Mapa topográfico Bromborough

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Sheffield nestles on the eastern foothills of the Pennines and is sculpted by a dramatic hill-and-valley system formed where five rivers — the Don, Sheaf, Rivelin, Loxley and Porter — converge, producing steep-sided valleys and gritstone ridgelines with much of the urban area built directly onto hillsides…

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Kent was also the location of the largest number of art schools in the country during the nineteenth century, estimated by the art historian David Haste, to approach two hundred. This is believed to be the result of Kent being a front line county during the Napoleonic Wars. At this time, before the invention…

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The Lake District is a roughly circular upland massif, deeply dissected by a broadly radial pattern of major valleys which are largely the result of repeated glaciations over the last 2 million years. The apparent radial pattern is not from a central dome, but from an axial watershed extending from St Bees…

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Birmingham is a snowy city relative to other large UK conurbations, due to its inland location and comparatively high elevation. Between 1961 and 1990 Birmingham Airport averaged 13.0 days of snow lying annually, compared to 5.33 at London Heathrow. Snow showers often pass through the city via the Cheshire gap…

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The city, like most of the UK, has a maritime climate highly influenced by the Gulf Stream. Located in the driest region of Britain, Cambridge's rainfall averages around 570 mm (22.44 in) per year, around half the national average, with some years occasionally falling into the semi-arid (under 500 mm (19.69…

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Near Weybridge are the UK headquarters of Sony with SSP Group (situated in Byfleet) and Procter & Gamble (next door to each other on The Heights Business Park near the former Brooklands racing circuit) with Kia Motors UK and Petroleum Geo-Services UK, and Gallaher Group (cigarettes) is to the north, next to…

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Rainfall tends to be associated with Atlantic depressions or with convection. In summer, convection caused by solar surface heating sometimes forms shower clouds and a large proportion of rainfall falls from showers and thunderstorms at this time of year. The wettest months are November and December and on the…

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Lincoln lies 157 mi (253 km) north of London, at an altitude of 67 ft (20.4 m) by the River Witham up to 246 ft (75.0 m) on Castle Hill. It fills a gap in the Lincoln Cliff escarpment, which runs north and south through central Lincolnshire, with altitudes up to 200 feet (61 metres). The city lies on the River…

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The west of the county lies on more resistant Cretaceous chalk. This chalk is responsible for a sweeping tract of largely downland landscapes that stretches from Dorset in the south west to Dover in the south east and north through East Anglia to the Yorkshire Wolds. The chalk is less easily eroded so forms…

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The city of Exeter was established on the eastern bank of the River Exe on a ridge of land backed by a steep hill. It is at this point that the Exe, having just been joined by the River Creedy, opens onto a wide flood plain and estuary which results in quite common flooding. Historically this was the lowest…

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As part of the United Kingdom, the North York Moors area generally has warm summers and relatively mild winters. Weather conditions vary from day to day as well as from season to season. The latitude of the area means that it is influenced by predominantly westerly winds with depressions and their associated…

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The western part of the district in the Vale of York borders on and is drained by the River Derwent. The landscape is generally low-lying and flat although minor ridges and glacial moraines provide some variations in topography. Where there are dry sandy soils there are remnants of historic heathlands and…

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In Yorkshire there is a very close relationship between the major topographical areas and the geological period in which they were formed. The Pennine chain of hills in the west is of Carboniferous origin. The central vale is Permo-Triassic. The North York Moors in the north-east of the county are Jurassic in…

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Bath is in the Avon Valley and is surrounded by limestone hills as it is near the southern edge of the Cotswolds, a designated Area of Outstanding Natural Beauty, and the limestone Mendip Hills rise around 7 miles (11 km) south of the city. The hills that surround and make up the city have a maximum altitude…

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Little of note happened at Dawlish until the end of the 18th century, when seaside locations on the south coast started to become popular with the wealthy, mainly caused by George III making Weymouth in Dorset his summer holiday residence from 1789. In May 1795, the antiquarian and topographer John Swete spent…

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London's topography is characterized by a gently rolling terrain shaped by the River Thames and its tributaries. The city lies within the London Basin, a natural depression bordered by higher grounds such as the North Downs to the south and the Chiltern Hills to the northwest. The Thames flows west to east,…

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A distinctive feature of the catchment is the marked variation in the topography and character of the landscape, which varies from the upland moorland headwaters of the Dark Peak, where the highest point of the catchment is the Kinder Scout plateau at 634 metres (2,080 ft); through to the intensively farmed…

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Elevations are higher in the north and west, reaching more than 800 feet (240 m) in the Chilterns near Tring. The county centres on the headwaters and upper valleys of the rivers Lea and the Colne; both flow south, and each is accompanied by a canal. Hertfordshire's undeveloped land is mainly agricultural,…

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An Iron Age shrine in the north of Hayling Island was later developed into a Roman temple in the 1st century BC and was first recorded in Richard Scott's Topographical and Historical Account of Hayling Island (1826). The site was dug between 1897 and 1907 and again from 1976 to 1978. The remains are now buried…

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As with the rest of the British Isles, Northampton experiences a maritime climate with cool summers and mild winters. The official Met Office weather station for Northampton is the Moulton Park Weather Station at the University of Northampton. Situated at an elevation of around 130 m (427 ft) above sea level…

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Tideswell is a village and civil parish in the Peak District of Derbyshire, England. It lies 6 miles (9.7 km) east of Buxton on the B6049, in a wide valley on a limestone plateau, at an altitude of 1,000 feet (300 m) above sea level, and is within the District of Derbyshire Dales. The population (including…

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Skegness fronts the North Sea. It is located on a low-lying flat region called Lincoln Marsh, which runs along the coast between Skegness and the Humber and separates the coast from the upland Wolds. Much of the parish's elevation is close to sea level, although a narrow band along the seafront is 4–5 m…

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Elevations range between 30 and 70 metres above sea level except higher in about 5% of the borough. The highest is an escarpment containing parts of the rural and wooded northern area, the hinterland of three Thames-side villages, facing the 30-mile long Chilterns AONB, west and north. A geological part of…

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Due to its central location in England and altitude range from 27 metres in the south to 636 metres in the north, Derbyshire contains many species at the edge of their UK distribution ranges. Some species with a predominantly northern British distribution are at the southern limit of their range, whilst others…

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A study published by Princeton University and McGill University, in 2020, concluded that the Manhood Peninsula is at particularly high risk of flooding as its topography is less than 5 metres (16 ft) above the current mean sea level and that by 2100 Selsey will be subject to permanent inundation.

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During the 12th century, the planned town of Ludlow was formed, in stages, the town providing a useful source of income for successive Marcher Lords, based on rents, fines, and tolls. They developed the town on a regular grid pattern, although this was adapted somewhat to match the local topography, from the…

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There is debate as to whether the stretch of water between Newby Bridge and Lakeside at the southern end of the lake should be considered part of Windermere, or a navigable stretch of the River Leven. This affects the stated length of the lake, which is 11.23 miles (18.07 km) long if measured from the bridge…

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