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Brodarica
Brodarica is a village located 8 km south of Šibenik, Croatia. It is located on the Adriatic Sea coast, across the island of Krapanj and west of the bay of Morinje, by the D8 state road. The population is 2,534 (census 2011). Image gallery File:View of Krapanj from Brodarica coast.jpg, View of Krapanj from Brodarica coast File:Brodarica promenade.jpg, Brodarica promenade File:Brodarica bridge.jpg, Brodarica bridge connecting Brodarica to Šibenik Šibenik () is a historic city in Croatia, located in central Dalmatia, where the river Krka flows into the Adriatic Sea. Šibenik is a political, educational, transport, industrial and tourist center of Šibenik-Knin County, and is also the ... File:Beach Rezalište in Brodarica.jpg, Beach Rezalište in Brodarica File:Ship carrying passengers from Krapanj to Brodarica.jpg, Boat carrying passengers from Krapanj to Brodarica File:Brodarica coast.jpg, Brodarica coast File:Sunset in Brodarica.jpg, alt=Sunset in Brodarica, ...
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Brodarica is a village located 8 km south of Šibenik, Croatia. It is located on the Adriatic Sea coast, across the island of Krapanj and west of the bay of Morinje, by the D8 state road. The population is 2,534 (census 2011). Image gallery File:View of Krapanj from Brodarica coast.jpg, View of Krapanj from Brodarica coast File:Brodarica promenade.jpg, Brodarica promenade File:Brodarica bridge.jpg, Brodarica bridge connecting Brodarica to Šibenik File:Beach Rezalište in Brodarica.jpg, Beach Rezalište in Brodarica File:Ship carrying passengers from Krapanj to Brodarica.jpg, Boat carrying passengers from Krapanj Krapanj is an island in the Adriatic Sea, located south of Šibenik, Croatia. Krapanj is one of the smallest inhabited islands of the Adriatic Sea covering 0.36 km2. It is also the most densely inhabited island and has the lowest elevation ... to Brodarica File:Brodarica coast.jpg, Brodarica coast File:Sunset in Brodarica.jpg, alt=Sunset in Brodarica, S ...
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Krapanj
Krapanj is an island in the Adriatic Sea, located south of Šibenik, Croatia. Krapanj is one of the smallest inhabited islands of the Adriatic Sea covering 0.36 km2. It is also the most densely inhabited island and has the lowest elevation (1.5 m above sea level). Krapanj is 300 m offshore at its closest point from the mainland village of Brodarica. Geography The average elevation is about and the highest point is above sea level. It lies in the Dinaric direction, from north-west to south-east. Geology Krapanj is composed of Mesozoic limestone and dolomite. Climate The island of Krapanj is situated in the central part of the Croatian littoral and is characterised by a warm, dry Mediterranean climate. According to data from the nearest weather station, in Šibenik, for the period from 1986 to 1996 the average annual temperature was and the average annual precipitation . History Many of the Adriatic Islands were populated in pre-history by the Illyrians. K ...
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Šibenik
Šibenik () is a historic city in Croatia, located in central Dalmatia, where the river Krka flows into the Adriatic Sea. Šibenik is a political, educational, transport, industrial and tourist center of Šibenik-Knin County, and is also the third-largest city in the Dalmatian region. As of 2011, the city has 34,302 inhabitants, while the municipality has 46,332 inhabitants. History Etymology There are multiple interpretations of how Šibenik was named. In his fifteenth century book ''De situ Illiriae et civitate Sibenici,'' Juraj Šižgorić describes the name and location of Šibenik. He attributes the name of the city to it being surrounded by a palisade made of ''šibe'' (sticks, singular being ''šiba''). Another interpretation is associated with the forest through the Latin toponym "Sibinicum", which covered a narrower microregion within Šibenik on and around the area of St. Michael's Fortress. Early history Unlike other cities along the Adriatic coast, which we ...
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D8 (Croatia)
The D8 state road is the Croatian section of the Adriatic Highway, running from the Slovenian border at Pasjak via Rijeka, Senj, Zadar, Šibenik, Split (city), Split, Opuzen and Dubrovnik to the border with Montenegro at Karasovići. Most of the D8 state road remains single carriageway, though with some dual carriageway stretches. The total length of the road through Croatia is . Until recently, the road was the primary route connecting the Adriatic coastal parts of Croatia. Since the 2000s, multilane motorways have taken over most of its traffic, and yet more motorways are still being built along the coast. The motorways parallel to the road are the A7 (Croatia), A7 (Rupa, Croatia, Rupa border crossing – Rijeka – Sveti Kuzam), A6 (Croatia), A6 (Rijeka – Bosiljevo 2 interchange, Bosiljevo) and A1 (Croatia), A1 (Zagreb – Bosiljevo – Zadar – Split (city), Split – Ploče), sections of the proposed Adriatic–Ionian motorway. Since the D8 closely follows the well- ...
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Croatia
, image_flag = Flag of Croatia.svg , image_coat = Coat of arms of Croatia.svg , anthem = "Lijepa naša domovino"("Our Beautiful Homeland") , image_map = , map_caption = , capital = Zagreb , coordinates = , largest_city = capital , official_languages = Croatian , languages_type = Writing system , languages = Latin , ethnic_groups = , ethnic_groups_year = 2021 , religion = , religion_year = 2021 , demonym = , government_type = Unitary parliamentary republic , leader_title1 = President , leader_name1 = Zoran Milanović , leader_title2 = Prime Minister , leader_name2 = Andrej Plenković , leader_title3 = Speaker of Parliament , leader_name3 = Gordan Jandroković , legislature = Sabor , sovereignty_type ...
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Adriatic Sea
The Adriatic Sea () is a body of water separating the Italian Peninsula from the Balkan Peninsula. The Adriatic is the northernmost arm of the Mediterranean Sea, extending from the Strait of Otranto (where it connects to the Ionian Sea) to the northwest and the Po Valley. The countries with coasts on the Adriatic are Albania, Bosnia and Herzegovina, Croatia, Italy, Montenegro, and Slovenia. The Adriatic contains more than 1,300 islands, mostly located along the Croatian part of its eastern coast. It is divided into three basins, the northern being the shallowest and the southern being the deepest, with a maximum depth of . The Otranto Sill, an underwater ridge, is located at the border between the Adriatic and Ionian Seas. The prevailing currents flow counterclockwise from the Strait of Otranto, along the eastern coast and back to the strait along the western (Italian) coast. Tidal movements in the Adriatic are slight, although larger amplitudes are known to occur occasi ...
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Morinje
Morinje (''Morinjski zaljev'', Italian: ''Morigne, Lago di Castello Andreis'') is the toponym for a bay in Croatia. The Morinje Bay in Dalmatia, with a surface area of 3.5 km² and a maximum depth of 21 metres, is situated five kilometres south-east of Šibenik in the central part of the eastern Adriatic coast. It is hydrogeomorphologically divided into two parts – a shallow northern funnel (Morinje) and the deeper southern channel-shaped Jadrtovac passage. With the postglacial rising of the sea level, the bay took its current shape. Morinje has no permanent riverine inflow, only an insignificant and intermittent superficial rivulet (Ribnik) and several underwater springs. In the 13th century, the area at Morinje was mentioned as ''Campus marinus''. A German nobleman in the late 15th century called the place “Moreya”. The historical settlement Jadrtovac developed from a fortification on the eastern shore. North-east of the bay is the Gothic church of Saint Lawrence Sain ...
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Beach Rezalište
A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are typically made from rock, such as sand, gravel, shingle, pebbles, etc., or biological sources, such as mollusc shells or coralline algae. Sediments settle in different densities and structures, depending on the local wave action and weather, creating different textures, colors and gradients or layers of material. Though some beaches form on inland freshwater locations such as lakes and rivers, most beaches are in coastal areas where wave or current action deposits and reworks sediments. Erosion and changing of beach geologies happens through natural processes, like wave action and extreme weather events. Where wind conditions are correct, beaches can be backed by coastal dunes which offer protection and regeneration for the beach. However, these natural forces have become more extreme due to climate change, permanently altering beaches at very rapid ...
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