Cetina

Coordinates: 43°26′23″N 16°41′11″E / 43.4398°N 16.6864°E / 43.4398; 16.6864
Source: Wikipedia, the free encyclopedia.
Cetina
Cetina flows through rocky, karst terrain.
Location
CountryCroatia
Physical characteristics
Source 
 • locationDinara
Mouth 
 • location
Adriatic Sea
 • coordinates
43°26′23″N 16°41′11″E / 43.4398°N 16.6864°E / 43.4398; 16.6864
Length101 km (63 mi)[1]
Basin size1,463 km2 (565 sq mi)[1]

Cetina (pronounced [tsětina]) is a river in southern Croatia. It has a length of 101 km (63 mi) and its basin covers an area of 1,463 km2 (565 sq mi).[1] From its source, Cetina descends from an elevation of 385 metres (1,263 ft) above sea level to the Adriatic Sea. It is the most water-rich river in Dalmatia.[2]

Geography and geology

Cetina has its source in the northwestern slopes of

Sinj karst field, through the city of Sinj. After that it runs eastward, through the city of Trilj and then back westward around the Mosor mountain, before flowing into the Adriatic in the city of Omiš
.

Apart from its visible basin, the Cetina also receives a lot of water from the west Bosnian karst field via underground routes. Its lower course begins from the Gubavica Falls, at 49 metres (161 ft) above sea level, near the village of Zadvarje, 20 kilometres (12 mi) from Omiš. Here it leaves its canyon and flows into a valley which has nevertheless retained something of the appearance of a canyon.[2]

The latter portion of Cetina and its relatively large drop in elevation was used to build several substantial

hydroelectric power plants.[4]
Its water is also bottled as Cetina.

The total drainage area of the catchment is around 12,000 km2, and the annual discharge is around 105 m3s−1 as a consequence of a mean annual rainfall of 1380 mm.[3]

Bounded to the east by the

dolomitic limestone and flysch. The underlying karst geology controls relief with a series of structurally aligned basins separated by high ridges.[3]

Sinjsko polje.
Bottom row: Near Trilj. Canyon near Šestanovac. Mouth of the river at Omiš
.


History and archaeology

The Cetina Valley and the narrow passage at Klis have always functioned as a principal trade route between the Croatian coast and hinterland. Strategically, it has been pivotal to the development, not only of the Balkans, but also of significant parts of Europe.[3] The earliest evidence for agricultural activity is from the Early

Ruda rivers at Trilj.[3]

The area is intimately associated with the heartland of the

fortress at Tilurium (Gardun), just above today's city of Trilj, which guards the entrance to the valley from the south and the approach to the provincial capital at Salona.[3]

During the early

toponymic evidence suggests that the Cetina Valley and perhaps the river itself became a frontier between Slavic and Late Roman power. The area around Sinj eventually emerged as a centre of Slavic power and ultimately established itself as a heartland of the Early Croatian State,[3]
especially in the areas of its upper flow.

During later periods the area was highly contested and passed between a number of regional and local powers before conquest by the Ottoman Empire during the early 16th century. After this it retained a frontier role between Ottoman Empire and Republic of Venice until the reconquest of the area 150 years later.[3]

Today canyon of the river Cetina is very popular among tourists looking for adventure activities like rafting, canyoning, zip-line, rock climbing, kayaking and other outdoor activities.

References

  1. ^
    ISSN 1333-3305. Archived from the original
    (PDF) on 13 November 2018. Retrieved 23 May 2018.
  2. ^
  3. ^ .
  4. ^ Mrla, Domagoj (2019-09-25). Analiza rada termoelektrane i hidroelektrane na Peruči (bachelor thesis) (in Croatian). University of Zagreb. Faculty of Mechanical Engineering and Naval Architecture. pp. 14–22.
This page is based on the copyrighted Wikipedia article: Cetina. Articles is available under the CC BY-SA 3.0 license; additional terms may apply.Privacy Policy