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Vlatko
June 29, 2017
The Guduča River is flooded in Prukljan, whose mouth is important in the ornithological sense. Today, this site is characterized by morphology and genesis typical of the river - the submerged lower river valley. The Krka Canyon is formed mostly in Tertiary, and after the last glacier, at the end of the Pleistocene 10,000 years ago, raising the sea level by about 100 meters gives today's appearance. The whole area from Skradin to the fortress of Sv. Nicholas is the mouth of the river Krka, so-called ria.
The Guduča River is flooded in Prukljan, whose mouth is important in the ornithological sense. Today, this site is characterized by morphology and genesis typical of the river - the submerged lower river valley. The Krka Canyon is formed mostly in Tertiary, and after the last glacier, at the end of…

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