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The Variscan orogeny or Hercynian orogeny was a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea. It remains visible today as a series of isolated massifs, including the Ardennes, Bohemian Massif, Vosges-Black Forest, Odenwald, Armorican…
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variscan orogeny mountains hercynian massifs europe massif chain belt continental collision ma late north central gondwana ardennes appalachian metamorphic rocks
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Variscan orogeny | related to Formation | The Variscan | 0.60 | section |
| Variscan orogeny | related to Formation | During | 0.60 | section |
| Variscan orogeny | related to Formation | Variscan | 0.60 | section |
| Variscan orogeny | related to Formation | Cambrian | 0.60 | section |
| Variscan orogeny | related to Formation | Ordovician | 0.60 | section |
| Variscan orogeny | related to Formation | Ma | 0.60 | section |
| Variscan orogeny | related to Formation | Rodinia | 0.60 | section |
| Variscan orogeny | related to Formation | Northern Europe | 0.60 | section |
| Variscan orogeny | related to Formation | Gondwana | 0.60 | section |
| Variscan orogeny | related to Formation | This | 0.60 | section |
| Variscan orogeny | related to Formation | Laurentia | 0.60 | section |
| Variscan orogeny | related to Formation | Baltica | 0.60 | section |
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