Tinkersick
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Tinkersick
Tinkersick or Tinker Sick is a stream east of Chesterfield, near Brimington in Derbyshire. The stream is an offshoot of the Chesterfield Canal. A breach in the Chesterfield canal in March 2007, caused by the collapse of a culvert carrying the Tinkersick under the canal, forced temporary closure of all but the top pound above Tapton Lock for about six weeks. Colliery Tinkersick Colliery operated until the mid 20th Century, being purchased by the Chesterfield Coal Co. Ltd in 1930 from the Hall Brothers. See also * List of rivers of England This is a list of rivers of England, organised geographically and taken anti-clockwise around the English coast where the various rivers discharge into the surrounding seas, from the Solway Firth on the Scottish border to the Welsh Dee on the W ... References Tourist attractions in Derbyshire Rivers of Derbyshire Rivers and valleys of the Peak District High Peak, Derbyshire {{England-river-stub ...
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Chesterfield Canal
The Chesterfield Canal is a narrow canal in the East Midlands of England and it is known locally as 'Cuckoo Dyke'. It was one of the last of the canals designed by James Brindley, who died while it was being constructed. It was opened in 1777 and ran for from the River Trent at West Stockwith, Nottinghamshire to Chesterfield, Derbyshire, passing through the Norwood Tunnel at Kiveton Park, at the time one of the longest tunnels on the British canal system. The canal was built to export coal, limestone, and lead from Derbyshire, iron from Chesterfield, and corn, deals, timber, groceries and general merchandise into Derbyshire. The stone for the Palace of Westminster was quarried in North Anston, Rotherham, and transported via the canal. It was reasonably profitable, paying dividends from 1789, and with the coming of the railways, some of the proprietors formed a railway company. It became part of the Manchester, Sheffield and Lincolnshire Railway company, and although there w ...
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Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long, large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known, amongst others, as brook, creek, rivulet, rill, run, tributary, feeder, freshet, narrow river, and streamlet. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of pr ...
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Chesterfield, Derbyshire
Chesterfield is a market town, market and industrial town in the county of Derbyshire, England. It is north of Derby and south of Sheffield at the confluence of the River Rother, South Yorkshire, Rivers Rother and River Hipper, Hipper. In 2011, the built-up-area subdivision had a population of 88,483, making it the second-largest settlement in Derbyshire, after Derby. The wider Borough of Chesterfield had a population of 103,569 in the 2021 Census. In 2021, the town itself had a population of 76,402. It has been traced to a transitory Ancient Roman architecture, Roman fort dated to approximately AD 80-100. The name of the later Anglo-Saxons, Anglo-Saxon village comes from the Old English ''ceaster'' (Roman fort) and ''feld'' (pasture). It has a sizeable street market three days a week. The town sits on an old coalfield, but little visual evidence of mining remains since the closure of the final town centre mine nicknamed “The Green Room”. The main landmark is the crooked sp ...
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Brimington
Brimington is a large village and civil parish in the Borough of Chesterfield in Derbyshire, England. The population of the parish taken at the 2011 census was 8,788. The town of Staveley is to the east, and Hollingwood is nearby. The parish includes Brimington Common along the Calow Road, and New Brimington, a late 19th-century extension towards the Staveley Iron Works. History The route of Icknield Street, a Roman road, passes close to the village. Brimington appears in the Domesday Book of 1086 as ''Brimintune''. At that time, the manor was the property of King William I and the population was recorded as being sixteen villagers, two smallholders and one slave. Although there was a church in the village in the medieval period, it was a chapel of ease with the parish church being Chesterfield. In the autumn of 1603, there was an outbreak of bubonic plague in Brimington; the victims were buried in the village but were recorded in the parish register at Chesterfield. ...
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Derbyshire
Derbyshire ( ) is a ceremonial county in the East Midlands of England. It borders Greater Manchester, West Yorkshire, and South Yorkshire to the north, Nottinghamshire to the east, Leicestershire to the south-east, Staffordshire to the south and west, and Cheshire to the west. Derby is the largest settlement, and Matlock is the county town. The county has an area of and a population of 1,053,316. The east of the county is more densely populated than the west, and contains the county's largest settlements: Derby (261,400), Chesterfield (88,483), and Swadlincote (45,000). For local government purposes Derbyshire comprises a non-metropolitan county, with eight districts, and the Derby unitary authority area. The East Midlands Combined County Authority includes Derbyshire County Council and Derby City Council. The north and centre of Derbyshire are hilly and contain the southern end of the Pennines, most of which are part of the Peak District National Park. They include Kinde ...
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List Of Rivers Of England
This is a list of rivers of England, organised geographically and taken anti-clockwise around the English coast where the various rivers discharge into the surrounding seas, from the Solway Firth on the Scottish border to the Welsh Dee on the Welsh border, and again from the Wye on the Welsh border anti-clockwise to the Tweed on the Scottish border. Tributaries are listed down the page in an upstream direction, i.e. the first tributary listed is closest to the sea, and tributaries of tributaries are treated similarly. Thus, in the first catchment below, the River Sark is the lowermost tributary of the Border Esk and the Hether Burn is the lowermost tributary of the River Lyne. The main stem (or principal) river of a catchment is labelled as (MS), left-bank tributaries are indicated by (L), right-bank tributaries by (R). Note that in general usage, the 'left (or right) bank of a river' refers to the left (or right) hand bank, as seen when looking downstream. Where a named riv ...
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Tourist Attractions In Derbyshire
Tourism is travel for pleasure, and the commercial activity of providing and supporting such travel. UN Tourism defines tourism more generally, in terms which go "beyond the common perception of tourism as being limited to holiday activity only", as people "travelling to and staying in places outside their usual environment for not more than one consecutive year for leisure and not less than 24 hours, business and other purposes". Tourism can be domestic (within the traveller's own country) or international. International tourism has both incoming and outgoing implications on a country's balance of payments. Between the second half of 2008 and the end of 2009, tourism numbers declined due to a severe economic slowdown (see Great Recession) and the outbreak of the 2009 H1N1 influenza virus. These numbers, however, recovered until the COVID-19 pandemic put an abrupt end to the growth. The United Nations World Tourism Organization has estimated that global international tourist a ...
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Rivers Of Derbyshire
A river is a natural stream of fresh water that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their banks and flood the surrounding area, spreading nutrients to the surrounding area. Sediment or alluvium carried by rivers shapes the landscape aro ...
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