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Caledonian orogeny - перевод на испанский
![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.")
![continental plate]] to form an accretionary orogen. (example: the [[Andes]])](https://commons.wikimedia.org/wiki/Special:FilePath/Active Margin.svg?width=200 "continental plate]] to form an accretionary orogen. (example: the [[Andes]])")
![[[Continental collision]] of two continental plates to form a collisional orogen. Typically, continental crust is subducted to lithospheric depths for [[blueschist]] to [[eclogite facies]] metamorphism, and then exhumed along the same subduction channel. (example: the [[Himalayas]])](https://commons.wikimedia.org/wiki/Special:FilePath/Continental-continental convergence Fig21contcont.gif?width=200 "[[Continental collision]] of two continental plates to form a collisional orogen. Typically, continental crust is subducted to lithospheric depths for [[blueschist]] to [[eclogite facies]] metamorphism, and then exhumed along the same subduction channel. (example: the [[Himalayas]])")
![[[Mount Rundle]], [[Banff, Alberta]].](https://commons.wikimedia.org/wiki/Special:FilePath/Mount Rundle, Banff, Canada (200544945).jpg?width=200 "[[Mount Rundle]], [[Banff, Alberta]].")
![delamination]]) as seen from the [[International Space Station]].](https://commons.wikimedia.org/wiki/Special:FilePath/Sierra Nevada Mountains.JPG?width=200 "delamination]]) as seen from the [[International Space Station]].")
Ex: This digital tapestry outlines the geologic story of continental collision and break-up, mountain-building, river erosion and deposition, glaciation, volcanism, and other events and processes that have shaped the region.
Определение
Википедия
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). It was caused by the closure of the Iapetus Ocean when the continents and terranes of Laurentia, Baltica and Avalonia collided.
The orogeny is named for Caledonia, the Latin name for Scotland. The term was first used in 1885 by Austrian geologist Eduard Suess for an episode of mountain building in northern Europe that predated the Devonian period. Geologists like Émile Haug and Hans Stille saw the Caledonian event as one of several episodic phases of mountain building that had occurred during Earth's history. Current understanding has it that the Caledonian orogeny encompasses a number of tectonic phases that can laterally be diachronous. The name "Caledonian" can therefore not be used for an absolute period of geological time, it applies only to a series of tectonically related events.
