Bay of Kotor: Difference between revisions

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| Name: || '''Bay of Kotor, <br /> Boka Kotorska (sr)'''
| Name: || '''Bay of Kotor, <br /> Boka Kotorska (sr)'''
|-bgcolor="#FFFFFF"
|-bgcolor="#FFFFFF"
|Position: || [[Montenegro]]
|Position: || [[Montenegro]], [[Croatia]]
|-bgcolor="#FFFFFF"
|-bgcolor="#FFFFFF"
|Rivers: || [[Karst hydrology]], Sopot, Skurda <br />[[submerged sources]]
|Rivers: || [[Karst hydrology]], Sopot, Skurda <br />[[submerged sources]]
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'''Boka Kotorska''' (Bay of Kotor, Bocche di Cattaro) in western [[Montenegro]] is a winding [[Headlands and bays|bay]] on the [[Adriatic sea]].
'''Boka Kotorska''' (Bay of Kotor, Bocche di Cattaro) in western [[Montenegro]], at the border with [[Croatia]], is a winding [[Headlands and bays|bay]] on the [[Adriatic sea]].


The bay was considered by some to be Europe's southernmost [[fjord]]. In fact it is a submerged river [[canyon]] of the once called Bokeljska reka which run from the high mountain plateaux of [[Mount Orjen]]. Very intensive tectonics and karstification processes led to the disintegration of the river system. After heavy rain the famous waterfall of Sopot spring at [[Risan]] appears. The Bay is composed of several smaller broad gulfs, united by narrower channels, forming one of the finest natural harbours in [[Europe]].
The bay was considered by some to be Europe's southernmost [[fjord]]. In fact it is a submerged river [[canyon]] of the once called Bokeljska reka which run from the high mountain plateaux of [[Mount Orjen]]. Very intensive tectonics and karstification processes led to the disintegration of the river system. After heavy rain the famous waterfall of Sopot spring at [[Risan]] appears. The Bay is composed of several smaller broad gulfs, united by narrower channels, forming one of the finest natural harbours in [[Europe]].
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Since 1918, Boka Kotorska was part of the [[Kingdom of Serbs, Croats and Slovenes]] (renamed to [[Yugoslavia]] in 1929). Between 1918 and 1922 the region was a separate county administered from [[Kotor]], between 1922 and 1929 it was part of [[Zetska oblast]], and between 1929 and 1941 part of [[Zetska banovina]]. According to the 1921 census, Boka had 36,539 inhabitants, of whom 23,777 were Orthodox Christians and 12,342 Catholics.
Since 1918, Boka Kotorska was part of the [[Kingdom of Serbs, Croats and Slovenes]] (renamed to [[Yugoslavia]] in 1929). Between 1918 and 1922 the region was a separate county administered from [[Kotor]], between 1922 and 1929 it was part of [[Zetska oblast]], and between 1929 and 1941 part of [[Zetska banovina]]. According to the 1921 census, Boka had 36,539 inhabitants, of whom 23,777 were Orthodox Christians and 12,342 Catholics.


The region Boka Kotorska was occupied by fascist Italy in [[1941]], and since 1945, it is part of the Republic of [[Montenegro]].
The region Boka Kotorska was occupied by fascist Italy in [[1941]], and since 1945, it is part of the Republic of [[Montenegro]], except peninsula of [[Privlaka]] at the western side of the entrance in the bay, that is part of [[Croatia]].


Today, most of the inhabitants of the region are Orthodox Christian declaring themselves in census either as Serbs either as Montenegrins, while about 11% of its population is Catholic mostly declaring themselves as Croats.
Today, most of the inhabitants of the region are Orthodox Christian declaring themselves in census either as Serbs either as Montenegrins, while about 11% of its population is Catholic mostly declaring themselves as Croats.
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[[Category:Geography of Montenegro]]
[[Category:Geography of Montenegro]]
[[Category:Geography of Serbia and Montenegro]]
[[Category:Geography of Serbia and Montenegro]]
[[Category:Geography of Croatia]]


[[de:Bucht von Kotor]]
[[de:Bucht von Kotor]]

Revision as of 14:47, 25 May 2006

Map
Infos
Name: Bay of Kotor,
Boka Kotorska (sr)
Position: Montenegro, Croatia
Rivers: Karst hydrology, Sopot, Skurda
submerged sources
Destination: Sea
Settlements: Kotor, Herceg Novi,
Risan, Tivat,
Dobrota, Perast
Records: Biggest bay in the adriatic,
submerged river canyon
(Bokeljska reka)
Numbers
Water Area: 87 km²
Max depth: 60 m
Average depth: 27.3 m
Water content: 2412, 306 km³ (2,4 mrd m³)
Highest point: Orjen = 1894 m
Lowest point: Sea surface = 0 m
Length: 28,13 km
Widest point: 7 km
Narrowest point: 0.3 km
Hydrologic system: karst hydrology ca. 4000 km²
Shoreline: 107.3 km
Images

Boka Kotorska (Bay of Kotor, Bocche di Cattaro) in western Montenegro, at the border with Croatia, is a winding bay on the Adriatic sea.

The bay was considered by some to be Europe's southernmost fjord. In fact it is a submerged river canyon of the once called Bokeljska reka which run from the high mountain plateaux of Mount Orjen. Very intensive tectonics and karstification processes led to the disintegration of the river system. After heavy rain the famous waterfall of Sopot spring at Risan appears. The Bay is composed of several smaller broad gulfs, united by narrower channels, forming one of the finest natural harbours in Europe.

History

The close by hamlet of Risan (Risano), was a thriving Illyrian city of Rhizon as early as 229 BC, and gave its name to the Boka, then known as Rhizonicus Sinus. Rhizon submitted to Rome in 168 BC, at the same time Ascrivium, or Ascruvium, the modern Kotor (Cattaro), is first mentioned as a neighboring city.

Kotor itself has been fortified since the early Middle Ages, and was one of the more influential Dalmatian city-states throughout the period. It later passed to Bulgaria and then to Serbia, until becoming a semi-independent republic under the protectorate of medieval Serbian kings. Its merchant fleet and importance gradually increased, and after the fall of Serbia to the Ottoman Empire in the late 14th century, Kotor was seized by the Venetian Republic.

The Bokelj's had a very strong fleet, which counted as many as 300 ships in the 18th century. Boka was a rival to Dubrovnik and Venice.

At the beginning of the 19th century, the region of Boka Kotorska was included into Illyrian provinces, which were part of the French Empire. The region was later annexed by the Austrian Empire and was included into province of Dalmatia.

According to the 1818 data, Boka had 29,899 inhabitants, of whom 21,310 were Orthodox Christians and 8,589 Roman Catholics. In that time municipalities with Orthodox majority were Kotor, Risan, Grbalj, Budva, and Herzeg-Novi, while municipalities with Catholic majority were Dobrota, Prčanj, Stoliv, Kontada kotorska, and Perast.

The population of municipalities of Boka in 1900:

  • Budva = 5,526 Orthodox Christians, 1,537 Catholics
  • Herceg-Novi = 7,377 Orthodox Christians, 2,198 Catholics
  • Kotor = 7,617 Catholics, 7,207 Orthodox Christians
  • Risan = 4,020 Orthodox Christians, 1,385 Catholics

According to 1910 census, Boka had 40,582 inhabitants of whom 24,794 were Orthodox Christians, and 14,523 Catholics.

Since 1918, Boka Kotorska was part of the Kingdom of Serbs, Croats and Slovenes (renamed to Yugoslavia in 1929). Between 1918 and 1922 the region was a separate county administered from Kotor, between 1922 and 1929 it was part of Zetska oblast, and between 1929 and 1941 part of Zetska banovina. According to the 1921 census, Boka had 36,539 inhabitants, of whom 23,777 were Orthodox Christians and 12,342 Catholics.

The region Boka Kotorska was occupied by fascist Italy in 1941, and since 1945, it is part of the Republic of Montenegro, except peninsula of Privlaka at the western side of the entrance in the bay, that is part of Croatia.

Today, most of the inhabitants of the region are Orthodox Christian declaring themselves in census either as Serbs either as Montenegrins, while about 11% of its population is Catholic mostly declaring themselves as Croats.

Boka Kotorska region is under protection of UNESCO, due to its very rich cultural heritage. The region around the town of Kotor is situated in probably the most beautiful fjord in Europe. In 1979 there was an earthquake that destroyed or seriously damaged numerous cultural monuments.

Population

Most inhabitants of Boka are Serbs (41.89%) and Montenegrins (34.68%) with some Croats (7.61%). As a result of the assimilation, the population of the Croats began to diminish since Yugoslavia was created in 1918, and especially after the civil war in Croatia in 1991 (In 1910, the Croat population of Boka was 18.9%).

The three municipalities making up Boka Kotorska have a total population of 71,443 (2003 census):

  • Kotor = 23,481 (11,002 Montenegrins, 7,197 Serbs, 1,842 Croats)
  • Tivat = 13,991 (4,911 Serbs, 4,126 Montenegrins, 2,761 Croats)
  • Herceg-Novi = 33,971 (17,818 Serbs, 9,651 Montenegrins, 831 Croats)

Of this, 76% are Serb Orthodox and 11% are Catholics.

Ethnic groups in Boka

Serbs and Montenegrins

Slavic and Serb tribes settled in Boka Kotorska in the 7th century. The region was divided between Travunians (who were Serb tribe) and Docleans (for whom is not explicitly stated were they Serbs by origin, but later they are also considered to be Serbs).

When autonomous Serbian Orthodox Church was established in the 13th century, one of its first eparchies was established in Boka.

During the history, there were 3 Orthodox monasteries and 250 Orthodox churches in Boka, most of whom still exist.

Croats

The towns of Kotor, Perast, Tivat, Dobrota, Prčanj, Herceg-Novi and Budva had a Croatian majority in 1910. A large Catholic majority in 1910 had peninsula Vrmac and southern part of Spich (from Sutomore to the border between Boka Kotorska and Montenegro near the town of Bar).

For example, the number of Croats in Kotor dropped from 69% in 1910 to 7% in 1991; in Herceg-Novi from 70% to 2%; in Tivat from 95% to 23%.

In 1991 there were 8% of Croats in Boka Kotorska region, and in 2003 the percent of Croats was 7.61%.

The Bokelj Marine 809 (Bokeljska mornarica 809) is a confraternity whose aim is to preserve Croat maritime tradition. In 809 the remains of St. Tripun were brought by Croat mariners from Asia Minor to Kotor. The Cathedral of St. Tripun in Kotor is the oldest Croat cathedral in this area built by Croats in 1166.

It is worth mentioning that the new Yugoslavia (consisting of Serbia and Montenegro) participated at the international maritime exhibition EXPO'98 in Lisbon, Portugal, by displaying the cultural and maritime heritage of Boka Kotorska. The display did not mention the Croats in Boka Kotorska.

The town of Perast had extremely difficult moments in 1654 when the attacks of the Turks were especially dangerous. Their brave and successful defense of Boka was the reason of the arrival of Petar Zrinski, a famous Croatian statesman, who also had numerous dramatic battles with the Turks. During his three day sojourn in Perast he presented his legendary sword to the town, as the sign of his recognition to their efforts to defend their homeland, and to stop the approach of the Ottoman Empire to Middle Europe.

Geography

Historic map of the Bay, 16th century

The outermost gulf is the gulf of Tivat (Teodo), and a small naval port. On the seaward side, there is the gulf of Herceg Novi (Castelnuovo), which guards the main entrance to Boka. The inner gulfs are the gulf of Risan to the northwest and the gulf of Kotor to the southeast.

On the landward side, the long walls running from the fortified old town of Kotor to the castle of Saint John, far above, formed a striking feature in the landscape; and the heights of the Krivošije (Krivoscie), a group of barren plateaux in Mount Orjen, were crowned by small forts.

There are many interesting places on the shores of the Boka Kotorska. Herceg Novi has an Orthodox convent of St. Sava nearby (monastiry Savina), standing amid beautiful gardens. It was founded in the 16th century, and contains many fine specimens of 17th century silversmith work. There is a Benedictine monastery on a small island opposite to Perast (Perasto), eight miles east of Herceg Novi. Perast itself was for a time an independent state in the 14th century.

Climate

Meteorological station on Orjen in the hinterland of the Bay

The Bay of Kotor lies within the Mediterranean subtropical belt. While summers are hot and sunny, autumn, winter and spring are rainy seasons. It is the climate type of the Mediterranean but modifications exist in the vast region. A peculiarity of the littoral Dinarids is the precipitation regime as at the Bay of Kotor, Mt. Orjen receives Europe's' most heavy precipitation. Like the monsoon rain is seasonally distributed, thus November thunderstorms sometimes pour 2000 l of water in several days, while August is frequently completely dry leading to forest fires. With a maximum discharge of 200 m³/sec water one of the biggest karst springs, the Sopot spring, is a remarkable indicator of this seasonality. Most of the time it is inactive but after heavy rain a remarkable waterfall appears 20 m above the Bay of Kotor.

Station Height [m] Type Character Precipitation [mm] Snow
Zubacki kabao 1894 D perhumid Mediterranean snowclimate ca. 6250 ap. 140 days
Crkvice 940 Cfsb (fs= without summerdryness), perhumid Mediterranean mountain climate 4926 70 days
Risan 0 Cs’’a (s’’= double winter rain season), perhumid Mediterranean coast climate 3500 2 days

* classification scheme after Köppen

Two wind systems are noteworthy for their ecological significance: Bora and Scirocco. Strong cold downslope winds of Bora type appear in winter and are most severe in the Bay of Risan. Gusts reach 250 km/h and can lead to a significant fall of temperatures in several hours with freezing events problematic for most of the Mediterranean cultures. Bora weather situations are frequent and sailors keep an eye on the mountains as cap clouds indicate an eminent Bora event. Scirocco is a warm humid rain and is important as it brings heavy rain. It appears throughout the year but is usually centered in autumn and spring.

Station Period Height [m] I II III IV V VI VII VIII IX X XI XII I-XII [mm/m²a]
Herceg Novi 1961-1984 40 230 221 183 135 130 73 28 45 160 181 326 262 1974
Risan 1961-1984 40 405 342 340 235 153 101 66 123 188 295 423 434 3105
Grahovo 1961-1984 710 351 324 305 251 142 94 55 103 202 416 508 473 3224
Podvrsnik 1961-1984 630 407 398 367 305 151 101 77 132 238 465 593 586 3820
Vrbanje 1961-1984 1010 472 390 388 321 181 104 70 122 224 369 565 536 3742
Knezlaz 1961-1984 620 547 472 473 373 207 120 72 136 268 400 629 661 4358
Crkvice 1961-1984 940 610 499 503 398 198 135 82 155 295 502 714 683 4774
Ivan. Korita 1960-1984 1350 434 460 742 472 128 198 74 46 94 300 694 972 4614
Goli vrh 1893-1913 1311 271 286 307 226 188 148 75 70 215 473 415 327 3129
Jankov vrh 1890-1909 1017 424 386 389 346 212 124 55 58 202 484 579 501 3750
Cetinje 1961-1984 655 434 357 367 288 164 92 72 118 209 306 489 498 3394
Grab-Zubci 1934-1960 677 333 325 257 195 183 83 59 86 173 360 447 485 2985
Trebinje 1931-1960 276 193 190 160 102 119 70 43 76 110 239 247 249 1762
Dubrovnik 1931-1960 49 147 113 102 92 79 60 24 38 97 156 213 186 1307

* monthly and yearly precipitation ranges in Dalmatia, Herzegovina and Montenegro

Gallery

Literature

  1. Prof. Lazo M. Kostić, O srpskom karakteru Boke Kotorske, Herceg Novi, 1994.
  2. Vasko Kostić, Svetosavska ozarenost nevjeste Jadrana, Kult Svetog Save u Boki, Novi Sad, 1999.

External links