SanjaVodič čiji je autor

Sanja
SanjaVodič čiji je autor

Razgledavanje

The dragon's eye of the pond is elliptical in shape. It is located on the Gradina peninsula in Rogoznica, opposite the Soline bay, where the famous Frapa marina is located. Because of this shape, it is called the Dragon's Eye. It is filled with salt water and deeply cut into the rocks overgrown with macchia and lower vegetation. It is connected to the sea by a spire whose opening can be seen on the surface of the water. The cave is called the Dragon's Ear and is larger and deeper than the lake itself.In the scientific sense, the Dragon's Eye is a kind of hydrological and geomorphological phenomenon because intense biochemical processes occur in it, so we can consider it a natural bioreactor.
91 penduduk tempatan mengesyorkan
Rogoznica
91 penduduk tempatan mengesyorkan
The dragon's eye of the pond is elliptical in shape. It is located on the Gradina peninsula in Rogoznica, opposite the Soline bay, where the famous Frapa marina is located. Because of this shape, it is called the Dragon's Eye. It is filled with salt water and deeply cut into the rocks overgrown with macchia and lower vegetation. It is connected to the sea by a spire whose opening can be seen on the surface of the water. The cave is called the Dragon's Ear and is larger and deeper than the lake itself.In the scientific sense, the Dragon's Eye is a kind of hydrological and geomorphological phenomenon because intense biochemical processes occur in it, so we can consider it a natural bioreactor.
It is first mentioned on Christmas Day 1066 in a grant from Peter Kresimir IV, and is also called the city of Kresimir. Until the mid-17th century, the plague epidemic was the largest city on the entire eastern Adriatic coast. [2] [3] Šibenik was de facto the capital of Croatia from December 1944 to May 1945. It is also significant as the site of the founding of the Croatian Navy. Cathedral of St. Jacob in Šibenik is the most significant architectural achievement of the 15th and 16th centuries in Croatia. Due to its exceptional values, in 2000, it was included in the UNESCO list of World Heritage Sites, which in 2017 was joined by the Fortress of Sts. Nicholas. With its seven travertine waterfalls, the Krka River is a natural and karst phenomenon. The tufa is a common occurrence in the surface flows of the Dinaric karst, but only exceptionally creates considerable deposits that build waterfalls such as those on the Krka River. The travertine waterfalls of the Krka River are very gentle and sensitive to natural changes and all human activities. Only with the constant growth of the phytogenic tufa can the waterfalls, which are the backbone of the hydrogeological and landscape image, and the basis of the biological diversity of the Krka National Park, be preserved. The formation and growth of waterfalls is the result of complex physicochemical and biological processes. For the tufa to grow, live and age, it is necessary to preserve the natural balance of the ecosystems of the rivers Krka and Čikola. With its seven travertine waterfalls: Bilusic Noise, Brljan, Manojlovac Waterfall, Rosnjak, Miljacka Waterfall, Rosko Waterfall and Skradinski Buk, the Krka River is a natural and karst phenomenon.
Šibenik-Knin County
It is first mentioned on Christmas Day 1066 in a grant from Peter Kresimir IV, and is also called the city of Kresimir. Until the mid-17th century, the plague epidemic was the largest city on the entire eastern Adriatic coast. [2] [3] Šibenik was de facto the capital of Croatia from December 1944 to May 1945. It is also significant as the site of the founding of the Croatian Navy. Cathedral of St. Jacob in Šibenik is the most significant architectural achievement of the 15th and 16th centuries in Croatia. Due to its exceptional values, in 2000, it was included in the UNESCO list of World Heritage Sites, which in 2017 was joined by the Fortress of Sts. Nicholas. With its seven travertine waterfalls, the Krka River is a natural and karst phenomenon. The tufa is a common occurrence in the surface flows of the Dinaric karst, but only exceptionally creates considerable deposits that build waterfalls such as those on the Krka River. The travertine waterfalls of the Krka River are very gentle and sensitive to natural changes and all human activities. Only with the constant growth of the phytogenic tufa can the waterfalls, which are the backbone of the hydrogeological and landscape image, and the basis of the biological diversity of the Krka National Park, be preserved. The formation and growth of waterfalls is the result of complex physicochemical and biological processes. For the tufa to grow, live and age, it is necessary to preserve the natural balance of the ecosystems of the rivers Krka and Čikola. With its seven travertine waterfalls: Bilusic Noise, Brljan, Manojlovac Waterfall, Rosnjak, Miljacka Waterfall, Rosko Waterfall and Skradinski Buk, the Krka River is a natural and karst phenomenon.

Razgledavanje

It is first mentioned on Christmas Day 1066 in a grant from Peter Kresimir IV, and is also called the city of Kresimir. Until the mid-17th century, the plague epidemic was the largest city on the entire eastern Adriatic coast. [2] [3] Šibenik was de facto the capital of Croatia from December 1944 to May 1945. It is also significant as the site of the founding of the Croatian Navy. Cathedral of St. Jacob in Šibenik is the most significant architectural achievement of the 15th and 16th centuries in Croatia. Due to its exceptional values, in 2000, it was included in the UNESCO list of World Heritage Sites, which in 2017 was joined by the Fortress of Sts. Nicholas. With its seven travertine waterfalls, the Krka River is a natural and karst phenomenon. The tufa is a common occurrence in the surface flows of the Dinaric karst, but only exceptionally creates considerable deposits that build waterfalls such as those on the Krka River. The travertine waterfalls of the Krka River are very gentle and sensitive to natural changes and all human activities. Only with the constant growth of the phytogenic tufa can the waterfalls, which are the backbone of the hydrogeological and landscape image, and the basis of the biological diversity of the Krka National Park, be preserved. The formation and growth of waterfalls is the result of complex physicochemical and biological processes. For the tufa to grow, live and age, it is necessary to preserve the natural balance of the ecosystems of the rivers Krka and Čikola. With its seven travertine waterfalls: Bilusic Noise, Brljan, Manojlovac Waterfall, Rosnjak, Miljacka Waterfall, Rosko Waterfall and Skradinski Buk, the Krka River is a natural and karst phenomenon.
Šibenik-Knin County
It is first mentioned on Christmas Day 1066 in a grant from Peter Kresimir IV, and is also called the city of Kresimir. Until the mid-17th century, the plague epidemic was the largest city on the entire eastern Adriatic coast. [2] [3] Šibenik was de facto the capital of Croatia from December 1944 to May 1945. It is also significant as the site of the founding of the Croatian Navy. Cathedral of St. Jacob in Šibenik is the most significant architectural achievement of the 15th and 16th centuries in Croatia. Due to its exceptional values, in 2000, it was included in the UNESCO list of World Heritage Sites, which in 2017 was joined by the Fortress of Sts. Nicholas. With its seven travertine waterfalls, the Krka River is a natural and karst phenomenon. The tufa is a common occurrence in the surface flows of the Dinaric karst, but only exceptionally creates considerable deposits that build waterfalls such as those on the Krka River. The travertine waterfalls of the Krka River are very gentle and sensitive to natural changes and all human activities. Only with the constant growth of the phytogenic tufa can the waterfalls, which are the backbone of the hydrogeological and landscape image, and the basis of the biological diversity of the Krka National Park, be preserved. The formation and growth of waterfalls is the result of complex physicochemical and biological processes. For the tufa to grow, live and age, it is necessary to preserve the natural balance of the ecosystems of the rivers Krka and Čikola. With its seven travertine waterfalls: Bilusic Noise, Brljan, Manojlovac Waterfall, Rosnjak, Miljacka Waterfall, Rosko Waterfall and Skradinski Buk, the Krka River is a natural and karst phenomenon.