Mapa topográfico Barnsley

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In 1919, the borough proposed to expand further and annex the neighbouring borough of Newcastle-under-Lyme and the Wolstanton United Urban District, both to the west of Stoke. This never took place, due to strong objections from Newcastle Corporation. A further attempt was made in 1930, with the promotion of…

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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.

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Farnborough is located in the northeastern corner of the county of Hampshire, near the border with Surrey. The town occupies a valley setting, with the main urban area situated between the River Blackwater to the east and higher ground to the west. The topography gradually rises from the valley floor, reaching…

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The River Plym, which flows off Dartmoor to the north-east, forms a smaller estuary to the east of the city called Cattewater. Plymouth Sound is protected from the sea by the Plymouth Breakwater, in use since 1814. In the Sound is Drake's Island which is seen from Plymouth Hoe, a flat public area on top of…

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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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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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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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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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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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The Hardknott Pass stands at a maximum elevation of 393 m (1,289 ft). The road descends steeply at a gradient of 30% (1 in 3) into the Duddon Valley. At the eastern end of the pass is Cockley Beck farm, built in the 1860s and owned by the National Trust. The route from Hardknott leads eastward towards the…

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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…

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The Catcliffe Glass Cone, part of the previous William Fenney's glassworks, is on Main Street. The centre of the village is dominated by a nine-arch viaduct that was built in 1901 to carry the Sheffield District Railway across the River Rother. Catcliffe Flash, to the south of the village, is a local nature…

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The Pennine climate is generally temperate like that of the rest of England, but the hills have more precipitation, stronger winds and colder weather than the surrounding areas. Higher elevations have a tundra climate. More snow falls on the Pennines than on surrounding lowland areas due to the elevation and…

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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…

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Catcliffe Flash, to the west of the village, is a local nature reserve that is made up of a lake and marshland formed as the elevation of the land beside the River Rother dropped due to coal mining subsidence. To the south-east of the village are three areas of ancient woodland, Treeton Wood, Hail Mary Hill…

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The surface undulates gently from the west to the east, where West Byfleet's land is drained in the parish of Byfleet itself by the River Wey. Soil ranges from sandy acidic soil in the west to more alluvial soil in the east, underlain by a mixture of gravel and clay. Elevations range from 18m Above Ordnance…

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Samuel Lewis reported a township population of 247 in 1831. By the seventh edition of his Topographical Dictionary of England, which was published in 1848, this figure had risen to 724. The population was reported as being 1,040 in 1851. The 1871 census recorded a population of 1,233, spread among 233 houses.

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Alderley Edge is 6 miles (10 km) northwest of Macclesfield and 15 miles (24 km) south of Manchester, at the base of a steep and thickly wooded sandstone escarpment, Alderley Edge, which is the area's chief topographical feature and overlooks the Cheshire Plain.

Altitud media: 92 m