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Average elevation: 42 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

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

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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…

Average elevation: 81 m

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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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Bishop of Salisbury Hubert Walter was instrumental in the negotiations with Saladin during the Third Crusade, but he spent little time in his diocese prior to his elevation to archbishop of Canterbury. The brothers Herbert and Richard Poore succeeded him and began planning the relocation of the cathedral into…

Average elevation: 96 m

For over 800 years the cathedral and its associated buildings—built on an elevation 68 feet (21 m) above the nearby fens—have visually influenced the city and its surrounding area. Geographer John Jones, writing in 1924, reports that "from the roof of King's Chapel in Cambridge, on a clear day, Ely can be…

Average elevation: 13 m

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…

Average elevation: 761 m

Average elevation: 85 m

Billinge Hill is in the Metropolitan Borough of St Helens in North West England. With a maximum elevation of 179 m (587 ft), it is the highest point of Merseyside. It lies in Billinge, within the historic county boundaries of Lancashire, and it is one of the 176 hills graded as a Marilyn in England.

Average elevation: 115 m

Average elevation: 145 m

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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Red Tarn, a classic corrie tarn, is a high-elevation tarn with low nutrient levels and poor in the number of species it supports. Characteristic vegetation zones include a water-starwort (Callitriche) in shallower areas and the alga Nitella flexilis in deeper water and around the inlet. Other species include a…

Average elevation: 680 m

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In the 1848 edition of 'A Topographical Dictionary of England', Samuel Lewis (the editor) wrote:- "the lands are in meadow and pasture, with a small portion of arable; the scenery is bold and romantic. In the quarries of the district are found vegetable fossils, especially firs and other mountain trees. The…

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Scafell Pike (/ˈskɔːfɛl paɪk/) is the highest and the most prominent mountain in England, at an elevation of 978 metres (3,209 ft) above sea level. It is located in the Lake District National Park, in Cumbria, and is part of the Southern Fells and the Scafell massif.

Average elevation: 679 m

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Overlying the Beacon Hill Formation, but found a little further down the hillside to the south, are the Bradgate Formation beds, the most notable of which is the Sliding Stone Slump Breccia rocks. Forming a line of crags below Old John, these are laminated mudstones, with layers of sandstone, mainly of…

Average elevation: 126 m

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By road, Portsmouth lies 73.5 miles (118.3 km) from Central London, 49.5 miles (79.7 km) west of Brighton, and 22.3 miles (35.9 km) east of Southampton. Portsmouth is situated primarily on Portsea Island and is the United Kingdom's only island city, although parts of it have expanded onto the mainland. Gosport…

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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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