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Image: Stampfli & Borel 2000 · Attribution

Armorican terrane

Armorican terrane

Microcontinent or group of continental fragments rifted away from Gondwana.

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  1. Variscan orogeny

    Collision of tectonic plates resulting in the creation of mountains.

    27%

  2. Avalonia

    Microcontinent in the Paleozoic era.

    22%

  3. Armorica

    Region of Gaul between the Seine and Loire rivers.

    18%

  4. Gondwana

    Neoproterozoic to Cretaceous landmass.

    17%

Readers come from

Share of the 713 readers arriving from another article

  1. Avalonia

    Microcontinent in the Paleozoic era.

    36%

  2. Variscan orogeny

    Collision of tectonic plates resulting in the creation of mountains.

    16%

  3. Laurasia

    Northern landmass that formed part of the Pangaea supercontinent.

    9.8%

  4. Paleo-Tethys Ocean

    Ocean on the margin of Gondwana between the Middle Cambrian and Late Triassic.

    9.3%

  5. Caledonian orogeny

    Mountain building event caused by the collision of Laurentia, Baltica and Avalonia.

    3.8%