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Crossens Pool
Crossens is the northernmost district of the town of Southport, Merseyside, England. Historically part of the ancient parish of North Meols and entirely in Lancashire, most of Crossens was transferred to Merseyside on 1 April 1974, when local government boundaries were reorganised nationally. Part of northern Crossens, known as Fiddlers Ferry, is in West Lancashire. Formerly, the village was a detached settlement lying on the western edge of Martin Mere, but after the drainage of the Mere and the expansion of Southport, it had become absorbed into the town's conurbation. History Formerly ''Crossenes'' or ''Crosnes'', meaning a “ness” or headland with a cross. The cross was possibly a guide for shipping or people crossing the Ribble Estuary from Freckleton (near Lytham). A hospice or lodging house was sited in Crossens where travellers could rest after making the crossing. It is also believed to be the point at which 2,000 horsemen from a retreating Royalist force crossed th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metropolitan Borough Of Sefton
The Metropolitan Borough of Sefton is a metropolitan borough of Merseyside, England. It was formed on Local Government Act 1972, 1 April 1974, by the amalgamation of the county boroughs of Bootle and Southport, the municipal borough of Crosby, Merseyside, Crosby, the Urban district (Great Britain and Ireland), urban districts of Formby and Litherland, and part of West Lancashire Rural District. It consists of a Sefton Coast, coastal strip of land on the Irish Sea which extends from Southport in the north to Bootle in the south, and an inland part to Maghull in the south-east, bounded by the city of Liverpool to the south, the Metropolitan Borough of Knowsley to the south-east, and West Lancashire to the east. It is named after Sefton, Sefton, Sefton, near Maghull. When the borough was created, a name was sought that would not unduly identify the borough with any of its constituent parts, particularly the former county boroughs of Bootle and Southport. The area had strong links ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Industrial Revolution
The Industrial Revolution was the transition to new manufacturing processes in Great Britain, continental Europe, and the United States, that occurred during the period from around 1760 to about 1820–1840. This transition included going from hand production methods to machines, new chemical manufacturing and iron production processes, the increasing use of steam power and water power, the development of machine tools and the rise of the mechanized factory system. Output greatly increased, and a result was an unprecedented rise in population and in the rate of population growth. Textiles were the dominant industry of the Industrial Revolution in terms of employment, value of output and capital invested. The textile industry was also the first to use modern production methods. The Industrial Revolution began in Great Britain, and many of the technological and architectural innovations were of British origin. By the mid-18th century, Britain was the world's leadi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cumfybus
Cumfybus is a bus company based in Southport, Merseyside. Its operations were small scale throughout the 1990s, but it has expanded significantly since its incorporation as a limited company in 2002, and in 2010 had a fleet of nearly 100 buses. History Cumfybus was founded in 1986 by Marshall and Patricia Vickers when a minibus was purchased to service nursing homes in Southport. before starting to bid for contracts tendered by Merseytravel. As time went on, depots were opened in Aintree, Southport, Kirkby and on the Wirral (initially at Birkenhead before moving to Moreton in 2012). Cumfybus had a short venture outside of Merseyside when it operated services around Blackpool and the Fylde area in 2010. In late 2012 the company moved all operations to a central location at Aintree. The yard at Southport was kept for additional storage and/or maintenance. The Fylde, Kirkby and Wirral depots were closed. In July 2013 Cumfybus opened a depot in Bolton following it being awarde ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stagecoach North West
Stagecoach North West was a major operator of bus services in North West England. It was a subsidiary of the Stagecoach Group, and had its origins in the purchase of Cumberland in 1987 and Ribble Motor Services in 1988 from the National Bus Company. The head office of Stagecoach North West was in Carlisle. Although the cities of Liverpool and Manchester are in the North West of England, Stagecoach Manchester and Stagecoach Merseyside were run as separate divisions. Stagecoach North West was split in September 2011 into Stagecoach Merseyside & South Lancashire and Stagecoach Cumbria & North Lancashire, with the former incorporating Chorley and Preston depots and the Gillmoss depot of Stagecoach Merseyside, and the latter incorporating Barrow, Carlisle, Kendal and Workington depots. After the split, the company, Stagecoach North West Ltd, continues to exist with the trading name Stagecoach Cumbria & North Lancashire. History Stagecoach North West operated services in Carlisle, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arriva North West
Arriva North WestCompanies House extract company no 1990871 Arriva Merseyside Limited formerly Merseyside Transport LimitedCompanies House extract company no 523376 Arriva North West Limited formerly North Western Road Car Company Limited is a major bus operator running services in primarily in the area and the county of |
Crossens Railway Station
Crossens railway station was a railway station serving Crossens, a suburb of Southport, Sefton, Merseyside, England. History Located on the Lancashire and Yorkshire Railway main line between and , it was opened to passengers by the West Lancashire Railwayin 1878. In April 1904 it became the last electrified station on the Lancashire and Yorkshire Railway's suburban lines from Liverpool Exchange railway station Liverpool Exchange railway station was a railway station located in the city centre of Liverpool, England. Of the four terminal stations in Liverpool's city centre, Exchange station was the only station not accessed via a tunnel. The station w ..., forming a terminus of the Southport - Crossens electric branch. Services ended on 6 September 1964 with the closure of the Southport to Preston line.Cadwallader, Jonathan and Jenkins, Martin (2010) ''Merseyside Electrics'', Ian Allan Publishing, (p34 has colour photo of Crossens station looking north, with electric trai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Lancashire Railway
The West Lancashire Railway (WLR) ran northeast from Southport to Preston in northwest England. History Construction was started by Samuel Swire the Mayor of Southport, on 19 April 1873. It opened on 15 September 1882. A branch was constructed from Penwortham to the Blackburn line at Whitehouse Junction allowing direct services from East Lancashire Railway to Southport. In 1881 a further branch was constructed from east of Hesketh Bank station southwards to Tarleton Lock on the Rufford Branch of the Leeds and Liverpool Canal by the River Douglas. This was mainly intended for goods, but a passenger service did run on the branch until 1912/3. The branch closed completely in 1930. Expansion, bankruptcy and take-over It also sponsored the Liverpool, Southport and Preston Junction Railway, opened in 1887 to provide greater access to Liverpool (in competition with its rival the Lancashire and Yorkshire Railway) and in an attempt to forge a commercial alliance with the Manchester ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Erratics
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geologists
A geologist is a scientist who studies the solid, liquid, and gaseous matter that constitutes Earth and other terrestrial planets, as well as the processes that shape them. Geologists usually study geology, earth science, or geophysics, although backgrounds in physics, chemistry, biology, and other sciences are also useful. Field research (field work) is an important component of geology, although many subdisciplines incorporate laboratory and digitalized work. Geologists can be classified in a larger group of scientists, called geoscientists. Geologists work in the energy and mining sectors searching for natural resources such as petroleum, natural gas, precious and base metals. They are also in the forefront of preventing and mitigating damage from natural hazards and disasters such as earthquakes, volcanoes, tsunamis and landslides. Their studies are used to warn the general public of the occurrence of these events. Geologists are also important contributors to climate chan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dumfries
Dumfries ( ; sco, Dumfries; from gd, Dùn Phris ) is a market town and former royal burgh within the Dumfries and Galloway council area of Scotland. It is located near the mouth of the River Nith into the Solway Firth about by road from the Anglo-Scottish border and just away from Cumbria by air. Dumfries is the county town of the historic county of Dumfriesshire. Before becoming King of Scots, Robert the Bruce killed his rival the Red Comyn at Greyfriars Kirk in the town on 10 February 1306. The Young Pretender had his headquarters here during a 3-day sojourn in Dumfries towards the end of 1745. During the Second World War, the bulk of the Norwegian Army during their years in exile in Britain consisted of a brigade in Dumfries. Dumfries is nicknamed ''Queen of the South''. This is also the name of the town's professional football club. People from Dumfries are known colloquially in Scots language as ''Doonhamers''. Toponymy There are a number of theories on the etymo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
