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Clent Hills
The Clent Hills lie south-west of Birmingham city centre in Clent, Worcestershire, England. The closest towns are Stourbridge and Halesowen, both in the West Midlands conurbation (and also historically in Worcestershire). The Clent Hills range consists of, in order from north-west to south-east: Wychbury Hill, Clent Hill (and Adams Hill), and Walton Hill (and Calcot Hill). The north Worcestershire range of hills continues eastwards to include Romsley Hill, Waseley Hills and the Lickey Hills. Clent Hill is the most popular hillwalking hill in the range, although it is not often mentioned because the whole area is referred to as Clent Hills. Just under a million visitors a year are estimated to come to the hills, making them Worcestershire's most popular non-paying attraction. Geology The Clent Hills are a major outcrop of the Clent Formation consisting of Clent Breccia (predominantly a red-brown mudstone matrix) dating from the early part of the Permian period. The formation ...
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Worcestershire
Worcestershire ( , ; written abbreviation: Worcs) is a county in the West Midlands of England. The area that is now Worcestershire was absorbed into the unified Kingdom of England in 927, at which time it was constituted as a county (see History of Worcestershire). Over the centuries the county borders have been modified, but it was not until 1844 that substantial changes were made. Worcestershire was abolished as part of local government reforms in 1974, with its northern area becoming part of the West Midlands and the rest part of the county of Hereford and Worcester. In 1998 the county of Hereford and Worcester was abolished and Worcestershire was reconstituted, again without the West Midlands area. Location The county borders Herefordshire to the west, Shropshire to the north-west, Staffordshire only just to the north, West Midlands to the north and north-east, Warwickshire to the east and Gloucestershire to the south. The western border with Herefordshire includ ...
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Clent Breccia
Haffield Breccia, or Clent Breccia, (now known as the Haffield and Clent Formations) consist of a texturally immature compacted gravel, rich in volcanic clasts with some sedimentary rocks, in a sandy or muddy matrix, which outcrops in the English Midlands, in South Staffordshire, Birmingham and the Malverns. It is thought to have been deposited by during flash floods in rivers that were flowing through a desert, somewhere between 200 and 280 million years ago during the Permian period. The gravel consists of angular fragments, showing that they have not been transported over long distances.- - - See also *Clent Hills The Clent Hills lie south-west of Birmingham city centre in Clent, Worcestershire, England. The closest towns are Stourbridge and Halesowen, both in the West Midlands conurbation (and also historically in Worcestershire). The Clent Hills rang ... References Further reading * * Permian System of Europe Geologic formations of the United Kingdom {{UK- ...
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Scythe
A scythe ( ) is an agricultural hand tool for mowing grass or harvesting crops. It is historically used to cut down or reap edible grains, before the process of threshing. The scythe has been largely replaced by horse-drawn and then tractor machinery, but is still used in some areas of Europe and Asia. Reapers are bladed machines that automate the cutting of the scythe, and sometimes subsequent steps in preparing the grain or the straw or hay. The word "scythe" derives from Old English ''siðe''. In Middle English and later, it was usually spelt ''sithe'' or ''sythe''. However, in the 15th century some writers began to use the ''sc-'' spelling as they thought (wrongly) the word was related to the Latin ''scindere'' (meaning "to cut"). Nevertheless, the ''sithe'' spelling lingered and notably appears in Noah Webster's dictionaries. A scythe consists of a shaft about long called a ''snaith'', ''snath'', ''snathe'' or ''sned'', traditionally made of wood but now sometimes met ...
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Isaac Nash
Isaac; grc, Ἰσαάκ, Isaák; ar, إسحٰق/إسحاق, Isḥāq; am, ይስሐቅ is one of the three patriarchs of the Israelites and an important figure in the Abrahamic religions, including Judaism, Christianity, and Islam. He was the son of Abraham and Sarah, the father of Jacob and Esau, and the grandfather of the twelve tribes of Israel. Isaac's name means "he will laugh", reflecting the laughter, in disbelief, of Abraham and Sarah, when told by God that they would have a child., He is the only patriarch whose name was not changed, and the only one who did not move out of Canaan. According to the narrative, he died aged 180, the longest-lived of the three patriarchs. Etymology The anglicized name "Isaac" is a transliteration of the Hebrew name () which literally means "He laughs/will laugh." Ugaritic texts dating from the 13th century BCE refer to the benevolent smile of the Canaanite deity El. Genesis, however, ascribes the laughter to Isaac's parents, Abraham ...
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Belbroughton
Belbroughton ( ) is a village and civil parish in the Bromsgrove District of Worcestershire, England. According to the 2001 census it had a population of 2,380. It is about six miles north of Bromsgrove, six miles east of Kidderminster and four miles south of Stourbridge. The village of Clent is nearby. The village is served by bus service 318 (Bromsgrove-Stourbridge) operared by Kev's Cars and Coaches. History Belbroughton was at the core of the North Worcestershire scythe-making district. Many of the mills of the area were formerly blade mills used for sharpening them, after a scythesmith had forged them from iron, with a thin strip of steel along the cutting edge. From the late 18th century until about 1870, the Waldron family of Field House Clent were the leading manufacturers. They were succeeded by Isaac Nash, whose business finally closed in 1967. Scythes were formerly not just made in Belbroughton, but also several adjacent parishes, including Chaddesley Corbett. ...
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Watermill
A watermill or water mill is a mill that uses hydropower. It is a structure that uses a water wheel or water turbine to drive a mechanical process such as milling (grinding), rolling, or hammering. Such processes are needed in the production of many material goods, including flour, lumber, paper, textiles, and many metal products. These watermills may comprise gristmills, sawmills, paper mills, textile mills, hammermills, trip hammering mills, rolling mills, wire drawing mills. One major way to classify watermills is by wheel orientation (vertical or horizontal), one powered by a vertical waterwheel through a gear mechanism, and the other equipped with a horizontal waterwheel without such a mechanism. The former type can be further divided, depending on where the water hits the wheel paddles, into undershot, overshot, breastshot and pitchback (backshot or reverse shot) waterwheel mills. Another way to classify water mills is by an essential trait about their location: tide mills ...
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River Stour, Worcestershire
The Stour is a river flowing through the counties of Worcestershire, the West Midlands and Staffordshire in the West Midlands region of England. The Stour is a major tributary of the River Severn, and it is about in length. It has played a considerable part in the economic history of the region. Etymology and usage The river-name ''Stour'', common in England, does not occur at all in Wales; Crawford noted two tributaries of the Po River near Turin, spelled ''Sture''. In Germany the ''Stoer'' ( Stör) flows into the River Elbe. The name ''Stour'' is pronounced differently in different cases. The Kentish Stour rhymes with ''tour''; the Oxfordshire Stour is sometimes rhymes with ''mower'', sometimes with ''hour''. The Worcestershire and Suffolk Stour always rhyme with ''hour''. The origin of the name(s) remains in dispute. The Middle English word '' stour'' has two distinct meanings and derivations, still current enough to appear in most substantial dictionaries. As an adjec ...
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Uffmoor Wood
Uffmoor Wood is a semi-natural woodland in Worcestershire, in the English Midlands. It is one of over a thousand woods cared for by the Woodland Trust. The wood has an area of , and . Sitting at the foot of the Clent Hills and about 3 km southwest of Halesowen, Uffmoor Wood is a popular recreational destination for local people. Adjacent to Hagley Woods, with its mystery of 'Who put Bella in the Wych Elm? "Who put Bella down the Wych Elm?" is graffiti that appeared in 1944 following the 1943 discovery by four children of the skeletonised remains of a woman inside a wych elm in Hagley Wood, Hagley (located in the estate of Hagley Hall), in Worceste ...', and the site of several pre-war murders, Uffmoor has developed a reputation for the supernatural. In May 2017 the Trust temporarily suspended public access to the wood because of misbehaviour including dirt bike scrambling, drug peddling and public sexual acts. External linksWoodland Trust: Welcome to Uffmoor Wood - Haleso ...
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Escarpment
An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations. The terms ''scarp'' and ''scarp face'' are often used interchangeably with ''escarpment''. Some sources differentiate the two terms, with ''escarpment'' referring to the margin between two landforms, and ''scarp'' referring to a cliff or a steep slope. In this usage an escarpment is a ridge which has a gentle slope on one side and a steep scarp on the other side. More loosely, the term ''scarp'' also describes a zone between a coastal lowland and a continental plateau which shows a marked, abrupt change in elevation caused by coastal erosion at the base of the plateau. Formation and description Scarps are generally formed by one of two processes: either by differential erosion of sedimentary rocks, or by movement of the Earth's crust at a geologic fault. The first process is the more common type: the escarpment is ...
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Vine Inn - Geograph
A vine (Latin ''vīnea'' "grapevine", "vineyard", from ''vīnum'' "wine") is any plant with a growth habit of trailing or scandent (that is, climbing) stems, lianas or runners. The word ''vine'' can also refer to such stems or runners themselves, for instance, when used in wicker work.Jackson; Benjamin; Daydon (1928). ''A Glossary of Botanic Terms with their Derivation and Accent'', 4th ed. London: Gerald Duckworth & Co. In parts of the world, including the British Isles, the term "vine" usually applies exclusively to grapevines (''Vitis''), while the term "climber" is used for all climbing plants. Growth forms Certain plants always grow as vines, while a few grow as vines only part of the time. For instance, poison ivy and bittersweet can grow as low shrubs when support is not available, but will become vines when support is available. A vine displays a growth form based on very long stems. This has two purposes. A vine may use rock exposures, other plants, or other ...
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Warwickshire Group
The Warwickshire Group is a lithostratigraphic unit of rock strata defined within the British Carboniferous system. Within the Pennine Basin it overlies (i.e. postdates) the Coal Measures Group and is deemed to be of late Westphalian and Stephanian age. In the South Wales Coalfield it consists of the Pennant Sandstone Formation and overlying Grovesend Formation. It contains the youngest Carboniferous rocks in Britain. The name Warwickshire Group is a relatively recent one, replacing a variety of earlier names for the succession of coal-barren red-beds such as Barren Coal Measures and Red Measures which overlie the productive coal measures. It is derived from the Warwickshire Coalfield The Warwickshire Coalfield extends between Warwick and Tamworth in the English Midlands. It is about from north to south and its width is around half that distance. Its western margin is defined by the 'Western Boundary Fault'. In the northeast ... where they achieve their thickest develop ...
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually relate ...
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