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.
The furthest westerly point on the mainland continent is Cabo da Roca in Portugal. <b>Monchique Islet</b> (<i>IlhÃ©u do Monchique</i>) part of the Azores at 31Âº 16' 24â³ W is the furthest westerly point of Europe and far more west than Ireland and Iceland. <br />The furthest westerly point on the mainland continent is Cabo da Roca in Portugal.