Walsall topographic map

Average elevation: 42 m

One of the most distinguishing features of Gateshead is its topography. The land rises 230 feet (70 m) from Gateshead Quays to the town centre and continues rising to a height of 525 feet (160 m) at Queen Elizabeth Hospital in Sheriff Hill. This is in contrast to the flat and low lying Team Valley located on…

Average elevation: 62 m

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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As with the rest of the United Kingdom, Bedford has a maritime climate, with a limited range of temperatures, and generally even rainfall throughout the year. The nearest Met Office weather station to Bedford is Bedford (Thurleigh) airport, about 6.5 miles (10.5 km) north of Bedford town centre at an elevation…

Average elevation: 37 m

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Because of its elevation, Dunstable Downs hosted a station in the shutter telegraph chain which connected the Admiralty in London to its naval ships in the port of Great Yarmouth during the years 1808 to 1814.

Average elevation: 178 m

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Ashdown Forest is an ancient area of open heathland occupying the highest sandy ridge-top of the High Weald Area of Outstanding Natural Beauty. It is situated 30 miles (48 km) south of London in the county East Sussex, England. Rising to an elevation of 732 feet (223 m) above sea level, its heights provide…

Average elevation: 117 m

Putney Heath is around 400 acres (160 hectares) less the nascent A3 road in size and rises to 45 metres (148 ft) above sea level. Because of its elevation, from 1796 to 1816 Putney Heath hosted a station in the shutter telegraph chain, which connected the Admiralty in London to its naval ships in Portsmouth.…

Average elevation: 18 m

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The geology and topography of the village lent itself to urbanisation and domestic industries; primitive weavers' cottages, coal pits and stone quarries were propelled by Bacup's natural supply of water power in the Early Modern period. The adoption of the factory system, which developed into the Industrial…

Average elevation: 337 m

"It consists of a screen of handsome fluted Ionic columns, with three carriage entrance archways, two-foot entrances, a lodge, etc. The extent of the whole frontage is about 107 ft (33 m). The central entrance has a bold projection: the entablature is supported by four columns; and the volutes of the capitals…

Average elevation: 25 m

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Uxbridge lies at a mean elevation of 130 feet (40 m) above mean sea level. Like much of the rest of the UK its climate is generally temperate, with few extremes of temperature or weather.

Average elevation: 44 m

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Average elevation: 61 m

Much of the town was built between about 1850 and 1900; placenames, date stones in terraces, and the vernacular architecture of cellars, local stone, locally-made brick, pipework and tiles and leaded glass, the last now mostly gone, reflect this. It was one of the first places in the world to have steam trams.…

Average elevation: 241 m

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Bradford is located at 53°45′00″N 01°50′00″W / 53.75000°N 1.83333°W / 53.75000; -1.83333 (53.7500, -1.8333)1. Topographically, it is located in the eastern moorland region of the South Pennines.

Average elevation: 167 m

Royston lies on the Barnsley Canal, and on the intersection of the B6132 and B6428 roads, due north of Monk Bretton at an elevation of around 246 feet (75 m) above sea level. The Trans Pennine Trail runs through Royston along the canal bank. The parish is part of the diocese of Leeds.

Average elevation: 74 m

Average elevation: 2 m

The elevation of the City ranges from sea level at the Thames to 21.6 metres (71 ft) at the junction of High Holborn and Chancery Lane. Two small but notable hills are within the historic core, Ludgate Hill to the west and Cornhill to the east. Between them ran the Walbrook, one of the many "lost" rivers or…

Average elevation: 42 m

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Topographically, Halifax is located in the south-eastern corner of the moorland region called the South Pennines. Halifax is situated about 4 miles (6 km) from the M62 motorway, close to Bradford and Huddersfield. The A641 road links the town with Brighouse, Bradford and Huddersfield. The Hebble Brook joins…

Average elevation: 195 m

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The local topography is flat, and in some places, the land lies below sea level, for example in parts of the Fens to the east and to the south of Peterborough. Human settlement in the area began before the Bronze Age, as can be seen at the Flag Fen archaeological site to the east of the current city centre,…

Average elevation: 17 m

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Rawdon Billing, sometimes referred to as Billing Hill, is a tree-topped hill situated in Rawdon, West Yorkshire, England. Reaching an elevation of 231 metres (758 ft), it is a significant landmark in the Aireborough area.

Average elevation: 170 m

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Average elevation: 115 m

Lying in the eastern foothills of the Pennines, there is a significant variation in elevation within the city's built-up area. The district ranges from 1,115 feet (340 m) in the far west on the slopes of Ilkley Moor to about 33 feet (10 m) where the rivers Aire and Wharfe cross the eastern boundary. Land rises…

Average elevation: 94 m

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Mary Russell Mitford lived in Reading for a number of years and then spent the rest of her life just outside the town at Three Mile Cross and Swallowfield. The fictional Belford Regis of her eponymous novel, first published in 1835, is largely based on Reading. Described with topographical accuracy, it is…

Average elevation: 56 m

Swindon has an oceanic climate (Cfb in the Köppen climate classification), like the vast majority of the British Isles, with cool winters and warm summers. The nearest official weather station is RAF Lyneham, about 10 miles (16 km) west southwest of Swindon town centre. The weather station's elevation is 145…

Average elevation: 108 m

Average elevation: 106 m

Kingston upon Hull is on the northern bank of the Humber Estuary. The city centre is west of the River Hull and close to the Humber. The city is built upon alluvial and glacial deposits which overlie chalk rocks but the underlying chalk has no influence on the topography. The land within the city is generally…

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