Teddington topographic map

Average elevation: 55 m

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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…

Average elevation: 100 m

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…

Average elevation: 168 m

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Average elevation: 23 m

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…

Average elevation: 37 m

Average elevation: 81 m

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,…

Average elevation: 66 m

Average elevation: 97 m

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…

Average elevation: 138 m

Average elevation: 64 m

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…

Average elevation: 239 m

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The local geology of the Swainswick valley around Sopers Wood, in the south Cotswolds, has been investigated because of the presence of landslides since the work of William Smith in 1799. These are caused by the over-steepened topography downslope of the cap rock formed by the Great Oolite where water egresses…

Average elevation: 131 m

Average elevation: 28 m

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…

Average elevation: 35 m

Average elevation: 145 m

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,…

Average elevation: 82 m

Average elevation: 94 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…

Average elevation: 18 m

Average elevation: 56 m

Average elevation: 120 m

North East England has a Marine west coast climate (generally found along the west coast of middle latitude continents) with narrower temperature ranges than the south of England and sufficient precipitation in all months. Summers and winters are mild rather than extremely hot or cold, due to the strong…

Average elevation: 165 m

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Average elevation: 166 m

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…

Average elevation: 46 m

Average elevation: 122 m

Many settlements developed because of their strategic importance in relation to geographical features, such as river crossings or valleys in ranges of hills. Examples include Axbridge on the River Axe, Castle Cary on the River Cary, North Petherton on the River Parrett, and Ilminster, where there was a…

Average elevation: 96 m

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…

Average elevation: 121 m

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Bicester has expanded rapidly in recent generations due to the town's picturesque historical town centre, garden town layout, independent and high-street shops, restaurants, as well as a rail connection to Oxford. It also boasts imminent connection to Cambridge, as well as rail links to Birmingham and London.…

Average elevation: 77 m

Average elevation: 17 m

Average elevation: 100 m

The East of England region has the lowest elevation range in the UK. Twenty percent of the region is below mean sea level, most of this in North Cambridgeshire, Norfolk and on the Essex Coast. Most of the remaining area is of low elevation, with extensive glacial deposits. The Fens, a large area of reclaimed…

Average elevation: 39 m

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…

Average elevation: 206 m

Average elevation: 80 m

Average elevation: 141 m

The interior of the county consists of a roughly east–west spine of infertile and exposed upland, with a series of granite intrusions, such as Bodmin Moor, which contains the highest land within Cornwall. From east to west, and with approximately descending altitude, these are Bodmin Moor, Hensbarrow north…

Average elevation: 55 m

Average elevation: 73 m

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…

Average elevation: 56 m

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Average elevation: 91 m

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Average elevation: 71 m

Lincolnshire has had a comparatively quiet history, being a rural county which was not heavily industrialised and faced little threat of invasion. In the Roman era Lincoln was a major settlement, called Lindum Colonia. In the fifth century what would become the county was settled by the invading Angles, who…

Average elevation: 26 m

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Cambridgeshire has a maritime temperate climate which is broadly similar to the rest of the United Kingdom, though it is drier than the UK average due to its low altitude and easterly location, the prevailing southwesterly winds having already deposited moisture on higher ground further west. Average winter…

Average elevation: 32 m

The highest elevation in Surrey is Leith Hill near Dorking. It is 295 m (968 ft) above sea level and is the second highest point in southeastern England after Walbury Hill in West Berkshire which is 297 m (974 ft).

Average elevation: 69 m

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Average elevation: 119 m

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Average elevation: 118 m

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Average elevation: 103 m

The source of the river at Teeshead just below Cross Fell is at an elevation of about 2,401 feet (732 m). It flows east-north-east through an area of shake holes through Carboniferous Limestone. Below Viewing Hill, it turns south to the Cow Green Reservoir constructed to store water to be released in dry…

Average elevation: 218 m

Average elevation: 113 m

Average elevation: 21 m

Wakefield's Parish Church was raised to cathedral status in 1888 and after the elevation of Wakefield to diocese, Wakefield Council immediately sought city status and this was granted in July 1888. However the industrial revolution, which changed West and South Yorkshire significantly, led to the growth of…

Average elevation: 172 m

Average elevation: 99 m

Average elevation: 23 m