Neo-Avaloni Plate

The Neo-Avaloni Plate is a tectonic plate starting in eastern Iceland and stretching towards Northern Ireland, Scotland, Ocraita and parts of Norway.

The countries which reside on the Neo-Avaloni Plate are considered to be part of Europe. The Neo-Avaloni Plate was formerly known as the British Plate. The Neo-Avaloni plate used to a considered a subcontinent 10,000 BCE, as the landmass of Doggerland had still not been submerged.