Mapa topográfico Thames Valley

Altitud media: 42 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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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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St Albans was an ancient borough created following the dissolution of the monastery in 1539. It consisted of the ancient parish of St Albans (also known as the Abbey parish) and parts of St Michael and St Peter. The municipal corporation was reformed by the Municipal Corporations Act 1835 and the boundary was…

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St. Lawrence's C of E Church, stands in the middle of the town. It has a 12th-century Norman transitional ground plan and foundation, probably laid over a Saxon 10th century stone building. Its ecclesiastical heritage may well relate back to Roman times as St Lawrence was patron saint of the Roman legions. The…

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The fell has a summit plateau which consist of many heather-covered hummocks, drystone walls and clumps of trees. Well-known Lake District writer Alfred Wainwright credits Grange Fell as a single fell with three main summits, namely Brund Fell, King's How and Ether Knott. The lesser known Ether Knott is now…

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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…

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The current town was founded in 1245 and developed as a fishing port. The name South Shields developed from the 'Schele' or 'Shield', which was a small dwelling used by fishermen. Another industry that was introduced, was that of salt-panning, later expanded upon in the 15th century, polluting the air and…

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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,…

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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…

Altitud media: 94 m

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.

Altitud media: 167 m

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By road, Portsmouth lies 73.5 miles (118.3 km) from Central London, 49.5 miles (79.7 km) west of Brighton, and 22.3 miles (35.9 km) east of Southampton. Portsmouth is situated primarily on Portsea Island and is the United Kingdom's only island city, although parts of it have expanded onto the mainland. Gosport…

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The town centre lies just below 33 ft (10m) above sea level. South of the town centre, rising from Richmond Bridge to an elevation of 165 ft (50m), is Richmond Hill. Just beyond the summit of Richmond Hill is Richmond Park, an area of 2,360 acres (9.55 km2; 3.7 sq mi) of wild heath and woodland originally…

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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…

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