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Kersal Moor
Kersal Moor is a recreation area in Kersal, Greater Manchester, England which consists of eight hectares of moorland bounded by Moor Lane, Heathlands Road, St. Paul's Churchyard and Singleton Brook. Kersal Moor, first called Karsey or Carsall Moor,Farrer, William and Brownbill, J. (editors) (1911). 'Townships: Broughton', ''A History of the County of Lancaster'': Volume 4, pp. 217–222. URL: http://www.british-history.ac.uk/report.aspx?compid=41408. Date accessed: 20 February 2008 originally covered a much larger area, running down to the River Irwell. Evidence of activity during the Neolithic period has been discovered and the area was used by the Romans. It was the site of the first Manchester Racecourse and the second golf course to be built outside Scotland. It has been extensively used for other sporting pursuits, military manoeuvres and public gatherings such as the Great Chartist Meeting of 1838, prompting the political theorist Friedrich Engels to dub it "the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kersal
Kersal is a suburb and district of Salford in the City of Salford, Greater Manchester, England, northwest of Manchester and was historically part of the county of Lancashire. History Kersal has been variously known as Kereshale, Kershal, Kereshole, Carshall and Kersall.see'Townships: Broughton', A History of the County of Lancaster: Volume 4 (1911), pp. 217–222. URL: http://www.british-history.ac.uk/report.aspx?compid=41408. Retrieved 28 October 2007 The name incorporates the Old English word ''halh'', meaning "a piece of flat alluvial land by the side of a river". "''Kers''al" indicates that this was land where cress grew. In 1142, Kereshale was given to the Priory of Lenton, an order of Cluniac monks, who established an early cell there named St Leonard's. On the Dissolution of the Monasteries in 1540 Henry VIII sold the priory and its lands to one Baldwin Willoughby. It was sold eight years later to Ralph Kenyon, who was acting on behalf of himself, James Cheth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gorse
''Ulex'' (commonly known as gorse, furze, or whin) is a genus of flowering plants in the family Fabaceae. The genus comprises about 20 species of thorny evergreen shrubs in the subfamily Faboideae of the pea family Fabaceae. The species are native to parts of western Europe and northwest Africa, with the majority of species in Iberia. Gorse is closely related to the brooms and like them has green stems and very small leaves and is adapted to dry growing conditions. However it differs in its extreme thorniness, the shoots being modified into branched thorns long, which almost wholly replace the leaves as the plant's functioning photosynthetic organs. The leaves of young plants are trifoliate, but in mature plants they are reduced to scales or small spines. All the species have yellow flowers, generally showy, some with a very long flowering season. Species The greatest diversity of ''Ulex'' species is found in the Iberian Peninsula, and most species have narrow distri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Common Broom
''Cytisus scoparius'' ( syn. ''Sarothamnus scoparius''), the common broom or Scotch broom, is a deciduous leguminous shrub native to western and central Europe. In Britain and Ireland, the standard name is broom; this name is also used for other members of the Genisteae tribe, such as French broom or Spanish broom; and the term ''common broom'' is sometimes used for clarification. In other English-speaking countries, the most common name is "Scotch broom" (or Scots broom); however, it is known as English broom in Australia. Classification The two subspecies of ''Cytisus scoparius'' are: * ''Cytisus scoparius'' subsp. ''scoparius'' - throughout the species' range * ''Cytisus scoparius'' subsp. ''maritimus'' (Rouy) Heywood - Western Europe, on maritime cliffs, differs in prostrate growth, not over 0.4 m tall, and downy young shoots Cultivation ''Cytisus scoparius'' is widely cultivated as an ornamental plant, with several cultivars selected for variation in flower colour, inclu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fern
A fern (Polypodiopsida or Polypodiophyta ) is a member of a group of vascular plants (plants with xylem and phloem) that reproduce via spores and have neither seeds nor flowers. The polypodiophytes include all living pteridophytes except the lycopods, and differ from mosses and other bryophytes by being vascular, i.e., having specialized tissues that conduct water and nutrients and in having life cycles in which the branched sporophyte is the dominant phase. Ferns have complex leaves called megaphylls, that are more complex than the microphylls of clubmosses. Most ferns are leptosporangiate ferns. They produce coiled fiddleheads that uncoil and expand into fronds. The group includes about 10,560 known extant species. Ferns are defined here in the broad sense, being all of the Polypodiopsida, comprising both the leptosporangiate ( Polypodiidae) and eusporangiate ferns, the latter group including horsetails, whisk ferns, marattioid ferns, and ophioglossoid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grasses
Poaceae () or Gramineae () is a large and nearly ubiquitous family of monocotyledonous flowering plants commonly known as grasses. It includes the cereal grasses, bamboos and the grasses of natural grassland and species cultivated in lawns and pasture. The latter are commonly referred to collectively as grass. With around 780 genera and around 12,000 species, the Poaceae is the fifth-largest plant family, following the Asteraceae, Orchidaceae, Fabaceae and Rubiaceae. The Poaceae are the most economically important plant family, providing staple foods from domesticated cereal crops such as maize, wheat, rice, barley, and millet as well as feed for meat-producing animals. They provide, through direct human consumption, just over one-half (51%) of all dietary energy; rice provides 20%, wheat supplies 20%, maize (corn) 5.5%, and other grains 6%. Some members of the Poaceae are used as building materials (bamboo, thatch, and straw); others can provide a source of bi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ericaceae
The Ericaceae are a family of flowering plants, commonly known as the heath or heather family, found most commonly in acidic and infertile growing conditions. The family is large, with c.4250 known species spread across 124 genera, making it the 14th most species-rich family of flowering plants. The many well known and economically important members of the Ericaceae include the cranberry, blueberry, huckleberry, rhododendron (including azaleas), and various common heaths and heathers ('' Erica'', '' Cassiope'', '' Daboecia'', and ''Calluna'' for example). Description The Ericaceae contain a morphologically diverse range of taxa, including herbs, dwarf shrubs, shrubs, and trees. Their leaves are usually evergreen, alternate or whorled, simple and without stipules. Their flowers are hermaphrodite and show considerable variability. The petals are often fused ( sympetalous) with shapes ranging from narrowly tubular to funnelform or widely urn-shaped. The corollas are usually rad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mosses
Mosses are small, non-vascular flowerless plants in the taxonomic division Bryophyta (, ) ''sensu stricto''. Bryophyta (''sensu lato'', Schimp. 1879) may also refer to the parent group bryophytes, which comprise liverworts, mosses, and hornworts. Mosses typically form dense green clumps or mats, often in damp or shady locations. The individual plants are usually composed of simple leaves that are generally only one cell thick, attached to a stem that may be branched or unbranched and has only a limited role in conducting water and nutrients. Although some species have conducting tissues, these are generally poorly developed and structurally different from similar tissue found in vascular plants. Mosses do not have seeds and after fertilisation develop sporophytes with unbranched stalks topped with single capsules containing spores. They are typically tall, though some species are much larger. ''Dawsonia'', the tallest moss in the world, can grow to in height. There are appr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edward William Binney
Edward William Binney FRS, FGS (1812–1882) was an English geologist. Background Edward William Binney was born at Morton, in Nottinghamshire in 1812, and educated at Queen Elizabeth's Grammar School, Gainsborough. He was articled to a solicitor in Chesterfield, and settled in Manchester in 1836. He retired soon afterwards from legal practice and gave his chief attention to geological pursuits. Geological Research Working especially on the Carboniferous and Permian rocks of the north of England, he also studied the Drift deposits of Lancashire, which resulted in him and Joseph Dalton Hooker finding the first coal balls, and made himself familiar with the geology of the area around Manchester. On the Coal Measures in particular he became an acknowledged authority, and his ''Observations on the Structure of Fossil Plants found in the Carboniferous Strata'' (1868–75) formed one of the monographs of the Palaeontographical Society. His large collection of fossils was pl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system (stratigraphy), system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago (Year#Abbreviations yr and ya, Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic, 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 vert ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeozoic
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the ocean but ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Azoic
Azoic Age, Azoic Era, Azoic Period and Azoic Eon were terms used before 1950 to describe the age of rocks formed before the appearance of life in the geologic sequence. The word "Azoic" is derived from the Greek ''a-'' meaning without and ''zoön'' meaning animal (or living being), it was first used to mean ''without death''.Dana, James Dwight (1863) ''Manual of geology: Treating of the Principles of the Science with Special Reference to American geological history, for the use of colleges, academies, and schools of science'' T. Bliss & Co., Philadelphia, p.130 [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
