Complex". Description Brickearth is a superficial deposit of homogeneous loam or silt [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flint
Flint, occasionally flintstone, is a sedimentary cryptocrystalline form of the mineral quartz, categorized as the variety of chert that occurs in chalk or marly limestone. Historically, flint was widely used to make stone tools and start fires. Flint occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones.''The Flints from Portsdown Hill'' Inside the nodule, flint is usually dark grey or black, green, white, or brown in colour, and has a glassy or waxy appearance. A thin, oxidised layer on the outside of the nodules is usually different in colour, typically white and rough in texture. The nodules can often be found along s and [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reading Formation
The Reading Formation is a geologic formation in southern England. It dates to the Paleocene period, and is part of the Lambeth Group. It overlies the London Basin and is below the Harwich Formation. The formation is composed of "a series of lenticular mottled clays and sands, here and there with pebbly beds and masses of fine sand converted into quartzite. These beds are generally unfossiliferous." Clay sources During the late medieval era, the Surrey whitewares pottery kilns were located near the Reading Formation, most notably the area between Farnham and Tongham The beds were an excellent source of white-firing clay. See also * List of fossiliferous stratigraphic units in England See also * Lists of fossiliferous stratigraphic units in Europe * Lists of fossiliferous stratigraphic units in the United Kingdom References * {{DEFAULTSORT:Fossiliferous stratigraphic units in England England England is a Countr ... References Paleogene England {{E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Woolwich Formation
The Woolwich Formation is a geological formation in southeast England. It preserves fossils dating back to the Paleogene period. See also * List of fossiliferous stratigraphic units in England See also * Lists of fossiliferous stratigraphic units in Europe * Lists of fossiliferous stratigraphic units in the United Kingdom References * {{DEFAULTSORT:Fossiliferous stratigraphic units in England England England is a Countr ... References * Paleogene England {{England-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalk Group
The Chalk Group (often just called the Chalk) is the lithostratigraphic unit (a certain number of rock strata) which contains the Upper Cretaceous limestone succession in southern and eastern England. The same or similar rock sequences occur across the wider northwest European chalk 'province'. It is characterised by thick deposits of chalk, a soft porous white limestone, deposited in a marine environment. Chalk is a limestone that consists of coccolith biomicrite. A biomicrite is a limestone composed of fossil debris ("bio") and calcium carbonate mud (" micrite"). Most of the fossil debris in chalk consists of the microscopic plates, which are called coccoliths, of microscopic green algae known as coccolithophores. In addition to the coccoliths, the fossil debris includes a variable, but minor, percentage of the fragments of foraminifera, ostracods and mollusks. The coccolithophores lived in the upper part of the water column. When they died, the microscopic calcium carbonat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalk
Chalk is a soft, white, porous, sedimentary carbonate rock. It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor. Chalk is common throughout Western Europe, where deposits underlie parts of France, and steep cliffs are often seen where they meet the sea in places such as the Dover cliffs on the Kent coast of the English Channel. Chalk is mined for use in industry, such as for quicklime, bricks and builder's putty, and in agriculture, for raising pH in soils with high acidity. It is also used for " blackboard chalk" for writing and drawing on various types of surfaces, although these can also be manufactured from other carbonate-based minerals, or gypsum. Description Chalk is a fine-textured, earthy type of limestone distinguished by its light colour, softness, and high porosity. It is composed mostly of tiny fragments of the calcite shells or sk ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hove Lawns - Geograph
Hove ( ) is a seaside resort in East Sussex, England. Alongside Brighton, it is one of the two main parts of the city of Brighton and Hove. Originally a fishing village surrounded by open farmland, it grew rapidly in the 19th century in response to the development of its eastern neighbour Brighton; by the Victorian era it was a fully developed town with borough status. Neighbouring parishes such as Aldrington and Hangleton were annexed in the late 19th and early 20th centuries. The neighbouring urban district of Portslade was merged with Hove in 1974. In 1997, as part of local government reform, the borough merged with Brighton to form the Borough of Brighton and Hove; this unitary authority was granted city status in 2000. Name and etymology Old spellings of Hove include Hou (Domesday Book, 1086), la Houue (1288), Huua (13th century), Houve (13th and 14th centuries), Huve (14th and 15th centuries), Hova (16th century) and Hoova (1675). The etymology was disputed at length d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
