Province of Brindisi | ||
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Province | ||
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Map highlighting the location of the province of Brindisi in Italy |
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Country | Italy | |
Region | Apulia | |
Capital(s) | Brindisi | |
Comuni | 20 | |
Government | ||
• President | Massimo Ferrarese | |
Area | ||
• Total | 1,839 km2 (710 sq mi) | |
Population (2013) | ||
• Total | 401,652 | |
• Density | 220/km2 (570/sq mi) | |
Time zone | CET (UTC+1) | |
• Summer (DST) | CEST (UTC+2) | |
Postal code | 72012-72015, 72017-72018, 72020-72027, 72029 | |
Telephone prefix | 080, 0831 | |
Vehicle registration | BR | |
ISTAT | 074 |
The Province of Brindisi (Italian: Provincia di Brindisi) is a province in the Apulia region of Italy. Its capital is the city of Brindisi. It has an area of 1,839 square kilometres (710 sq mi) and a total population of 401,652 (2013).
The Province of Brindisi is situated in southeastern Italy, extending for 1,839 square kilometres (710 sq mi), the second smallest province in the region after the Province of Barletta-Andria-Trani. It was established in 1927 from the ancient Terra d'Otranto. With the Adriatic Sea to the east, it is bordered to the north by the Province of Bari, on the west by the Province of Taranto and to the south-east by the Province of Lecce. The northern, central and western parts are hilly with much woodland, with the Murgia hills of particular note, while to the north-west, bordering on the provinces of Taranto and Bari, it is lower-lying, with the Itria Valley (Valle d'Itria). The maximum height reached within the province is 414 metres (1,358 ft) above sea level, near Selva di Fasano. The other peaks are slightly lower and are all located in the north-central area. The coastline in the province is 80.606 kilometres (50.086 mi) long, partly rocky, with many alternating stretches of sandy beaches, small harbours and bays. To the south it is essentially flat and widely used for crops.
The province, according to the Geological Map of Italy, prepared by the Geological Survey of Italy, is composed of various types of land: in the central-southern area there is a predominance of dolomitic limestone (present generally in the inhabited zone from the plateau of the Murgia), small eluvial deposits, sand, clay, grey silted marshes (around Francavilla Fontana, Oria and San Donaci), chalk and limestone, including firm bioclastic limestone and chalky sandstone. In the north-central part, particularly Bari and Mola, the limestone stems from the Late Cretaceous, and deposits of limestone and sandstone date back to the . There are no significant rivers, because of the karst terrain, but there are many springs that gush out producing little streams. As for waterways, the longest is the Canale Reale, which flows into the territory of Villa Castelli, bordering Francavilla Fontana, and flows into the Natural Reserve of Torre Guaceto. Along the coast, in addition, there are numerous ponds and small freshwater lakes, fed by underground aquifers.