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According to German linguist Stefan Zimmer, Caledonia is derived from the tribal name Caledones (a Latinization of a Brittonic nominative plural n-stem Calēdones or Calīdones, from earlier *Kalē=Black River=don/Danue Goddess[i]oi), which he etymologises as perhaps 'possessing hard feet' ("alluding to standfastness or endurance"), from the Proto-Celtic roots *kal-'hard' and *pēd-'foot', [3 ...
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]
Caledonia is a Roman name of Celtic origin for most of the area that has become Scotland.. Caledonia may also refer to: . Caledonia, an old name for Scotland; Caledonians, also known as Caledonii or Caledonia Confederacy, name given by historians to the Iron Age indigenous people of Scotland
A majority of the Caldoche are of French descent and have their origins as free colonial or penal settlers, with smaller but significant numbers of Caldoche being of Italian, German, British, Polish, Belgian and Irish heritage. French is the main language spoken by the Caldoche. New Caledonia was used as a penal colony from
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As it represented the power of the clan Chiefs of Kanaks over their subjects, it was adopted as part of the flag of the Kanaks by the organization leading the independent movement in New Caledonia. The Grand Huts also known as grande case (chief's hut) are decorated with a flèche faîtière as a filial, representing the ancestral spirits ...
Iaai (Iaai pronunciation: in English as / ˈ j aɪ / Y-EYE) is a language of Ouvéa Island (New Caledonia). It shares the island of Ouvéa with Fagauvea, a Polynesian outlier language. Iaai is the sixth-most-spoken language of New Caledonia, with 4078 speakers as of 2009. [2] It is taught in schools in an effort to preserve it.
The Caledonian Wilson cycle commenced with the continental break-up of Rodinia [17] and the opening of the Iapetus ocean about 616–583 Ma ago. [18] [19] [20] The Iapetus was at its widest in the Late Cambrian–Early Ordovician [21] [1] before it began to close by subduction of Iapetus oceanic crust along the Gondawanan and Laurentian margins starting between 500 and 488 Ma ago.