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'''Laurussia''' was a minor [[supercontinent]] which formed in the [[Devonian]] [[Period (geology)|period]]. It is often called the '''[[Old Red Sandstone]] Continent''' or '''Euramerica'''.
 
'''Laurussia''' was a minor [[supercontinent]] which formed in the [[Devonian]] [[Period (geology)|period]]. It is often called the '''[[Old Red Sandstone]] Continent''' or '''Euramerica'''.
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Laurussia included much of what is now northern [[Europe]], [[Greenland]] and [[North America]].  
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Laurussia included much of what is now northern [[Europe]], [[Greenland]] and [[North America]].
 
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== Lifespan ==
==Lifespan==
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Laurussia formed when 3 continents Baltica, North America, and Avalonia collided with each other during the [[Silurian]]. Baltica and Avalonia collided with each other first in the Shelveian Phase of the Caledonian orogeny. Then Avalonia and Baltica collided with North America in the Acadian Phase of the Caledonian orogeny. This drift of Avalonia closed the [[Iapetus Ocean]] and opened the Rheic Ocean behind it.
 
Laurussia formed when 3 continents Baltica, North America, and Avalonia collided with each other during the [[Silurian]]. Baltica and Avalonia collided with each other first in the Shelveian Phase of the Caledonian orogeny. Then Avalonia and Baltica collided with North America in the Acadian Phase of the Caledonian orogeny. This drift of Avalonia closed the [[Iapetus Ocean]] and opened the Rheic Ocean behind it.
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== Laurussia Media ==
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<gallery widths='160px' heights='100%' mode='traditional' caption=''>
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File:Paleoglobe NO 1590 mya-vector-colors.svg|Columbia/Nuna 1,590&nbsp;Mya
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File:Rodinia 900Ma.jpg|Rodinia 900&nbsp;Mya centred on Laurentia with Baltica and Amazonia on its southern margin.View centred on 30°S,130°E.
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File:Laurasia 430Ma.jpg|Laurussia (left) during the closure of the Iapetus Ocean 430&nbsp;Mya (middle Silurian). View centred on 0°, 60° W.
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File:Mollweide Paleographic Map of Earth, 405 Ma (Emsian Age).png|Map of Earth around 405 million years ago, during the Early Devonian, showing Euramerica (centre) and Gondwana (south and east)
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File:Laurasia 330Ma.jpg|Pangaea formed during the closure of the Rheic Ocean 330&nbsp;Mya (early Carboniferous). View centred on 30°S, 30°E.
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</gallery>
 
{{geo-stub}}
 
{{geo-stub}}
       
[[Category:Supercontinents]]
 
[[Category:Supercontinents]]