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.
Westernmost point. Monchique Islet, Azores Islands, Portugal (31Â° 16â² 30â³ W) (If considered part of Europe, though it sits on the North American Plate). If not, then the Capelinhos Volcano, Faial Island, Azores Islands, Portugal (28Â° 50â² 00â³ W), the westernmost point of the Eurasian Plate above sea level.