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Jabuka–Andrija Fault
The Jabuka–Andrija Fault is a seismically active thrust fault under the Adriatic Sea in Croatia. A 2003 series of earthquakes near Jabuka island, the strongest reaching a magnitude of 5.5, was caused by movements along the Jabuka–Andrija Fault. See also * Jabuka (island) Jabuka (, which means ''apple'' in Croatian) is an uninhabited volcanic island in the Adriatic Sea, west of the island of Vis. It is part of the Dalmatian archipelago. The closest land masses are the small islands of Svetac and Brusnik. Jab ... * Svetac, an island also known as Sveti Andrija References Geology of Croatia Seismic faults of Europe {{DEFAULTSORT:Jabuka-Andrija Fault ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thrust Fault
A thrust fault is a break in the Earth's crust, across which older rocks are pushed above younger rocks. Thrust geometry and nomenclature Reverse faults A thrust fault is a type of reverse fault that has a dip of 45 degrees or less. If the angle of the fault plane is lower (often less than 15 degrees from the horizontal) and the displacement of the overlying block is large (often in the kilometer range) the fault is called an ''overthrust'' or ''overthrust fault''. Erosion can remove part of the overlying block, creating a ''fenster'' (or ''window'') – when the underlying block is exposed only in a relatively small area. When erosion removes most of the overlying block, leaving island-like remnants resting on the lower block, the remnants are called ''klippen'' (singular '' klippe''). Blind thrust faults If the fault plane terminates before it reaches the Earth's surface, it is called a ''blind thrust'' fault. Because of the lack of surface evidence, blind thrust fa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adriatic Sea
The Adriatic Sea () is a body of water separating the Italian Peninsula from the Balkans, 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 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 prevailing currents flow counterclockwise from the Strait of Otranto. Tidal movements in the Adriatic are slight, although acqua alta, larger amplitudes occur occasionally. The Adriatic's salinity is lower than the Mediterranean's because it collects a third of the fresh water flowing into the Mediterranean, acting as a dilution basin. The surface water temperatures ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Croatia
Croatia, officially the Republic of Croatia, is a country in Central Europe, Central and Southeast Europe, on the coast of the Adriatic Sea. It borders Slovenia to the northwest, Hungary to the northeast, Serbia to the east, Bosnia and Herzegovina and Montenegro to the southeast, and shares a maritime border with Italy to the west. Its capital and largest city, Zagreb, forms one of the country's Administrative divisions of Croatia, primary subdivisions, with Counties of Croatia, twenty counties. Other major urban centers include Split, Croatia, Split, Rijeka and Osijek. The country spans , and has a population of nearly 3.9 million. The Croats arrived in modern-day Croatia, then part of Illyria, Roman Illyria, in the late 6th century. By the 7th century, they had organized the territory into Duchy of Croatia, two duchies. Croatia was first internationally recognized as independent on 7 June 879 during the reign of Duke Branimir of Croatia, Branimir. Tomislav of Croatia, Tomis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jabuka (island)
Jabuka (, which means ''apple'' in Croatian) is an uninhabited volcanic island in the Adriatic Sea, west of the island of Vis. It is part of the Dalmatian archipelago. The closest land masses are the small islands of Svetac and Brusnik. Jabuka is the farthest from the nearest land mass out of all Croatian islands. Flora and fauna Its coast is steep and difficult to approach, and landings can be made only when the weather is clear. The easiest access is on the south-west side. On the island, noteworthy species such as a Dalmatian Wall Lizard and some plants (''Centaurea jabukensis'' and ''Centaurea crithmifolia'', both ''Asteraceae'') are protected endemics. In 1958 the island was declared a geological monument of nature. The surrounding sea is rich with fish, especially sea bream. However, due to remoteness, lack of safe harbour, strong currents, and sudden changes of weather, fishermen have traditionally avoided the waters around Jabuka. Birds Jabuka, along with Vis, S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Svetac
Sveti Andrija (, meaning "Saint Andrew"), often called Svetac (, meaning "saint"), is an island in the Croatian part of the Adriatic Sea. Svetac is situated from Komiža (a town on the island of Vis). It is uninhabited, although it used to have permanent residents. Approximately 300 meters off the south-west coast of the island there is the islet of Kamnik, and farther on the open sea there is the volcanic island called Jabuka. About to the southeast there is the small volcanic island of Brusnik. History Svetac was inhabited in prehistoric era, as evidenced by archeological remains, the oldest of which were found in Tovorski bod, a cave in the south part of the island. A Benedictine monastery built on the island was abandoned in late 15th or early 16th century. In 1760, a small pine tar factory was opened. After the pine forest on the island was completely cut down, the factory was closed, and Svetac was acquired by members of Zanki family, who settled there. The population ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of Croatia
The geology of Croatia has some Precambrian rocks mostly covered by younger sedimentary rocks and deformed or superimposed by tectonic activity. The country is split into two main onshore provinces, a smaller part of the Pannonian Basin and the larger Dinarides. These areas are very different. The carbonate platform karst landscape of Croatia helped to create the weathering conditions to form bauxite, gypsum, clay, spilite, and limestone. Geography The territory covers , consisting of of land and of water. Elevation ranges from the mountains of the Dinaric Alps with the highest point of the Dinara peak at near the border with Bosnia and Herzegovina in the south to the shore of the Adriatic Sea which makes up its entire southwest border. Insular Croatia consists of over a thousand islands and islets varying in size, 48 of which List of inhabited islands of Croatia, permanently inhabited. The largest islands are Cres and Krk, each of them having an area of around . Karst t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
