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Lincolnshire Edge
The Lincoln Cliff or Lincoln Edge is a portion of a major escarpment that runs north–south through the historic divisions of Lindsey and Kesteven in central Lincolnshire and is a prominent landscape feature in a generally flat portion of the county. Towards its northern end, near Scunthorpe, it is sometimes referred to as the Trent Cliff. The name preserves an obsolete sense of the word "cliff", which could historically refer to a hillside as well as a precipitous rock face. Description The scarp is formed by resistant Jurassic age rocks, principally the Lincolnshire Limestone Formation, and is remarkable for its length and straightness. However it is modest in height, rising about 50 metres or less above the surrounding landscape. It runs for over 50 miles from the Leicestershire border near Grantham to the Humber Estuary, and is broken only twice by river gaps at Ancaster and Lincoln, through which the rivers Slea and Witham respectively flow. To the west of the Cliff ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Region
A natural region (landscape unit) is a basic geographic unit. Usually, it is a region which is distinguished by its common natural features of geography, geology, and climate. From the ecological point of view, the naturally occurring flora and fauna of the region are likely to be influenced by its geographical and geological factors, such as soil and water availability, in a significant manner. Thus most natural regions are homogeneous ecosystems. Human impact can be an important factor in the shaping and destiny of a particular natural region. Main terms The concept "natural region" is a large basic geographical unit, like the vast boreal forest region. The term may also be used generically, like in alpine tundra, or specifically to refer to a particular place. The term is particularly useful where there is no corresponding or coterminous official region. The Fens of eastern England, the Thai highlands, and the Pays de Bray in Normandy, are examples of this. Others mig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ermine Street
Ermine Street is a major Roman road in England that ran from London (''Londinium'') to Lincoln ('' Lindum Colonia'') and York ('' Eboracum''). The Old English name was ''Earninga Strǣt'' (1012), named after a tribe called the ''Earningas'', who inhabited a district later known as ''Armingford Hundred'', around Arrington, Cambridgeshire, and Royston, Hertfordshire. "Armingford", and "Arrington" share the same Old English origin. The original Celtic and Roman names for the route remain unknown. It is also known as the Old North Road from London to where it joins the A1 Great North Road near Godmanchester. Course Ermine Street begins at Bishopsgate, where one of the seven gates in the wall surrounding Roman London was located. From here it runs north up Norton Folgate, Shoreditch High Street and Kingsland Road through Stoke Newington (forming Stoke Newington Road and Stoke Newington High Street), Tottenham, Edmonton and eastern Enfield (Ponders End, Enfield Hig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roman Roads In Britain
Roman roads in Britannia were initially designed for military use, created by the Roman army during the nearly four centuries (AD 43–410) that Britannia was a province of the Roman Empire. It is estimated that about of paved trunk roads (surfaced roads running between two towns or cities) were constructed and maintained throughout the province. Most of the known network was complete by 180. The primary function of the network was to allow rapid movement of troops and military supplies, but it subsequently provided vital infrastructure for commerce, trade and the transportation of goods. A considerable number of Roman roads remained in daily use as core trunk roads for centuries after the end of Roman rule in Britain in 410. Some routes are now part of the UK's national road network. Others have been lost or are of archeological and historical interest only. After the Romans departed, systematic construction of paved highways in the United Kingdom did not resume unti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
B1398 Road
B roads are numbered routes in Great Britain of lesser importance than A roads. See the article Great Britain road numbering scheme In Great Britain, there is a numbering scheme used to Categorization, classify and identify all roads. Each road is given a single letter (representing a category) and a subsequent number (between one and four digits). Though this scheme was in ... for the rationale behind the numbers allocated. Zone 1 (3 digits) Zone 1 (4 digits) {{DEFAULTSORT:B Roads in Zone 1 of the Great Britain Numbering Scheme 1 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
A607 Road
The A607 is an A roads in Great Britain, A road in England that starts in Belgrave, Leicester and heads northeastwards through Leicestershire and the town of Grantham, Lincolnshire, terminating at Bracebridge Heath, a village on the outskirts of Lincoln, Lincolnshire, Lincoln. It is a primary route from Thurmaston to the A1 junction at Grantham. Route Leicester to Grantham The road begins in Leicester on the A594 road (Leicester), A594 inner ring road from the ''Burleys Flyover'' intersection, near Thames Tower, as ''Belgrave Gate''. The section of road was the A46 road, A46, and also the A6. At ''Belgrave Circle'' (a grade separated junction – the ''Belgrave Flyover'') it meets ''Abbey Park, Leicester, Abbey Park Road'' (B5327) north of the Murco, Murco Petroleum Ltd ''Flyover Filling Station'' and Leicester College's Abbey Park Campus at ''Painter Street'', with the college's Technology and Engineering Centre to the east, next to the ''Bridle Lane Tavern''. North of Belgrave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic Way
The Jurassic Way is a designated and signed long-distance footpath that connects the Oxfordshire town of Banbury with the Lincolnshire town of Stamford in England. It largely follows an ancient ridgeway traversing Britain; most of its route is in Northamptonshire on the Jurassic limestone ridge in the north of that county. The trail goes near the Oxford and Grand Union canals, past the Great Central Railway's Catesby Tunnel and viaduct, the River Welland, the 82-arch viaduct at Harringworth, and Rockingham Castle. It connects with these long-distance footpaths: *Grand Union Canal Walk, * Hereward Way, * Macmillan Ways, * Midshires Way, * Oxford Canal Walk. The |
River Witham
The River Witham is a river almost entirely in the county of Lincolnshire in the east of England. It rises south of Grantham close to South Witham at , passes through the centre of Grantham (where it may be closely followed using the Riverside Walk through Wyndham Park and Queen Elizabeth Park), passes Lincoln at and at Boston, , flows into The Haven, a tidal arm of The Wash, near RSPB Frampton Marsh. The name "Witham" seems to be extremely old and of unknown origin.; see Old European hydronymy Archaeological and documentary evidence shows the importance of the Witham as a navigable river from the Iron Age onwards. From Roman times it was navigable to Lincoln, from where the Fossdyke was constructed to link it to the River Trent. The mouth of the river moved in 1014 following severe flooding, and Boston became important as a port. From 1142 onwards, sluices were constructed to prevent flooding by the sea, and this culminated in the Great Sluice, which was constructed in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Slea
The River Slea is a tributary of the River Witham, in Lincolnshire, England. In 1872 the river was described as "a never-ending source of pure water", and was a trout river renowned throughout the East coast of England. But in the late 1960s, the Anglian Water Authority took control of the river, and thereafter it became rapidly degraded, due mostly to over-abstraction of water for use in farming. Course The Slea rises near West Willoughby, two miles south-west of Ancaster, at an altitude of 70 metres. The river descends 30 metres in the first 3 km of its course through Ancaster before flowing past a Site of Special Scientific Interest (alongside Sleaford Golf Club) into Sleaford Sleaford is a market town and Civil parishes in England, civil parish in the North Kesteven district of Lincolnshire, England. On the edge of the The Fens, Fenlands, it is north-east of Grantham, west of Boston, Lincolnshire, Boston, and sou .... Through Sleaford it flows above ground i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lincoln, England
Lincoln () is a cathedral city and non-metropolitan district, district in Lincolnshire, England, of which it is the county town. In the 2021 Census, the city's district had a population of 103,813. The 2021 census gave the Lincoln Urban Area, urban area of Lincoln, including Bracebridge Heath, North Hykeham, South Hykeham and Waddington, Lincolnshire, Waddington, a recorded population of 127,540. Roman Britain, Roman ''Lindum Colonia'' developed from an Iron Age settlement of Celtic Britons, Britons on the River Witham, near the Fosse Way road. Over time its name was shortened to Lincoln, after successive settlements, including by Anglo-Saxons and Danes (tribe), Danes. Landmarks include Lincoln Cathedral (English Gothic architecture; for over 200 years the world's tallest building) and the 11th-century Norman architecture, Norman Lincoln Castle. The city hosts the University of Lincoln, Bishop Grosseteste University, Lincoln City F.C. and Lincoln United F.C. Lincoln is the large ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ancaster, Lincolnshire
Ancaster is a village and civil parish in the South Kesteven district of Lincolnshire, England, on the site of a Roman town. The population of the civil parish was 1,317 at the 2001 census, increasing to 1,647 at the 2011 census. The civil parish includes the settlements of Sudbrook and West Willoughby. The village is related to the titles of Duke of Ancaster and Kesteven and Earl of Ancaster, both of which are now extinct. History Ancaster was a Roman town at the junction of the Roman roads of Ermine Street and King Street. During the Romano-British period, the Romans built a roadside settlement on the site of a "Corieltauvi" settlement. It was traditionally thought to have been named "Causennis," although that is now believed to be Saltersford near Grantham. Ancaster lies on Ermine Street, the major Roman road heading north from London. To the north-west of Ancaster is a Roman marching camp, and some 4th-century Roman earthworks are still visible. Excavations have f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humber Estuary
The Humber is a large tidal estuary on the east coast of Northern England. It is formed at Trent Falls, Faxfleet, by the confluence of the tidal rivers River Ouse, Yorkshire, Ouse and River Trent, Trent. From there to the North Sea, it forms part of the boundary between the East Riding of Yorkshire on the north bank and North Lincolnshire on the south bank. Also known as the River Humber, it is tidal its entire length. Below Trent Falls, the Humber passes the junction with the Market Weighton Canal on the north shore, the confluence of the River Ancholme on the south shore; between North Ferriby and South Ferriby and under the Humber Bridge; between Barton-upon-Humber on the south bank and Kingston upon Hull on the north bank (where the River Hull joins), then meets the North Sea between Cleethorpes on the Lincolnshire side and the long and thin headland of Spurn, Spurn Head to the north. Ports on the Humber include the Port of Hull, the Port of Grimsby and the Port of Immin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
