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Hapton Valley Colliery
Hapton Valley Colliery was a coal mine on the edge of Hapton, Lancashire, Hapton near Burnley in Lancashire, England. Its first shafts were sunk in the early 1850s and it had a life of almost 130 years, surviving to be the last deep mine operating on the Burnley Coalfield. Geology The Burnley Coalfield, separated from the South Lancashire Coalfield, is in the form of an oval bowl extending north-east from Blackburn, past Colne to the Pennines, Pennine Hills. Bounded by the Pendle Hill, Pendle monocline to the north and the Rossendale Valley anticline to the south, the coalfield is dissected by a series of predominately north-westerly trending Fault (geology), faults, the most significant fault is the Cliviger Valley Fault at Burnley with a throw of up to in Cliviger valley. The intersecting Theiveley Lead Mine Fault is one of a smaller number of easterly aligned structures. Unlike South Lancashire, only the Lower Westphalian (stage), Westphalian coal measures are available. The h ...
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Hapton, Lancashire
Hapton is a village and civil parish in the Borough of Burnley in Lancashire, England, west of Burnley, with a railway station on the East Lancashire Line. At the United Kingdom Census 2011, it had a population of 1,979. The parish adjoins the Burnley parishes of Dunnockshaw, Habergham Eaves and Padiham and Lowerhouse area of Burnley, the Hyndburn parish of Altham and Huncoat area of Accrington and the Loveclough area of Rossendale. The Leeds and Liverpool Canal and M65 motorway both pass through the village. History The name Hapton is thought to have been derived from the Old English words and meaning the enclosure on the hill. The civil parish of Hapton is thought to be the amalgamation of three medieval manors. Hapton is linked to the original castle and village that would later develop near it. To the northwest lies Shuttleworth, thought to be the origin of the family better known at Gawthorpe Hall. The third manor was called Birtwistle and its location is uncertai ...
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Glacial Till
image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is diagnostic of till. image:Glacial till exposed in roadcut-750px.jpg, Glacial till with tufts of grass Till or glacial till is unsorted glacier, glacial sediment. Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Description Till is a form of '' glacial drift'', which is rock material transported by a glacier and deposited directly from the ice or from running water emerging from the ice. It is distinguished from other forms of drift in that it is depos ...
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Drift Mining
Drift mining is either the mining of an ore deposit by underground methods, or the working of coal seams accessed by adits driven into the surface outcrop of the coal bed. A drift mine is an underground mine in which the entry or access is above water level and generally on the slope of a hill, driven horizontally into the ore seam. Random House dictionary says the origin of the term "drift mine" is an Americanism, circa 1885–1890. Drift is a more general mining term, meaning a near-horizontal passageway in a mine, following the bed (of coal, for instance) or vein of ore. A drift may or may not intersect the ground surface. A drift follows the vein, as distinguished from a crosscut that intersects it, or a level or gallery, which may do either. All horizontal or subhorizontal development openings made in a mine have the generic name of drift. These are simply tunnels made in the rock, with a size and shape depending on their use—for example, haulage, ventilation, or exp ...
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Track Gauge
In rail transport, track gauge (in American English, alternatively track gage) is the distance between the two rails of a railway track. All vehicles on a rail network must have wheelsets that are compatible with the track gauge. Since many different track gauges exist worldwide, gauge differences often present a barrier to wider operation on railway networks. The term derives from the metal bar, or gauge, that is used to ensure the distance between the rails is correct. Railways also deploy two other gauges to ensure compliance with a required standard. A '' loading gauge'' is a two-dimensional profile that encompasses a cross-section of the track, a rail vehicle and a maximum-sized load: all rail vehicles and their loads must be contained in the corresponding envelope. A ''structure gauge'' specifies the outline into which structures (bridges, platforms, lineside equipment etc.) must not encroach. Uses of the term The most common use of the term "track gauge" refers to the ...
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Stationary Steam Engine
Stationary steam engines are fixed steam engines used for pumping or driving mills and factories, and for power generation. They are distinct from locomotive engines used on railways, traction engines for heavy steam haulage on roads, steam cars (and other motor vehicles), agricultural engines used for ploughing or threshing, marine engines, and the steam turbines used as the mechanism of power generation for most nuclear power plants. They were introduced during the 18th century and widely made for the whole of the 19th century and most of the first half of the 20th century, only declining as electricity supply and the internal combustion engine became more widespread. Types of stationary steam engine There are different patterns of stationary steam engines, distinguished by the layout of the cylinders and crankshaft: * Beam engines have a rocking beam providing the connection between the vertical cylinder and crankshaft. *Table engines have the crosshead above the vert ...
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Tram Road
Tramways are lightly laid railways, sometimes with the wagons or carriages moved without locomotives. Because individual tramway infrastructure is not intended to carry the weight of typical standard-gauge railway equipment, the tramways over which they operate may be built from less substantial materials. Tramways can exist in many forms; sometimes just tracks temporarily placed on the ground to transport materials around a factory, mine or quarry. Many, if not most, use narrow-gauge railway technology. The trains can be manually pushed by hand, pulled by animals (especially horses and mules), cable hauled by a stationary engine, or use small, light locomotives. The term is not in use in North America but in common use in the United Kingdom, and elsewhere, where British Railway terminology and practices had large influences on management practices, terminology, and railway cultures such as Australia, New Zealand, and those parts of Asia that consulted with British experts whe ...
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Green Brook, Lancashire
Green Brook is a minor river in Lancashire, England. It is long, and including tributaries, has the catchment area of . Green Brook begins at the confluence of ''Hapton Clough'' and ''Habergham Clough'' in Spa Wood, next to the cemetery of Burnley. Hapton Clough is the product of ''Thorny Bank Clough'' and ''Tower Brook'', which meet near Old Barn Farm, in Hapton. While Habergham Clough begins at the confluence of New Barn Clough and Micklehurst Clough, near ''Iron House Farm'', in Habergham Eaves. From Spa Wood, Green Brook heads north, into one tunnel, which passes under the A679 Accrington Road, the Leeds and Liverpool Canal, the East Lancashire Railway Line, and the M65 Motorway, to emerge at ''Lowerhouse Lodges''. In Lowerhouse, it collects Sweet Clough, and turns west into Padiham Padiham ( ) is a town and civil parish on the River Calder, about west of Burnley, Lancashire, England. It forms part of the Borough of Burnley. Originally by the River Calder, it is ...
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Green Brook, Spa Wood
Green is the color between cyan and yellow on the visible spectrum. It is evoked by light which has a dominant wavelength of roughly 495570 nm. In subtractive color systems, used in painting and color printing, it is created by a combination of yellow and cyan; in the RGB color model, used on television and computer screens, it is one of the additive primary colors, along with red and blue, which are mixed in different combinations to create all other colors. By far the largest contributor to green in nature is chlorophyll, the chemical by which plants photosynthesize and convert sunlight into chemical energy. Many creatures have adapted to their green environments by taking on a green hue themselves as camouflage. Several minerals have a green color, including the emerald, which is colored green by its chromium content. During post-classical and early modern Europe, green was the color commonly associated with wealth, merchants, bankers, and the gentry, while red was r ...
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Coke (fuel)
Coke is a grey, hard, and porous coal-based fuel with a high carbon content and few impurities, made by heating coal or oil in the absence of air—a destructive distillation process. It is an important industrial product, used mainly in iron ore smelting, but also as a fuel in stoves and forges when air pollution is a concern. The unqualified term "coke" usually refers to the product derived from low-ash and low-sulphur bituminous coal by a process called coking. A similar product called petroleum coke, or pet coke, is obtained from crude oil in oil refineries. Coke may also be formed naturally by geologic processes.B. Kwiecińska and H. I. Petersen (2004): "Graphite, semi-graphite, natural coke, and natural char classification — ICCP system". ''International Journal of Coal Geology'', volume 57, issue 2, pages 99-116. History China Historical sources dating to the 4th century describe the production of coke in ancient China. The Chinese first used coke for heating ...
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Metallurgical
Metallurgy is a domain of materials science and engineering that studies the physical and chemical behavior of metallic elements, their inter-metallic compounds, and their mixtures, which are known as alloys. Metallurgy encompasses both the science and the technology of metals; that is, the way in which science is applied to the production of metals, and the engineering of metal components used in products for both consumers and manufacturers. Metallurgy is distinct from the craft of metalworking. Metalworking relies on metallurgy in a similar manner to how medicine relies on medical science for technical advancement. A specialist practitioner of metallurgy is known as a metallurgist. The science of metallurgy is further subdivided into two broad categories: chemical metallurgy and physical metallurgy. Chemical metallurgy is chiefly concerned with the reduction and oxidation of metals, and the chemical performance of metals. Subjects of study in chemical metallurgy include mi ...
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Hameldon Hill
Hameldon Hill is a Carboniferous sandstone hill with a summit elevation of , situated between the towns of Burnley and Accrington in Lancashire, England. It is listed as a "HuMP" or "Hundred Metre Prominence", its parent being Freeholds Top, a Marilyn near Bacup. Other nearby settlements include Hapton and hamlets of Clowbridge and Dunnockshaw in the Borough of Burnley, Huncoat and Baxenden in Hyndburn, and Crawshawbooth, Goodshaw and Loveclough in the Borough of Rossendale. Located on the western side of the Pennines, its summit is the highest point an isolated area, separated from the South Pennines and the West Pennine Moors. The Cliviger Gorge lies to the east, the Rossendale Valley to the south, and the valley of the River Hyndburn to the west. Pendle Hill stands to the north, across the wide valley of the Lancashire Calder. History The name Hameldon is used for two others in the local area, and is possibly the same as Hambledon Hill in Dorset. The second element i ...
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Outcrop
An outcrop or rocky outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth. Features Outcrops do not cover the majority of the Earth's land surface because in most places the bedrock or superficial deposits are covered by soil and vegetation and cannot be seen or examined closely. However, in places where the overlying cover is removed through erosion or tectonic uplift, the rock may be exposed, or ''crop out''. Such exposure will happen most frequently in areas where erosion is rapid and exceeds the weathering rate such as on steep hillsides, mountain ridges and tops, river banks, and tectonically active areas. In Finland, glacial erosion during the last glacial maximum (ca. 11000 BC), followed by scouring by sea waves, followed by isostatic uplift has produced many smooth coastal and littoral outcrops. Bedrock and superficial deposits may also be exposed at the Earth's surface due to human excavations such as quarrying and build ...
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