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Douglas Navigation
The Douglas Navigation was a canalised section of the River Douglas or Asland, in Lancashire, England, running from its confluence with the River Ribble to Wigan. It was authorised in 1720, and some work was carried out, but the undertakers lost most of the share money speculating on the South Sea Bubble. Alexander Leigh attempted to revive it eleven years later, and opened it progressively between 1738 and 1742. Leigh began work on a parallel canal called Leigh's Cut to improve the passage from Newburgh to Gathurst, but progress was slow and it was unfinished in 1771. The working life of the navigation was short, as it was bought out by the Leeds and Liverpool Canal Company in 1772, to prevent a rival scheme to build a canal from Liverpool to Wigan. The canal company could not really afford the purchase price, but needed to secure the water supply to prevent the rival scheme from using it. The Leeds and Liverpool completed Leigh's Cut, built locks to enable sailing boats on th ...
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River Douglas, Lancashire
The River Douglas, also known as the River Asland or Astland, flows through parts of Lancashire and Greater Manchester in North West England. It is a tributary of the River Ribble and has several tributaries, the major ones being the River Tawd and the River Yarrow. In 1720 an act of Parliament was passed allowing Thomas Steers and William Squire to make the Douglas navigable to small ships between Wigan and its mouth. Amid financial irregularities, the Douglas Navigation was not completed until 1742, and by 1783, it had been superseded by the Leeds and Liverpool Canal. It reverted to being a river, although the remains of several locks can still be seen between Parbold and Gathurst. The Rufford Branch of the canal joins the river at Tarleton. The river rises on Winter Hill on the West Pennine Moors, and flows for through several towns and onto the Ribble estuary past Tarleton, the last or so being tidal. In 1892 the Douglas was diverted in Wigan to allow the construction ...
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South Sea Company
The South Sea Company (officially The Governor and Company of the merchants of Great Britain, trading to the South Seas and other parts of America, and for the encouragement of the Fishery) was a British joint-stock company founded in January 1711, created as a public-private partnership to consolidate and reduce the cost of the national debt. To generate income, in 1713 the company was granted a monopoly (the Asiento de Negros) to supply African slaves to the islands in the "South Seas" and South America. When the company was created, Britain was involved in the War of the Spanish Succession and Spain and Portugal controlled most of South America. There was thus no realistic prospect that trade would take place, and as it turned out, the Company never realised any significant profit from its monopoly. However, Company stock rose greatly in value as it expanded its operations dealing in government debt, and peaked in 1720 before suddenly collapsing to little above its ...
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Canals Opened In 1742
Canals or artificial waterways are waterways or engineered channels built for drainage management (e.g. flood control and irrigation) or for conveyancing water transport vehicles (e.g. water taxi). They carry free, calm surface flow under atmospheric pressure, and can be thought of as artificial rivers. In most cases, a canal has a series of dams and locks that create reservoirs of low speed current flow. These reservoirs are referred to as ''slack water levels'', often just called ''levels''. A canal can be called a ''navigation canal'' when it parallels a natural river and shares part of the latter's discharges and drainage basin, and leverages its resources by building dams and locks to increase and lengthen its stretches of slack water levels while staying in its valley. A canal can cut across a drainage divide atop a ridge, generally requiring an external water source above the highest elevation. The best-known example of such a canal is the Panama Canal. Many ca ...
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Canals In Lancashire
Canals or artificial waterways are waterways or engineered channels built for drainage management (e.g. flood control and irrigation) or for conveyancing water transport vehicles (e.g. water taxi). They carry free, calm surface flow under atmospheric pressure, and can be thought of as artificial rivers. In most cases, a canal has a series of dams and locks that create reservoirs of low speed current flow. These reservoirs are referred to as ''slack water levels'', often just called ''levels''. A canal can be called a ''navigation canal'' when it parallels a natural river and shares part of the latter's discharges and drainage basin, and leverages its resources by building dams and locks to increase and lengthen its stretches of slack water levels while staying in its valley. A canal can cut across a drainage divide atop a ridge, generally requiring an external water source above the highest elevation. The best-known example of such a canal is the Panama Canal. Many ca ...
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History Of The British Canal System
History (derived ) is the systematic study and the documentation of the human activity. The time period of event before the invention of writing systems is considered prehistory. "History" is an umbrella term comprising past events as well as the memory, discovery, collection, organization, presentation, and interpretation of these events. Historians seek knowledge of the past using historical sources such as written documents, oral accounts, art and material artifacts, and ecological markers. History is not complete and still has debatable mysteries. History is also an academic discipline which uses narrative to describe, examine, question, and analyze past events, and investigate their patterns of cause and effect. Historians often debate which narrative best explains an event, as well as the significance of different causes and effects. Historians also debate the nature of history as an end in itself, as well as its usefulness to give perspective on the problems of the p ...
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Canals Of The United Kingdom
The canals of the United Kingdom are a major part of the network of inland waterways in the United Kingdom. They have a varied history, from use for irrigation and transport, through becoming the focus of the Industrial Revolution, to today's role of recreational boating. Despite a period of abandonment, today the canal system in the United Kingdom is again increasing in use, with abandoned and derelict canals being reopened, and the construction of some new routes. Canals in England and Wales are maintained by navigation authorities. The biggest navigation authorities are the Canal & River Trust and the Environment Agency, but other canals are managed by companies, local authorities or charitable trusts. The majority of canals in the United Kingdom can accommodate boats with a length of between and are now used primarily for leisure. There are a number of canals which are far larger than this, including New Junction Canal and the Gloucester and Sharpness Canal, which can acc ...
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Freckleton
Freckleton is a village and civil parish on the Fylde coast in Lancashire, England, to the south of Kirkham and east of the seaside resort of Lytham St. Annes. In 2001 the parish had a population of 6,045, reducing to 6,019 at the 2011 Census. The village is near Warton, with its links to BAE Systems. Warton Aerodrome's runway is partly within Freckleton's boundary. Freckleton has a parish council, and is part of Fylde Borough, and Fylde constituency. History The name of the village appears in the ''Domesday Book'' as "Frecheltun" and is said to derive from 'Farmstead of a man called Frecla', with Old English tun and Nordic personal name. It was one of 62 settlements to be found in the Hundred of "Agemvndrenesse" (Amounderness). Another suggested derivation is from the Anglo-Saxon word for "lusty" or "argumentative".Bevan, E. M. and Ramsbottom, M. (1994), ''A Walk Round Old Freckleton'', Hedgehog Historical Publications, . Freckleton supplied water to the Roman fort a ...
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Tarleton
Tarleton is a village and civil parish in the borough of West Lancashire, Lancashire, England. It situated in the Lancashire mosslands approximately 10 miles north east of Southport, approximately 10 miles south west of Preston, approximately 10 miles west of the (formerly mining and cotton milling) town of Chorley, and approximately 10 miles north of Ormskirk. The village is known for farming due to its rich soil quality. The River Douglas runs northwards to the east of the village, which is locally thought to be where the Vikings camped on the river banks of what is now Tarleton. The parish also includes the village of Mere Brow and the hamlets of Sollom and Holmes. History Tarleton is derived from the Old Norse ''Tharaldr'', a personal name and the Old English ''tun'', a farmstead or enclosure. The township was recorded as Tharilton in 1246 and subsequently Tarleton. Tarleton is mentioned in the Feet of Fines in 1298. A local family with the Tarleton name either was nam ...
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Bank Bridge And Warehouse
A bank is a financial institution that accepts deposits from the public and creates a demand deposit while simultaneously making loans. Lending activities can be directly performed by the bank or indirectly through capital markets. Because banks play an important role in financial stability and the economy of a country, most jurisdictions exercise a high degree of regulation over banks. Most countries have institutionalized a system known as fractional reserve banking, under which banks hold liquid assets equal to only a portion of their current liabilities. In addition to other regulations intended to ensure liquidity, banks are generally subject to minimum capital requirements based on an international set of capital standards, the Basel Accords. Banking in its modern sense evolved in the fourteenth century in the prosperous cities of Renaissance Italy but in many ways functioned as a continuation of ideas and concepts of credit and lending that had their roots in the anc ...
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Act Of Parliament
Acts of Parliament, sometimes referred to as primary legislation, are texts of law passed by the Legislature, legislative body of a jurisdiction (often a parliament or council). In most countries with a parliamentary system of government, acts of parliament begin as a Bill (law), bill, which the legislature votes on. Depending on the structure of government, this text may then be subject to assent or approval from the Executive (government), executive branch. Bills A draft act of parliament is known as a Bill (proposed law), bill. In other words, a bill is a proposed law that needs to be discussed in the parliament before it can become a law. In territories with a Westminster system, most bills that have any possibility of becoming law are introduced into parliament by the government. This will usually happen following the publication of a "white paper", setting out the issues and the way in which the proposed new law is intended to deal with them. A bill may also be introduced in ...
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Slate
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for ex ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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