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The Caledonians (/ ˌ k æ l ɪ ˈ d oʊ n i ən z /; Latin: Caledones or Caledonii; Ancient Greek: Καληδῶνες, Kalēdōnes) or the Caledonian Confederacy were a Brittonic-speaking tribal confederacy in what is now Scotland during the Iron Age and Roman eras.
An expandable bathymetric and topographic map of New Caledonia and Vanuatu, formerly the New Hebrides.Click to enlarge. New Caledonia is made up of a main island, the Grande Terre, and several smaller islands, the Belep archipelago to the north of the Grande Terre, the Loyalty Islands to the east of the Grande Terre, the Isle of Pines to the south of the Grande Terre, the Chesterfield Islands ...
New Caledonia has a land area of 18,575 km 2 (7,172 sq mi) divided into three provinces. The North and South Provinces are on the New Caledonian mainland, while the Loyalty Islands Province is a series of four inhabited islands off the east coast of mainland (from north to south: Ouvéa , Lifou , Tiga , and Maré ).
Caledonia (/ ˌ k æ l ɪ ˈ d oʊ n i ə /; Latin: Calēdonia [kaleːˈdonia]) was the Latin name used by the Roman Empire to refer to the part of Scotland that lies north of the River Forth, which includes most of the land area of Scotland. [1] Today, it is used as a romantic or poetic name for all of Scotland. [2]
Below is a list of countries and dependencies in North America by area. [1] The region includes Canada, the Caribbean, Saint Pierre and Miquelon, Central America, Greenland, Mexico, and the United States. Canada is the largest country in North America and the Western Hemisphere.
Maps are also available as part of the Wikimedia Atlas of the World project in the Atlas of Central America. Subcategories This category has the following 4 subcategories, out of 4 total.
1990s CIA political map of the Americas in Lambert azimuthal equal-area projection. The Americas, sometimes collectively called America, [3] [4] [5] known initially as India Nova, [6] are a landmass comprising the totality of North America and South America.
In the Neoproterozoic most of the Earth's landmasses were united in the Rodinia supercontinent.The majority of its bulk consisted of the landmass of Gondwana. [Note 1] Near the end of the Neoproterozoic, during the breakup of this supercontinent, Laurentia [Note 2] and Baltica [Note 3] rifted from the western (Amazonian craton) and northern (African) margins of Gondwana respectively.