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.
Situated in the northeastern portion of the Balkan Peninsula, the country is halfway between the equator and the North Pole and equidistant from the westernmost part of Europe--the Atlantic Coast--and the most easterly--the Ural Mountains.