This file presents all the airports in Greece. There are at about 35 Airports in Greece. Most of them on the Aegean Islands. The main "gate" greece is El. Venizelos Airport, Athens. But you can be anywhere to Greece by plane.
This file is important for all people travelling to Greece, or the Greek islands! Includes everything you need to know about the town of Rafina - the second most important port in Greece. There are more than 50 placemarks, with info about many, a photo of the famous monument of a nude lady in the central square and of course all 3 hotels in Rafina. Enjoy!
Greek: Δωδεκάνησα, Dodekánisa, meaning "twelve islands"
are a group of Greek islands in the Aegean Sea, off the southwest coast of Turkey. They have a rich history, and many of even the smallest inhabited islands boast dozens of Byzantine churches and medieval castles.
The Leeward Islands are the northern islands of the Lesser Antilles. They are called "leeward" because the prevailing winds in the area blow from south to north. Thus, the Leeward Islands are downwind, on the backside, or leeward from the Windward Islands, the group of islands that first meet the Trade Winds coming from the south.
The Cyclades, from the Greek Κυκλάδες, ("circular," modern Greek Kykládes) form an island group south-east of the mainland of Greece. They are a part of the vast number of islands which constitute the Greek archipelago in the Aegean Sea. The name was originally used to indicate those islands that formed a rough circle around the sacred island of Delos.
Galapagos Islands map overlay
The Galapagos Islands are found 1000 kilometres (600 miles) off the west coast of Ecuador, South America. The archipelago is made up of 13 large islands, 6 smaller islands and 107 rocks and islets. The very first island is thought to have formed between 5 and 10 million years ago, as a result of tectonic activity. The youngest islands, Isabela and Fernandina...
Hawaiian Islands (historically the Sandwich Islands) in the Pacific Ocean. All of the Islands were formed by volcanoes arising from the sea floor through a vent described in geological theory as a hotspot.
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