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Qu'est-ce (qui) est Caledonian orogeny - définition
Caledonian orogeny
![geological history]], the [[Atlantic Ocean]] opened and the different parts of the orogenic belt moved apart.<ref>Reconstruction based on Matte (2001); Stampfli ''et al.'' (2002); Torsvik ''et al.'' (1996) and Ziegler (1990)</ref> See also [[Iapetus Suture]] and [[Trans-European Suture Zone]].](https://commons.wikimedia.org/wiki/Special:FilePath/Caledonides EN.svg?width=200 "geological history]], the [[Atlantic Ocean]] opened and the different parts of the orogenic belt moved apart.<ref>Reconstruction based on Matte (2001); Stampfli ''et al.'' (2002); Torsvik ''et al.'' (1996) and Ziegler (1990)</ref> See also [[Iapetus Suture]] and [[Trans-European Suture Zone]].")
![Geological map of [[Fennoscandia]]. The Sveconorwegian Orogen (including the Western Gneiss Region) is shown in pink. The [[nappe]]s emplaced by the much younger Caledonian orogeny are shown in light green.](https://commons.wikimedia.org/wiki/Special:FilePath/Overview Baltic shield.png?width=200 "Geological map of [[Fennoscandia]]. The Sveconorwegian Orogen (including the Western Gneiss Region) is shown in pink. The [[nappe]]s emplaced by the much younger Caledonian orogeny are shown in light green.")
MOUNTAIN-BUILDING ERA
Caledonian Orogeny; Caledonian mountains; Caledonides; Caledonian Mountains; Caledonian Orogenic Belt; Caledonian folding; Caledonian fold mountains; Grampian phase; Grampian Orogeny; Scandian phase
The Caledonian orogeny was a mountain-building era recorded in the northern parts of the British Isles, the Scandinavian Mountains, Svalbard, eastern Greenland and parts of north-central Europe. The Caledonian orogeny encompasses events that occurred from the Ordovician to Early Devonian, roughly 490–390 million years ago (Ma).
Caledonian Airways
![Boeing 707-349C]] G-AWTK of Caledonian Airways departing from [[Manchester Airport]] in 1969 when operating a transatlantic passenger charter flight](https://commons.wikimedia.org/wiki/Special:FilePath/Boeing 707-349C G-AWTK Caled RWY 26.07.69 edited-2.jpg?width=200 "Boeing 707-349C]] G-AWTK of Caledonian Airways departing from [[Manchester Airport]] in 1969 when operating a transatlantic passenger charter flight")
![scheme]] at Manchester in August 1966](https://commons.wikimedia.org/wiki/Special:FilePath/Bristol 175 Britannia 314 G-ATMA Caledn Ringway 23.08.66 edited-2.jpg?width=200 "scheme]] at Manchester in August 1966")
![Nairobi Embakasi]] in February 1976](https://commons.wikimedia.org/wiki/Special:FilePath/British Caledonian Boeing 707-338C.jpg?width=200 "Nairobi Embakasi]] in February 1976")
![Gatwick Airport]] in June 1975.](https://commons.wikimedia.org/wiki/Special:FilePath/British Caledonian Boeing 707 at Gatwick.jpg?width=200 "Gatwick Airport]] in June 1975.")
![Berlin Tegel]] in October 1967](https://commons.wikimedia.org/wiki/Special:FilePath/Caledonian Bristol Britannia.jpg?width=200 "Berlin Tegel]] in October 1967")
![Berlin Tempelhof]] in June 1964](https://commons.wikimedia.org/wiki/Special:FilePath/Caledonian DC-6B.jpg?width=200 "Berlin Tempelhof]] in June 1964")
![DC-10-30]]](https://commons.wikimedia.org/wiki/Special:FilePath/G-BWIN.jpg?width=200 "DC-10-30]]")
DEFUNCT BRITISH AIRLINE
Caledonian Airlines; Caledonian/BUA; Caledonian Airways (1988-1999)
Caledonian Airways was a wholly private, independentindependent from government-owned corporations Scottish charter airline formed in April 1961. It began with a single 104-seat Douglas DC-7C leased from Sabena.
Sveconorwegian orogeny
![A-type]] granites.](https://commons.wikimedia.org/wiki/Special:FilePath/Rodinia reconstruction.jpg?width=200 "A-type]] granites.")
OROGENIC BELT IN SOUTHWESTERN SWEDEN AND SOUTHERN NORWAY
Sirdal Magmatic Belt; Dalslandian orogeny
The Sveconorwegian orogeny was an orogenic system active 1140 to 960 million years ago and currently exposed as the Sveconorwegian orogenic belt in southwestern Sweden and southern Norway. In Norway the orogenic belt is exposed southeast of the front of the Caledonian nappe system and in nappe windows.
