Variscan orogeny
![Location of the Hercynian-Alleghenian mountain belts in the middle of the Carboniferous period. Present day coastlines are indicated in grey for reference.[1]](/Images/godic/202502/19/Hercynides_EN.svg5528.png")
![Distribution of orogenies with similar ages to the Variscan orogeny (shaded)](/Images/godic/202502/19/Distribution_of_varisican_orogenies5528.png")
The Variscan or Hercynian orogeny is a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.
Variscides
英语百科
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