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De geologie van Schotland is verrassend ge … De geologie van Schotland is verrassend gevarieerd voor de grootte van het land, met een groot aantal verschillende geologische kenmerken. Er zijn drie verschillende geografische regio's aan te wijzen: de Hooglanden en Eilanden is een diverse regio die ten noorden en westen van de ligt; de Central Lowlands is een riftvallei die vooral uit formaties uit het Paleozoïcum bestaat, en de Southern Uplands, die ten zuiden van een tweede breuklijn ligt en voornamelijk uit Silurisch afzettingen bestaat. Het gesteente bestaat onder andere uit zeer oud Archeïsch gneis, metamorf gesteente met ingedrongen graniet die ontstaan zijn tijdens de Caledonische orogenese, commercieel belangrijke elementen als steenkool, olie en ijzer met carboon afzettingen en de overblijfselen van Tertiairse vulkanen. Gedurende de geschiedenis varieerde het klimaat van Schotland van poolklimaat tot woestijn tot tropisch waardoor een zeer grote variëteit aan fossielen is terug te vinden. Schotland heeft ook een belangrijke rol gespeeld in ontdekkingen als platentektoniek en de ontwikkeling van theorieën over de vorming van gesteentes en was het vaderland van belangrijke figuren als James Hutton, en Archibald Geikie. Verschillende locaties als de '' bij Siccar Point in Berwickshire en de Moine thrust in het noordwesten waren ook belangrijk in de ontwikkeling van de geologie.ngrijk in de ontwikkeling van de geologie.
, The geology of Scotland is unusually varie … The geology of Scotland is unusually varied for a country of its size, with a large number of differing geological features. There are three main geographical sub-divisions: the Highlands and Islands is a diverse area which lies to the north and west of the Highland Boundary Fault; the Central Lowlands is a rift valley mainly comprising Palaeozoic formations; and the Southern Uplands, which lie south of the Southern Uplands Fault, are largely composed of Silurian deposits. The existing bedrock includes very ancient Archean gneiss, metamorphic beds interspersed with granite intrusions created during the Caledonian mountain building period (the Caledonian orogeny), commercially important coal, oil and iron bearing carboniferous deposits and the remains of substantial Palaeogene volcanoes. During their formation, tectonic movements created climatic conditions ranging from polar to desert to tropical and a resultant diversity of fossil remains. Scotland has also had a role to play in many significant discoveries such as plate tectonics and the development of theories about the formation of rocks and was the home of important figures in the development of the science including James Hutton (the "father of modern geology"), Hugh Miller and Archibald Geikie. Various locations such as 'Hutton's Unconformity' at Siccar Point in Berwickshire and the Moine Thrust in the north west were also important in the development of geological science. in the development of geological science.
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De geologie van Schotland is verrassend ge … De geologie van Schotland is verrassend gevarieerd voor de grootte van het land, met een groot aantal verschillende geologische kenmerken. Er zijn drie verschillende geografische regio's aan te wijzen: de Hooglanden en Eilanden is een diverse regio die ten noorden en westen van de ligt; de Central Lowlands is een riftvallei die vooral uit formaties uit het Paleozoïcum bestaat, en de Southern Uplands, die ten zuiden van een tweede breuklijn ligt en voornamelijk uit Silurisch afzettingen bestaat.amelijk uit Silurisch afzettingen bestaat.
, The geology of Scotland is unusually varie … The geology of Scotland is unusually varied for a country of its size, with a large number of differing geological features. There are three main geographical sub-divisions: the Highlands and Islands is a diverse area which lies to the north and west of the Highland Boundary Fault; the Central Lowlands is a rift valley mainly comprising Palaeozoic formations; and the Southern Uplands, which lie south of the Southern Uplands Fault, are largely composed of Silurian deposits.are largely composed of Silurian deposits.
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Geologie van Schotland
, Geology of Scotland
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