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  • Variscan orogeny - Wikipedia
    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
  • Europe - Hercynian, Orogenic, Belt | Britannica
    The Hercynian, or Variscan, orogenic belt evolved during the Devonian and Carboniferous periods, from about 419 to 299 million years ago
  • Hercynian Orogeny - an overview | ScienceDirect Topics
    The Variscan (often termed Hercynian) orogeny spans most of central and south-eastern Europe from South Portugal to Poland and beyond into the Balkans and Turkey It is a collage of microcontinents which drifted off from the northern margin of Gondwana and includes Avalonia and the Armorican Terranes Assemblage (ATA)
  • The Variscan Orogeny
    In basic terms, an orogeny is a mountain building event that occurs at convergent plate boundaries An orogen is a type of geological province, along with shields, basins, platforms, large igneous provinces and the extended crust Present day orogens include the Himalayas and the Andes
  • HERCYNIAN Definition Meaning - Merriam-Webster
    The meaning of HERCYNIAN is of or relating to an extensive mountain range covered with forests in ancient Germany
  • Hercynian Forest - Wikipedia
    The Hercynian Forest was an ancient and dense forest that stretched across Western Central Europe, from Northeastern France to the Carpathian Mountains, including most of Southern Germany, though its boundaries are a matter of debate
  • The Role of the Hercynian Mountains of Central Europe in Shaping Plant . . .
    The Hercynian (Variscan) orogeny is a period of intense rock-forming movements that occurred during the Palaeozoic era, between the late Silurian and the end of the Permian
  • Hercynian orogeny | geology | Britannica
    Mountains formed during the Hercynian orogeny (mountain-building episode) of the Carboniferous Period (between about 360 and 300 million years ago) have been largely worn down by erosion, and elevations rarely exceed 1,300 feet (400 metres)
  • New insights into the Hercynian Orogeny, and their implications for the . . .
    We use the term “Hercynian” here for the timing of widespread deformation in the mid-Carboniferous, but not to imply that the Hercynian deformation in Arabia was caused by the Hercynian collision in the north Atlantic region
  • Hercynian orogeny - Oxford Reference
    A major and prolonged episode of mountain building that began in the Late Devonian and continued throughout the Carboniferous, affecting a broad belt along an approximately WSW to ENE line from what are now south-western England and north-western Europe to southern Europe and the Iberian Peninsula, and eastern N America and the Andes





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