Friuli–Venezia Giulia, regione (region) of northeastern Italy, bordering Austria to the north, Slovenia to the east, the Adriatic Sea to the south, and the Veneto region to the west. It has an area of 3,030 square miles (7,847 square km), comprising the province (provinces) of Udine, Pordenone, Gorizia, and Trieste.

In the north the solid wall of the Carnic Alps, broken only by the Monte Croce (Plöcken) Pass and the low Tarvisio saddle, form a spectacular backdrop to the Tagliamento River valley, the heart of Friuli. The southern part of the region is a low coastal plain, some of it occupied by the shallow lagoons of Grado and Caorle. To the southeast, that part of the former Free Territory of Trieste that is now an integral part of Italy extends as a narrow corridor, between the Carso (Kras) limestone plateau and the Adriatic Sea, as far as the city of Trieste. The region is one of Italy’s most seismically active, as seen in a May 1976 earthquake centred north of Udine that killed more than 1,000 people.

Known in Roman times as the Julian region, the area was divided after the barbarian invasions into a coastal part (dominated by the Byzantines through the city and port of Grado) and an inland zone ruled by the dukes of Friuli and the counts of Gorizia. The rise of the Roman Catholic patriarchate of Aquileia to prominence in the 11th century brought Friuli and the Istrian peninsula, as well as the seacoast, under the control of this ecclesiastical sovereignty.

The period of Aquileian hegemony ended when Venice became the great power in northeastern Italy (1420) and shared its dominion over the region with Austria (at Gorizia and Trieste). After 1815 all of Venezia Giulia and Friuli fell under Habsburg rule; Udine province (including Pordenone) became part of Italy in 1866, and the rest of the region (including much of what is now Slovenia and Croatia) was added in 1918. After World War II the Istrian peninsula, the hinterland of Trieste, and the Carso plateau became part of Yugoslavia, while Trieste and the area surrounding it became a free territory divided into northern and southern (A and B) zones under U.S.-British and Yugoslavian administration, respectively. Udine province was detached from the Veneto and united with Gorizia province to form Friuli–Venezia Giulia. The London agreement of 1954 restored the city of Trieste and part of zone A to Italy, and the city became the region’s capital. A statute of autonomy for the region was passed on January 31, 1963. The province of Pordenone was formed in 1968.

The region ranges in terrain from rocky uplands and foothills in the north to arid or marshy lowlands in the south. However, rainfall in the north—the highest in Italy—favours the development of natural meadows for livestock, and the ham and dairy products of Friuli are famous. Corn (maize) and some other cereals are grown in the valley of the Tagliamento, and there is market gardening around Udine. The larger cities—Udine, Pordenone, Gorizia, Monfalcone, and Trieste—have all experienced considerable industrial development, and Trieste is one of Italy’s great ports, although its trade is smaller than it was before 1914, when it served most of central Europe. The region is connected by rail and road with Austria, Slovenia, and Venice and thence the rest of Italy. A Friulian separatist movement exists and periodically presses its demands for Friulian autonomy; Friulians represent about three-fifths of the region’s population. Pop. (2011) 1,218,985.

This article was most recently revised and updated by Amy Tikkanen.
Italian:
Alpi Dolomitiche

News

Aziz Ziriat: Family 'heartbroken' after his body is found in Dolomites June 2, 2025, 4:51 AM ET (BBC)
Body of missing British hiker found in Dolomites May 31, 2025, 9:10 AM ET (The Telegraph)

Dolomites, mountain group lying in the eastern section of the northern Italian Alps, bounded by the valleys of the Isarco (northwest), the Pusteria (north), the Piave (east and southeast), the Brenta (southwest), and the Adige (west). The range comprises a number of impressive peaks, 18 of which rise to more than 10,000 feet (3,050 metres). The highest point is the Marmolada (10,964 feet [3,342 metres]), the southern face of which consists of a precipice 2,000 feet (610 metres) high. The range and its characteristic rock take their name from the 18th-century French geologist Dieudonné Dolomieu, who made the first scientific study of the region and its geology. Geologically, the mountains are formed of light-coloured dolomitic limestone, which erosion has carved into grotesque shapes. The resulting landforms include jagged, saw-edged ridges, rocky pinnacles, screes (pebble deposits) of limestone debris, deep gorges, and numerous steep rock faces at relatively low levels. Glaciated features occur at higher levels; 41 glaciers lie in the region. Many of the lower and more gentle scree slopes were once forested; only patches of woodland remain, however, interspersed with grassy meadows.

The main valleys provide relatively easy access to most parts of the Dolomites. The main north–south road uses the Campolongo Pass (6,152 feet [1,875 metres]). The east–west roads cross the well-known passes of Pordoi (7,346 feet [2,239 metres]), Falzarego (6,906 feet [2,105 metres]), Tre Croci (5,935 feet [1,809 metres]), Sella (7,404 feet [2,257 metres]), and Gardena (6,959 feet [2,121 metres]). The main centre of this tourist and mountain-climbing region is Cortina d’Ampezzo. Other resorts are Auronzo, San Martino di Castrozza, and Ortisei, with its narrow-gauge railway. On the western and southeastern margins, respectively, are located the larger towns of Bolzano and Belluno.

Most of the main peaks were first climbed in the 1860s and ’70s by English mountaineers. Landslides after heavy rainstorms in the southern Dolomites twice caused the Vaiont Dam (on a tributary of the Piave River) to overspill and drown the village of Longarone, causing the loss of more than 2,500 lives in 1963 and the destruction of houses and communications in 1966. In 2009 the Dolomites were inscribed on UNESCO’s World Heritage List.

The Editors of Encyclopaedia BritannicaThis article was most recently revised and updated by Michele Metych.