Variscan orogeny

（重定向自Hercynian 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]

Distribution of orogenies with similar ages to the Variscan orogeny (shaded)

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.

单词	Hercynian orogeny
释义	Hercynian orogeny 英语百科 Variscan orogeny （重定向自Hercynian orogeny） 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.
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