Carshalton topographic map

Average elevation: 66 m

Average elevation: 96 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: 26 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: 97 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

Average elevation: 94 m

Near Weybridge are the UK headquarters of Sony with SSP Group (situated in Byfleet) and Procter & Gamble (next door to each other on The Heights Business Park near the former Brooklands racing circuit) with Kia Motors UK and Petroleum Geo-Services UK, and Gallaher Group (cigarettes) is to the north, next to…

Average elevation: 69 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

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

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Average elevation: 87 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: 73 m

Average elevation: 66 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

Average elevation: 175 m

The local climate around Luton is differentiated somewhat from much of South East England due to its position in the Chiltern Hills, meaning it tends to be 1–2 degrees Celsius cooler than the surrounding towns – often flights at Luton airport, lying 160 m (525 ft) above sea level, will be suspended when…

Average elevation: 146 m

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Average elevation: 141 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: 23 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

Due to its central location in England and altitude range from 27 metres in the south to 636 metres in the north, Derbyshire contains many species at the edge of their UK distribution ranges. Some species with a predominantly northern British distribution are at the southern limit of their range, whilst others…

Average elevation: 144 m

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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

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

Average elevation: 118 m

Average elevation: 39 m

The highest point at 636 m (2,087 ft) is Kinder Scout, in the Peak District of the southern Pennines in northwest Derbyshire near Glossop. Other hilly areas of 95 to 280 m (312 to 919 ft) in altitude, together with lakes and reservoirs, rise in and around the Charnwood Forest north of Peterborough, Leicester,…

Average elevation: 75 m

Average elevation: 298 m

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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

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: 95 m

Average elevation: 99 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: 116 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: 43 m

Average elevation: 80 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: 153 m

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Average elevation: 88 m

Average elevation: 146 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

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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Average elevation: 52 m

Jane Austen attended Reading Ladies Boarding School, based in the Abbey Gateway, in 1784–1786. 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…

Average elevation: 54 m

Average elevation: 31 m

The western part of the district in the Vale of York borders on and is drained by the River Derwent. The landscape is generally low-lying and flat although minor ridges and glacial moraines provide some variations in topography. Where there are dry sandy soils there are remnants of historic heathlands and…

Average elevation: 30 m

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Average elevation: 31 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: 195 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: 101 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: 31 m

Average elevation: 29 m

Average elevation: 70 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: 70 m

In the Yorkshire and the Humber region, there is a very close relationship between the major topographical areas and the underlying geology. 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 region are Jurassic…

Average elevation: 120 m

Average elevation: 23 m

Average elevation: 7 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

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Average elevation: 55 m