Meteora! In central Greece and particularly in the North-Western part of Thessaly, between North East of Hasia and West of Pindos, where the plain of Thessaly ends, gigantic rocks raise, that create a spectacle which might be unique worldwide.
No reference concerning these rocks exists, neither in mythology nor by some Greek or foreign historians.
Historians and geologists started to be interested in the creation of these rocks about 1000 years ago, expressing several theories.
The prevailing theory is that one of the German geologist Philipson, who came to Greece in the late 19th century. According to his theory, a large river had his estuary in this area which for millions of years was covered by a narrow and deep part of the sea. The river waters place matter, stones and generally several materials that were transferred by its waters at the estuary from Northern parts of primordial central Europe. From the accumulation of these materials, deltaic cones were formed.
25-30 million years ago, after some geological changes took place during the centuries, the central part of today’s Europe was lifted. That’s how the opening of Tempi was created, having, as a result, the pouring of the waters in today’s Aegean sea.
During the tertiary period, at the time of the alpine orogenies, the solid volumes of the “rocks” were cut off from the mountain chain of Pindos that was created and as the centuries went by, the plain of Pinios river was formed between them.
With the continuous corrosion by the wind and the rain as well as by other geological changes, these rocks took their present form through the passing of millions of years.
Organised day trips to Meteora are available from Corfu and Halkidiki considering that a very early morning start is involved. Meteora can also be visited if you are holidaying in Athens but we would strongly recommend an overnight stay.
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