zafiris
January 2nd, 2005, 08:05 PM
24 monasteries in the most amazing place in Greece.
http://www.meteora-greece.com/photos/meteora_va_2.jpg
http://www.meteora-greece.com/photos/meteora_ni_2.jpg
http://www.kalampaka.com/photos/Agios_Stefanos/HPIM1142.jpg
http://www.kalampaka.com/photos/Agios_Stefanos/HPIM0455.jpg
http://www.kalampaka.com/photos/Agios_Stefanos/HPIM4659-1.jpg
http://www.kalampaka.com/photos/Agios_Stefanos/HPIM4629-1.jpg
http://www.kalampaka.com/photos/Agios_Stefanos/HPIM3304.jpg
http://www.kalampaka.com/photos/Agia_Triada/HPIM1140.jpg
http://www.kalampaka.com/photos/Agia_Triada/HPIM1053.jpg
http://www.kalampaka.com/photos/Agios_Nikolaos/HPIM1171.jpg
http://www.kalampaka.com/photos/Agios_Nikolaos/HPIM1699.jpg
http://www.kalampaka.com/photos/Roussanou/HPIM5030.jpg
http://www.kalampaka.com/photos/Roussanou/HPIM0236.jpg
http://www.kalampaka.com/photos/Roussanou/HPIM4210.jpg
http://www.kalampaka.com/photos/climbing/climber2.jpg
http://www.kalampaka.com/photos/Panagia/HPIM1122.jpg
http://www.kalampaka.com/photos/Panagia/HPIM3414.jpg
http://www.kalampaka.com/photos/fylakes_skites/HPIM3372.jpg
http://www.kalampaka.com/photos/Mpantovas/HPIM4517.jpg
http://www.kalampaka.com/photos/Ypapanti/HPIM4300.jpg
http://www.kalampaka.com/photos/Ypapanti/HPIM0347.jpg
http://www.kalampaka.com/photos/Agios_Georgios_Mantilas/HPIM3399.jpg
http://www.kalampaka.com/photos/Agios_Georgios_Mantilas/HPIM5069.jpg
http://www.kalampaka.com/photos/Megalo_Meteoro/HPIM3836.jpg
http://www.kalampaka.com/photos/Varlaam/HPIM0150.jpg
http://www.kalampaka.com/photos/Varlaam/HPIM4320.jpg
http://www.kalampaka.com/photos/Varlaam/HPIM1706.jpg
http://www.kalampaka.com/photos/Kalampaka/HPIM1049.jpg
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 million 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.
http://www.meteora-greece.com/photos/meteora_va_2.jpg
http://www.meteora-greece.com/photos/meteora_ni_2.jpg
http://www.kalampaka.com/photos/Agios_Stefanos/HPIM1142.jpg
http://www.kalampaka.com/photos/Agios_Stefanos/HPIM0455.jpg
http://www.kalampaka.com/photos/Agios_Stefanos/HPIM4659-1.jpg
http://www.kalampaka.com/photos/Agios_Stefanos/HPIM4629-1.jpg
http://www.kalampaka.com/photos/Agios_Stefanos/HPIM3304.jpg
http://www.kalampaka.com/photos/Agia_Triada/HPIM1140.jpg
http://www.kalampaka.com/photos/Agia_Triada/HPIM1053.jpg
http://www.kalampaka.com/photos/Agios_Nikolaos/HPIM1171.jpg
http://www.kalampaka.com/photos/Agios_Nikolaos/HPIM1699.jpg
http://www.kalampaka.com/photos/Roussanou/HPIM5030.jpg
http://www.kalampaka.com/photos/Roussanou/HPIM0236.jpg
http://www.kalampaka.com/photos/Roussanou/HPIM4210.jpg
http://www.kalampaka.com/photos/climbing/climber2.jpg
http://www.kalampaka.com/photos/Panagia/HPIM1122.jpg
http://www.kalampaka.com/photos/Panagia/HPIM3414.jpg
http://www.kalampaka.com/photos/fylakes_skites/HPIM3372.jpg
http://www.kalampaka.com/photos/Mpantovas/HPIM4517.jpg
http://www.kalampaka.com/photos/Ypapanti/HPIM4300.jpg
http://www.kalampaka.com/photos/Ypapanti/HPIM0347.jpg
http://www.kalampaka.com/photos/Agios_Georgios_Mantilas/HPIM3399.jpg
http://www.kalampaka.com/photos/Agios_Georgios_Mantilas/HPIM5069.jpg
http://www.kalampaka.com/photos/Megalo_Meteoro/HPIM3836.jpg
http://www.kalampaka.com/photos/Varlaam/HPIM0150.jpg
http://www.kalampaka.com/photos/Varlaam/HPIM4320.jpg
http://www.kalampaka.com/photos/Varlaam/HPIM1706.jpg
http://www.kalampaka.com/photos/Kalampaka/HPIM1049.jpg
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 million 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.