Bloxwich topographic map

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

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

Average elevation: 55 m

Average elevation: 96 m

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Average elevation: 66 m

Average elevation: 56 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: 87 m

Average elevation: 28 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

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

Average elevation: 97 m

Average elevation: 23 m

Average elevation: 17 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: 8 m

Average elevation: 103 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: 141 m

Average elevation: 31 m

Average elevation: 64 m

Average elevation: 103 m

Average elevation: 21 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: 22 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

All of the county is drained by the Thames. Berkshire divides into two topological (and associated geological) sections: east and west of Reading. North-east Berkshire has the low calciferous (limestone) m-shaped bends of the Thames south of which is a broader, clayey, gravelly former watery plain or belt from…

Average elevation: 100 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

Average elevation: 12 m

Average elevation: 151 m

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Average elevation: 118 m

Putney Heath is around 160 hectares (400 acres) in size and sits at approximately 45 metres (148 feet) 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. This was…

Average elevation: 35 m

Average elevation: 113 m

Average elevation: 43 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

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

Average elevation: 73 m

Average elevation: 223 m

Average elevation: 95 m

Average elevation: 81 m

The cathedral city of Ely is 24 miles (39 km) east-southeast across the Fens and the university city of Cambridge is 30 miles (48 km) to the southeast. The local topography is flat, and in places, the land lies below sea level.

Average elevation: 17 m

Average elevation: 87 m

Average elevation: 20 m

Average elevation: 122 m

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…

Average elevation: 168 m

Average elevation: 115 m

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…

Average elevation: 66 m

Average elevation: 39 m

Average elevation: 48 m

Average elevation: 111 m

A large part of the north-west of the county, around Coalville, forms part of the new National Forest area extending into Derbyshire and Staffordshire. The highest point of the county is Bardon Hill at 278 m (912 ft), which is also a Marilyn; with other hilly/upland areas of around 150–200 metres (490–660…

Average elevation: 97 m

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

Average elevation: 159 m

Average elevation: 225 m

The area was historically part of the county of Middlesex. Whilst an important centre of royal authority from Saxon times, Westminster was not formally incorporated as a borough for local government purposes until 1900. However, it was declared a city in 1540 on the elevation of Westminster Abbey to being a…

Average elevation: 23 m

Average elevation: 52 m

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Average elevation: 46 m

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Average elevation: 13 m

Average elevation: 68 m

Average elevation: 118 m

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…

Average elevation: 130 m

Average elevation: 298 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: 119 m

Portsmouth is 73.5 miles (118.3 km) by road from central London, 49.5 miles (79.7 km) west of Brighton, and 22.3 miles (35.9 km) east of Southampton. It is located primarily on Portsea Island and is the United Kingdom's only island city, although the city has expanded to the mainland. Gosport is a borough to…

Average elevation: 7 m

Average elevation: 63 m

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Average elevation: 35 m

Average elevation: 59 m

Average elevation: 81 m

Ipswich experiences an oceanic climate, like the rest of the British Isles, with a narrow range of temperature and rainfall spread evenly throughout the year. One of the two nearest for which data is available is East Bergholt, about 7 miles (11 km) south west of the town centre and at a similar elevation, and…

Average elevation: 29 m

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…

Average elevation: 100 m

Average elevation: 26 m

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Average elevation: 41 m

Average elevation: 42 m

Average elevation: 16 m

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Average elevation: 37 m

Average elevation: 163 m

Average elevation: 35 m

The new chapel, with its elegant slender tower, was opened on 16 October 1862; the building works had cost around £800. The striking terracotta relief panel, The City of Refuge, on the front elevation of the chapel, was created by the renowned Doulton & Co artist George Tinworth and is signed with his…

Average elevation: 25 m

Average elevation: 276 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…

Average elevation: 3 m

Average elevation: 138 m

Average elevation: 26 m