Cross bedding forms primarily by migration or ripples and dunes in water or air. Ripple or dune migration leads to formation of dipping foreset laminae owing to avalanching or suspension settling in the zone of separation on the lee sides of the bedforms.
The most southerly point of Europe (well of the European continent) is the Greek island of Gavdos, just south of Crete.
Continental Europeâs highest sea cliff (621m) is the VixÃ­a Herbeira at Santo AndrÃ© de Teixido in Galicia (SPAIN). Hornelen in Norway, Cape Enniberg in the Faroes, and Croaghaun on Achill Island in Ireland are all higher but are islands.