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By the eighteenth century, the name English Channel was in common usage in England. Following the Acts of Union 1707, this was replaced in official maps and documents with British Channel or British Sea for much of the next century. However, the term English Channel remained popular and was finally in official usage by the nineteenth century. [11]
This is a list of rivers of England, organised geographically and taken anti-clockwise around the English coast where the various rivers discharge into the surrounding seas, from the Solway Firth on the Scottish border to the Welsh Dee on the Welsh border, and again from the Wye on the Welsh border anti-clockwise to the Tweed on the Scottish border.
The earliest cities (Latin: civitas) in Britain were the fortified settlements organised by the Romans as capitals of the Celtic tribes under Roman rule.The British clerics of the early Middle Ages later preserved a traditional list of the "28 Cities" (Old Welsh: cair) which was mentioned in De Excidio Britanniae [c] and Historia Brittonum.
Dymaxion map of the world with the 30 largest countries and territories by area. This is a list of the world's countries and their dependencies, ranked by total area, including land and water. This list includes entries that are not limited to those in the ISO 3166-1 standard, which covers sovereign states and dependent territories.
The Channel Islands [note 1] are an archipelago in the English Channel, off the French coast of Normandy.They are divided into two Crown Dependencies: the Bailiwick of Jersey, which is the largest of the islands; and the Bailiwick of Guernsey, consisting of Guernsey, Alderney, Sark, Herm and some smaller islands.
List of cities in the Pitcairn Islands - Pitcairn, Henderson, Ducie, and Oeno Islands (UK overseas territory) List of cities in Poland - Republic of Poland; List of cities in Portugal - Portuguese Republic; List of cities in Puerto Rico - Commonwealth of Puerto Rico (US overseas commonwealth)
Map showing hypothetical extent of Doggerland from Weichselian glaciation until the current situation. Paleogeographers studying the Quaternary period have suggested that 600,000 years ago, although the Channel and the North Sea were flooded, the Weald-Artois ridge remained as a land bridge between Britain and Continental Europe, [1] allowing people, plants and animals to cross. [2]
Though pitted by troughs and rivers, the English Channel was almost mainly land at the height of the last ice age. [6] The predominant geology of both and of the seafloor is chalk. Although somewhat resistant to erosion, erosion of both coasts has created the famous white cliffs of Dover in the UK and the Cap Blanc Nez in France.