- Italian:
- Mare Adriatico
- Bosnian, Croatian, and Montenegrin:
- Jadransko More
- Albanian:
- Deti i Adriatikut
Adriatic Sea
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What is the Adriatic Sea?
The Adriatic Sea is an arm of the Mediterranean Sea that lies between the Italian and Balkan peninsulas. The Strait of Otranto links it with the Ionian Sea to the southeast. It is approximately 500 miles (800 km) long and has an average width of 100 miles (160 km), with an area of 50,590 square miles (131,050 sq km).
The Italian coast is relatively straight, while the Croatian coast has many islands that create intricate inlets. The Gulf of Venice is the Adriatic's northern section. The bora, a strong northeast wind, can cause rough seas. The lowest surface temperatures are in the northern Adriatic, where the mean temperature in February falls to 41 °F (5 °C) in the Gulf of Trieste; ice can occasionally form there in the depth of winter.
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Where is the Adriatic Sea located?
The Adriatic Sea is an arm of the Mediterranean Sea located between the Italian and Balkan peninsulas. It links to the Ionian Sea through the Strait of Otranto at its southeastern boundary. The Croatian coast is full of islands, while the Italian coast is relatively straight. The sea is approximately 500 miles long and averages 100 miles in width, with a maximum depth of 4,035 feet.
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Which countries border the Adriatic Sea?
The Adriatic Sea, an arm of the Mediterranean Sea, is bordered by the Italian and Balkan peninsulas. The Italian coast is relatively straight, while the Croatian coast features numerous islands and intricate inlets. Slovenia also borders the Adriatic Sea.
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How is the Adriatic Sea connected to the Mediterranean Sea?
The Adriatic Sea, an arm of the Mediterranean Sea, is linked to the Ionian Sea by the Strait of Otranto. This strait, located at the Adriatic's southeastern boundary between Italy and Albania, serves as the connection point between the Adriatic and Ionian Seas. Though ancient authors considered the Ionian Sea part of the Adriatic Sea, they are now viewed as separate bodies of water. The Mediterranean Sea connects to the Atlantic Ocean via the Strait of Gibraltar and to the Black Sea via the Dardanelles, the Sea of Marmara, and the Bosporus.
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What kinds of plants and animals live in the Adriatic Sea?
The Adriatic Sea, an arm of the Mediterranean Sea, is deficient in marine life due to its low nutrient content. However, three main zones of marine life exist, each with distinctive species.
The waters of the Adriatic Sea are home to various life forms. The fishes of the Mediterranean are related to subtropical Atlantic species. Demersal fishes such as flounder, sea bass, red mullet, sharks, rays, and skates are caught by trawlers. Hake is one of the more commercially important species. Pelagic species, such as sardines, anchovy, and sprat, are commonly caught in the upper layers of the sea. Important nonedible marine products include corals.
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Why is the Adriatic Sea important to the people and economies of the region?
The Adriatic Sea is an arm of the Mediterranean Sea that plays a vital role in the economies and lives of the people in the region. It has been important in the historical development of Mediterranean Europe and is of considerable scientific interest.
For countries like Croatia and Albania, the Adriatic Sea is important for fishing and aquaculture, with sea bass, tuna, and mussels being popular products. Also, canned fish is sold to surrounding countries. The Italian coastline, which is about 4,600 miles (7,400 km), has many ports, and most of the imports and exports leave and arrive by sea. In Dalmatia, tourism has become a major economic factor, and Dubrovnik and Split are major Mediterranean tourist attractions.
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Adriatic Sea, arm of the Mediterranean Sea, lying between the Italian and Balkan peninsulas. The Strait of Otranto at its southeasterly limit links it with the Ionian Sea. It is about 500 miles (800 km) long with an average width of 100 miles, a maximum depth of 4,035 feet (1,324 metres), and an area of 50,590 sq mi (131,050 sq km). The Adriatic has been of great importance in the historical development of Mediterranean Europe and is of considerable scientific interest in itself. Modern study of the Adriatic has been carried out mainly under the auspices of several Italian and Balkan scientific institutes.
There is a striking contrast between its two shores. The Italian coast is relatively straight and continuous, having no islands, whereas the Croatian coast is full of both large and small islands, generally oblong in shape and running parallel to the continental shore. Many tortuous straits form inlets between the islands similar to those of the Norwegian fjords and make the coastline very intricate.
The depths of the Adriatic near its shores bear a close relationship to the physiography of the adjacent coasts. Wherever such coasts are high and mountainous, the nearby sea depths are considerable, as in the case of the Istrian and Dalmatian areas of Slovenia and Croatia. Where low and sandy shores are found, the nearby sea is shallow, as in the vicinity of Venice or, farther south, near the delta of the Italian Po River. Generally speaking, the waters are shallow all along the Italian coast. The site of maximum depth of the Adriatic Sea is situated south of the central area; average depth is 1,457 feet (444 metres).
The Adriatic has two types of rather special sea bottoms, difficult to arrange in a rigorous classification but very common in the Mediterranean, namely, inlet-derived sediments and heat-altered sediments of the sea bottom proper. In general, the seabed consists of a yellowish mud and sand, containing fragments of shells, fossil mollusks, and corals. The main winds prevailing in the area are the bora, a strong northeast wind that blows from the nearby mountains into the sea, and a southeasterly wind named the sirocco that is less troublesome from a navigational point of view. During the six winter months, bora and sirocco alternate, with or without an interval of a few days calm. The tides of the Adriatic, which have been intensively studied, follow a complicated pattern, sweeping into the region from the south and being linked with those of the Ionian Sea.
The tidal range is about three feet, in contrast to the general Mediterranean tidal range of about 0.9 foot. The surface currents are chiefly influenced by the blowing winds, with currents spurred by north winds reaching a speed of four miles per hour.
Temperatures in the surface layers of the sea reach 75–77 °F (24–25 °C) during the month of August, and the minimum readings, some 50 °F (10 °C), are usually reached during January and February. In the northern Adriatic, river mouth temperatures are even lower because the waters are cooled by melting ice and snow. At greater depths (820–980 feet) the maximum temperatures fluctuate around 57 °F (14 °C), while minimum temperatures are about 52 °F (11 °C).
The Adriatic Sea, like the Mediterranean in general, is deficient in life; nutrient content, as indicated by the amount of phosphates and nitrates, is extremely low. Three main areas of marine life may nevertheless be recognized. In the northern Adriatic area, significant winter cooling and a lowered salinity further impoverish the typical Mediterranean marine life. In the middle Adriatic area, life is much richer than farther north, while the southern Adriatic area has its own distinctive forms of life.
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