Požega Valley on a map of Croatia
|• Total||1,249 km2 (482 sq mi)|
|• Density||49/km2 (130/sq mi)|
|a Požega Valley is not designated as an official region, it is a geographic region only. |
b The figure is an approximation based on the territorial span and population of the municipalities bounded by Psunj, Papuk, Krndija, Požeška Gora and Dilj mountains and hills.
The Požega Valley (Croatian : Požeška kotlina) is a geographic microregion of Croatia, located in central Slavonia, encompassing the eastern part of the Požega-Slavonia County. It is located in the Pannonian Basin, bounded by Psunj, Papuk and Krndija mountains from west and north, and Požeška Gora and Dilj from south and east, as the Pannonian plain is interspersed by horst and graben structures. The largest settlement in the region is the city of Požega, followed by Pleternica and Kutjevo. The main watercourse in the region is Orljava River. The region covers 1,249 square kilometres (482 square miles) and has a population of 60,599.
The Požega Valley was first inhabited in the prehistoric era, with archaeological finds spanning the Neolithic to classical antiquity and the Early Middle Ages, the period to which the oldest surviving historical records of the region date. Between the 13th and the 16th centuries, the region was organized as the centre of the Požega County and a royal estate. Ottoman rule in the region lasted for about 150 years—from the 1530s to the 1680s. During that time, the area was the centre of Sanjak of Pojega. Subsequently, the city of Osijek became the administrative and military centre of the newly formed Kingdom of Slavonia from Požega.
The Požega Valley is a geographic microregion of Croatia, located in central Slavonia, enveloped by the Slavonian mountains. 984-metre (3,228 ft) Psunj, 953-metre (3,127 ft) Papuk, and 792-metre (2,598 ft) The Krndija mountains, the northern slopes of 618-metre (2,028 ft) Požeška Gora and 461-metre (1,512 ft) the Dilj hills, and lowland is surrounded by the mountains and hills—occupying the eastern part of Požega-Slavonia County.It consists of southern slopes of
The main watercourse in the region is the 89 kilometres (55 miles) long Orljava River, rising in Psunj, flowing along the southern rim of the valley through Požega and Pleternica before leaving the valley through a gap between Požeška Gora and Dilj near its confluence with the Sava River. It receives water from numerous smaller watercourses— Londža is the most significant. The region, as with most of Croatia, enjoys a moderately warm and rainy continental climate as defined by the Köppen climate classification.
The region encompasses three cities — Kutjevo, Pleternica and Požega —and five municipalities — Brestovac, Čaglin, Jakšić, Kaptol and Velika. The largest settlement in the region is the city of Požega, with an urban population of 19,506. The region's 1,249 square kilometres (482 square miles) supports a population of 60,599, with a population density of 48.518/km2 (125.66/sq mi).
|City or municipality||Area||Population|
|Brestovac||279 km2 (108 sq mi)||3,726|
|Čaglin||180 km2 (69 sq mi)||2,723|
|Jakšić||44 km2 (17 sq mi)||4,058|
|Kaptol||85 km2 (33 sq mi)||3,472|
|Kutjevo||174 km2 (67 sq mi)||6,247|
|Pleternica||198 km2 (76 sq mi)||11,323|
|Požega||134 km2 (52 sq mi)||26,248|
|Velika||155 km2 (60 sq mi)||5,607|
|TOTAL||1,249 km2 (482 sq mi)||63,404|
|Note: All the cities and municipalities are a part of the Požega-Slavonia County.|
Sources: Croatian Bureau of Statistics, Spatial plan of the Požega-Slavonia County
The Požega Valley is entirely located in the Pannonian Basin, one of three major geomorphological parts of Croatia. – 12 Mya (million years ago) and intensified subsidence observed until 5 Mya as well as flood basalts about 7.5 Mya.The Pannonian Basin took shape through Miocenian thinning and the subsidence of crust structures formed during Late Paleozoic Variscan orogeny. The Paleozoic and Mesozoic structures are visible in the mountains and hills surrounding the valley. The processes also led to the formation of a stratovolcanic chain in the basin 17
Contemporary uplift of the Carpathian Mountains prevented water flowing to the Black Sea, and the Pannonian Sea formed in the basin. Sediments were transported to the basin from the uplifting of the Carpathian and Dinaric mountains, with particularly deep fluvial sediments deposited during the Pleistocene with the uplift of the Transdanubian Mountains. 3,000 metres (9,800 feet) of the sediment was deposited in the basin, and the Pannonian Sea eventually drained through the Iron Gate gorge. In the southern Pannonian Basin, the Neogene to Quaternary sediment depth is normally lower, averaging 500 to 1,500 metres (1,600 to 4,900 feet).Ultimately, up to
The results of those processes are large plains in eastern Slavonia, Baranya and Syrmia, as well as in river valleys. The plains are interspersed by horst and graben structures, which are believed to have broken the Pannonian Sea surface as islands.[ citation needed ] Psunj, Papuk and Krndija consist mostly of Paleozoic rocks that are 350 – 300 million years old. Požeška Gora and Dilj consist of much more recent Neogene rocks, but Požeška Gora also contains Upper Cretaceous sediments and igneous rocks forming the main 30-kilometre (19 mi) ridge of the hill and representing the largest igneous landform in Croatia. A smaller igneous landform is also present on Papuk, near Voćin. The two mountains are possible remnants of a volcanic arc related to Alpine orogeny —uplifting of the Dinaric Alps.
The Požega Valley has been inhabited since prehistory, as confirmed by remnants of Neolithic Starčevo culture discovered near Požega, as well as Copper and Iron Age finds discovered in areas of Požega, Jakšić and Kaptol. : Vallis Aurea, Croatian : Zlatna dolina), and the name is still affectionally used. Finds dated to the Early Middle Ages include 9th-century Avar and Slavic culture items and a 12th-century Benedictine abbey in Rudine at the foot of Psunj. Rudine represents the most important early medieval archaeological find in the region, and items found there include a glagolitic inscription dated to 1129.The valley was the site of the Roman city of Incerum, thought to have been located in an area between present-day Požega and Velika, where remnants of a Roman villa and graves have been found. The Romans called the valley Golden Valley (Latin
Historic records from 1210 describe the region as a part of Požega County and the medieval Kingdom of Croatia, with Požega as the county seat, a fortress (1227) and a royal estate belonging to queens of Hungary.In the 13th and 14th centuries, Franciscans and Dominicans established abbeys in Požega. Cistercians established an abbey in Kutjevo and initiated the region's winegrowing and winemaking traditions. The Cistercian wine cellar in Kutjevo has continuously supported winemaking since it was completed in 1232, making it the oldest continuously-operated winery in Croatia. In the early 13th century, the capitulum of the Roman Catholic Diocese of Pécs was established in Kaptol, containing a public archive of the region. The archive operated until 1536, when it was evacuated to Hungary ahead of the Ottoman army. The archive was returned to the Croatian State Archives in 1960.
Following the Battle of Mohács, the Ottomans expanded their possessions in Slavonia by seizing Đakovo in 1536 and Požega in 1537. In 1540, as Osijek came under Ottoman control, regular administration in Slavonia was introduced by the establishment of the Sanjak of Pojega. Ottoman control in Slavonia expanded and by 1552 conquest was complete.During the Great Turkish War (1667–1698), the Ottomans abandoned the region in 1687 and finally liberated in 1689 when Luka Ibrišimović led a revolt in Požega. Subsequently, as Požega County was restored in the region, Osijek became the administrative and military centre of the newly formed Kingdom of Slavonia, unseating Požega.
Following the Croatian–Hungarian Settlement of 1868, the kingdoms of Croatia and Slavonia were united as the Kingdom of Croatia-Slavonia.After Austria-Hungary occupied Bosnia and Herzegovina following the 1878 Treaty of Berlin, the Croatian and Slavonian Military Frontier territory returned to Croatia-Slavonia in 1881, pursuant to provisions of the settlement, removing the region from the immediate frontier of Croatia.
On 29 October 1918, the Croatian Sabor declared independence and joined the newly formed State of Slovenes, Croats and Serbs,which in turn entered into union with the Kingdom of Serbia on 4 December 1918 to form the Kingdom of Serbs, Croats, and Slovenes. The new kingdom abolished traditional subdivisions of Croatia, including Požega County, in 1922 when oblasts were introduced, succeeded by the banovinas of Yugoslavia. The Cvetković–Maček Agreement of 1939 created the autonomous Banovina of Croatia, incorporating the region. In April 1941, Yugoslavia was occupied by Germany and Italy. Following the invasion the region was incorporated into the Independent State of Croatia, a Nazi-backed puppet state as a zone under German occupation for the war's duration. Armed resistance soon developed in the country, and by 1942, controlled substantial territories, especially in Slavonia's mountains. After World War II, the region became a part of the Socialist Croatia within the Communist Yugoslavia.
In the 1980s the political situation in Yugoslavia deteriorated.In 1990 the Communist Party fragmented along national lines. That same year, the first multi-party elections were held in Croatia, with Franjo Tuđman's win exacerbating nationalist tensions. The Serbs in Croatia, intent on achieving independence from Croatia, declared the autonomy of areas that became the unrecognized Republic of Serbian Krajina. As tensions rose, Croatia declared independence, effective 8 October 1991. The Croatian War of Independence began when the Yugoslav National Army and various Serb paramilitaries attacked Croatia. By the end of 1991, a high intensity war fought along a wide front reduced government control to about two-thirds of its historic territory. Western Slavonia was occupied in August 1991, following an advance by the Yugoslav forces north from Banja Luka across the Sava River cutting the primary communication route to the nation's capital. This was partially pushed back by the Croatian Army in operations named Otkos 10 and Orkan 91 that established a front line around Okučani and south of Pakrac. The line held virtually unchanged for more than three years until Operation Flash in May 1995 when full access to the region was restored.
Croatia, officially the Republic of Croatia, is a country at the crossroads of Central and Southeast Europe on the Adriatic Sea. It borders Slovenia to the northwest, Hungary to the northeast, Serbia to the east, Bosnia and Herzegovina and Montenegro to the southeast, and shares a maritime border with Italy to the west and southwest. Its capital and largest city, Zagreb, forms one of the country's primary subdivisions, with twenty counties. Croatia has 56,594 square kilometres and a population of 4.07 million.
The Geography of Croatia is defined by its location—it is described as a part of Central Europe and Southeast Europe, a part of the Balkans and Mitteleuropa. Croatia's territory covers 56,594 km2 (21,851 sq mi), making it the 127th largest country in the world. Bordered by Bosnia and Herzegovina and Serbia in the east, Slovenia in the west, Hungary in the north and Montenegro and the Adriatic Sea in the south, it lies mostly between latitudes 42° and 47° N and longitudes 13° and 20° E. Croatia's territorial waters encompass 18,981 square kilometres (7,329 sq mi) in a 12 nautical miles wide zone, and its internal waters located within the baseline cover an additional 12,498 square kilometres (4,826 sq mi).
Slavonia is, with Dalmatia, Croatia proper and Istria, one of the four historical regions of Croatia. Taking up the east of the country, it roughly corresponds with five Croatian counties: Brod-Posavina, Osijek-Baranja, Požega-Slavonia, Virovitica-Podravina and Vukovar-Syrmia, although the territory of the counties includes Baranya, and the definition of the western extent of Slavonia as a region varies. The counties cover 12,556 square kilometres or 22.2% of Croatia, inhabited by 806,192—18.8% of Croatia's population. The largest city in the region is Osijek, followed by Slavonski Brod and Vinkovci.
Požega is a city in western Slavonia, eastern Croatia, with a total population of 26,248. It is the administrative center of the Požega-Slavonia County.
Bjelovar-Bilogora County is a county in central Croatia.
Vukovar-Syrmia County, Vukovar-Sirmium County or Vukovar-Srijem County is the easternmost Croatian county. It includes the eastern parts of the region of Slavonia and the western parts of the region of Syrmia, as well as the lower Sava river basin, Posavina and Danube river basin Podunavlje. Due to the overlapping definitions of geographic regions, division on Slavonia and Syrmia approximately divides the county vertically into north-west and south-east half, while division on Posavina and Podunavlje divides it horizontally on north-east and south-west half.
Požega-Slavonia County is a Croatian county in western Slavonia. Its capital is Požega. Its population was 78,034 as of the 2011 census.
The Sava is a river in Central and Southeast Europe, a right tributary of the Danube. It flows through Slovenia, Croatia and along its border with Bosnia and Herzegovina, and finally through Serbia, feeding into the Danube in its capital, Belgrade. The Sava forms the main northern limit of the Balkan Peninsula, and the southern edge of the Pannonian Plain.
The Pannonian Sea was a shallow ancient sea, where the Pannonian Basin in Central Europe is now. The Pannonian Sea existed during the Miocene and Pliocene epochs, when a 3–4 km (1.9–2.5 mi) depth of marine sediments were deposited in the Pannonian Basin.
Velika is a village and a municipality in the Požega Valley in Slavonia.
Krndija is a mountain in Slavonia, Croatia, extending eastwards from Papuk. It is located south of Orahovica and Našice and north of Požega.
Papuk is the largest mountain in the Slavonia region in eastern Croatia, near the city of Požega. It extends between Bilogora to the northwest, Krndija to the east, and Ravna gora and Psunj to the southwest.
Požeška gora,, is a mountain located south of Požega, Croatia in the region of central Slavonia. The mountain is a part of Slavonian mountains enveloping the Požega Valley, located adjacent to Psunj to the east of Požeška gora, and to the west of Dilj. Požeška gora and Dilj are separated by a gap through which Orljava River flows south out of the Požega Valley. The highest peak of the mountain is Kapavac, 618 metres above sea level.
Operation Swath-10 was a military offensive undertaken by the Croatian Army against the SAO Western Slavonia Territorial Defense Forces on Bilogora Mountain in western Slavonia. Occurring from 31 October to 4 November 1991, during the Croatian War of Independence, the operation was a Croatian victory and its success set the stage for follow-up advances by Croatian forces on Papuk Mountain in Operation Papuk-91 in late November and December. By the end of the year the HV gained control of Papuk, securing transport routes between eastern Slavonia and the rest of Croatia.
Operation Hurricane-91 was a military offensive undertaken by the Croatian Army against the Yugoslav People's Army and SAO Western Slavonia Territorial Defense Forces in the Sava River valley, in the region of Western Slavonia during the Croatian War of Independence. The operation began on 29 October 1991 and ended on 3 January 1992 when a nationwide ceasefire was signed to implement the Vance plan. The offensive was aimed at recapturing the region, in conjunction with two other HV offensives launched against SAO Western Slavonia in the north of the region within days.
Negoslavci is a village and a municipality in Vukovar-Syrmia County in eastern Croatia. It is located south of the town of Vukovar, seat of the county. Landscape of the Negoslavci Municipality is marked by the Pannonian Basin plains and agricultural fields of corn, wheat, common sunflower and sugar beet.
Croatia proper is one of the four historical regions of the Republic of Croatia, together with Dalmatia, Slavonia, and Istria. It is located between Slavonia in the east, the Adriatic Sea in the west, and Dalmatia to the south. The region is not officially defined, and its borders and extent are described differently by various sources. In contemporary geography, the terms Central Croatia and Mountainous Croatia are used to describe most of this area, the former referring to the northeastern part and the latter to the southwestern part; the far western part is known as the Croatian Littoral. Croatia proper is the most significant economic area of the country, contributing well over 50% of Croatia's gross domestic product. The capital of the Republic of Croatia, Zagreb, is the largest city and most important economic centre in Croatia proper.
The Pannonian island mountains is a term for isolated mountains scattered across the Pannonian Plain, chiefly its western and southern parts, in Hungary, Serbia and Croatia. In prehistoric times, these mountains were islands of the ancient Pannonian Sea that disappeared about 600,000 years ago.
Orljava is a river in Slavonia, eastern Croatia, a left tributary of Sava. It is 87.6 kilometres (54.4 mi) long and its basin covers an area of 1,618 square kilometres (625 sq mi).
Topography of Croatia is defined through three major geomorphological parts of the country. Those are the Pannonian Basin, the Dinaric Alps, and the Adriatic Basin. The largest part of Croatia consists of lowlands, with elevations of less than 200 metres above sea level recorded in 53.42% of the country. Bulk of the lowlands are found in the northern regions of the country, especially in Slavonia, itself a part of the Pannonian Basin plain. The plains are interspersed by the horst and graben structures, believed to break the Pannonian Sea surface as islands. The greatest concentration of ground at relatively high elevations is found in Lika and Gorski Kotar areas in the Dinaric Alps, but such areas are found in all regions of Croatia to some extent. The Dinaric Alps contain the highest mountain in Croatia—1,831-metre (6,007 ft) Dinara, as well as all other mountains in Croatia higher than 1,500 metres. Croatia's Adriatic Sea mainland coast is 1,777.3 kilometres long, while its 1,246 islands and islets encompass further 4,058 kilometres of coastline—the most indented coastline in the Mediterranean. Karst topography makes up about half of Croatia and is especially prominent in the Dinaric Alps, as well as throughout the coastal areas and the islands.