Topografische kaart Lyme Bay

Gemiddelde hoogte: 66 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…

Gemiddelde hoogte: 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…

Gemiddelde hoogte: 168 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…

Gemiddelde hoogte: 69 m

Gemiddelde hoogte: 96 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…

Gemiddelde hoogte: 37 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…

Gemiddelde hoogte: 165 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…

Gemiddelde hoogte: 18 m

Gemiddelde hoogte: 55 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…

Gemiddelde hoogte: 206 m

Gemiddelde hoogte: 77 m

Gemiddelde hoogte: 64 m

Gemiddelde hoogte: 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…

Gemiddelde hoogte: 138 m

Gemiddelde hoogte: 168 m

Gemiddelde hoogte: 113 m

Gemiddelde hoogte: 44 m

Gemiddelde hoogte: 26 m

Gemiddelde hoogte: 115 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).

Gemiddelde hoogte: 69 m

Gemiddelde hoogte: 103 m

Gemiddelde hoogte: 80 m

Gemiddelde hoogte: 225 m

Gemiddelde hoogte: 103 m

Skegness fronts the North Sea. It is located on a low-lying flat region called Lincoln Marsh, which runs along the coast between Skegness and the Humber and separates the coast from the upland Wolds. Much of the parish's elevation is close to sea level, although a narrow band along the seafront is 4–5 m…

Gemiddelde hoogte: 2 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…

Gemiddelde hoogte: 39 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…

Gemiddelde hoogte: 32 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…

Gemiddelde hoogte: 55 m

Gemiddelde hoogte: 223 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…

Gemiddelde hoogte: 56 m

Gemiddelde hoogte: 22 m

Gemiddelde hoogte: 23 m

Gemiddelde hoogte: 71 m

Gemiddelde hoogte: 204 m

Gemiddelde hoogte: 110 m

Neither the thin infertile sands of the High Weald or the wet sticky clays of the Low Weald are suited to intensive arable farming and the topography of the area often increases the difficulties. There are limited areas of fertile greens and which can be used for intensive vegetable growing, as in the valley…

Gemiddelde hoogte: 41 m

Gemiddelde hoogte: 48 m

Gemiddelde hoogte: 31 m

Gemiddelde hoogte: 21 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…

Gemiddelde hoogte: 35 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…

Gemiddelde hoogte: 3 m

Gemiddelde hoogte: 36 m

Gemiddelde hoogte: 122 m

Gemiddelde hoogte: 142 m

Gemiddelde hoogte: 90 m

Gemiddelde hoogte: 86 m

Gemiddelde hoogte: 97 m

Gemiddelde hoogte: 43 m

Gemiddelde hoogte: 159 m

Gemiddelde hoogte: 73 m

Gemiddelde hoogte: 31 m

Gemiddelde hoogte: 28 m

Gemiddelde hoogte: 132 m

Gemiddelde hoogte: 83 m

Gemiddelde hoogte: 50 m

Gemiddelde hoogte: 210 m

Gemiddelde hoogte: 100 m

Gemiddelde hoogte: 128 m

Gemiddelde hoogte: 72 m

Gemiddelde hoogte: 204 m

Gemiddelde hoogte: 325 m

Gemiddelde hoogte: 53 m

Gemiddelde hoogte: 61 m

Gemiddelde hoogte: 58 m

Gemiddelde hoogte: 6 m

Gemiddelde hoogte: 198 m

Gemiddelde hoogte: 40 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…

Gemiddelde hoogte: 46 m

The chalk uplands of the South Downs occupies the coastal strip between Brighton and Eastbourne. There are two river gaps: the Rivers Ouse and Cuckmere. The Seven Sisters, where the Downs meet the sea, are the remnants of dry valleys cut into the chalk; they end at Beachy Head, 530 feet (162 m) above sea…

Gemiddelde hoogte: 44 m

Gemiddelde hoogte: 137 m

Gemiddelde hoogte: 32 m

Gemiddelde hoogte: 37 m

On Cotswold Avenue is the site of a Roman amphitheatre which, while buried, retains its shape in the earthen topography of the small park setting. Cirencester was one of the most substantial cities of Roman-era Britain.

Gemiddelde hoogte: 128 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,…

Gemiddelde hoogte: 66 m

Gemiddelde hoogte: 16 m

Gemiddelde hoogte: 52 m

Gemiddelde hoogte: 4 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…

Gemiddelde hoogte: 144 m

The South Downs National Park's chalk downland is a feature that sets it apart from other national parks in Britain. However, almost a quarter (23%) of the national park consists of a quite different and strongly contrasting physiographic region, the western Weald, whose densely wooded hills and vales are…

Gemiddelde hoogte: 54 m

Gemiddelde hoogte: 23 m

Gemiddelde hoogte: 17 m

Gemiddelde hoogte: 113 m

Gemiddelde hoogte: 141 m

Gemiddelde hoogte: 186 m

Gemiddelde hoogte: 94 m

Gemiddelde hoogte: 15 m

Gemiddelde hoogte: 20 m

Gemiddelde hoogte: 42 m

Gemiddelde hoogte: 4 m

Gemiddelde hoogte: 22 m

Gemiddelde hoogte: 84 m

Gemiddelde hoogte: 59 m

Gemiddelde hoogte: 139 m

Gemiddelde hoogte: 26 m

Gemiddelde hoogte: 71 m

Gemiddelde hoogte: 60 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…

Gemiddelde hoogte: 37 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…

Gemiddelde hoogte: 120 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…

Gemiddelde hoogte: 130 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…

Gemiddelde hoogte: 121 m