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History of Croatia. Part of a series on the. History of Croatia. Early history. Middle Ages. Modernity. 20th century. Contemporary Croatia. Timeline. Croatia portal. v. t. e. At the time of the Roman Empire, the area of modern Croatia comprised two Roman provinces, Pannonia and Dalmatia.
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- Climate
- Plant and animal life
Croatia, country located in the northwestern part of the Balkan Peninsula. It is a small yet highly geographically diverse crescent-shaped country. Its capital is Zagreb, located in the north.
The present-day republic is composed of the historically Croatian regions of Croatia-Slavonia (located in the upper arm of the country), Istria (centred on the Istrian Peninsula on the northern Adriatic coast), and Dalmatia (corresponding to the coastal strip). Although these regions were ruled for centuries by various foreign powers, they remained firmly Western-oriented in culture, acquiring a legacy of Roman law, the Latin alphabet, and western European political and economic traditions and institutions. A part of Yugoslavia for much of the 20th century, Croatia suffered considerably from the disintegration of that federation in the early 1990s. The European trajectory of Croatia was finally realized in 2013 when it joined the European Union; in 2023 Croatia adopted the euro as its currency.
As the Croatian Canadian scholar Tony Fabijančić writes, Croatia’s tumultuous first years as an independent country also have obscured its centuries-long history:
Croatia (Hrvatska) is an ancient nation, yet a very young nation state. Once a formidable kingdom under Tomislav in the tenth century, a naval power in the sixteenth and seventeenth, and an awakening national entity in the nineteenth, it had to endure a thousand years of foreign meddling, subjugation, incursions, and outright wars before being recognized in 1992 as a distinct entity.
The upper arm of the Croatian crescent is bordered on the east by the Vojvodina region of Serbia and on the north by Hungary and Slovenia. The body of the crescent forms a long coastal strip along the Adriatic Sea, and the southern tip touches on Montenegro. Within the hollow of the crescent, Croatia shares a long border with Bosnia and Herzegovina, which actually severs a part of southern Croatia from the rest of the country by penetrating to the Adriatic in a narrow corridor.
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Croatia is composed of three major geographic regions. In the north and northeast, running the full length of the upper arm of the Croatian crescent, are the Pannonian and para-Pannonian plains. To the north of Zagreb, the Zagorje Hills, fragments of the Julian Alps now covered with vines and orchards, separate the Sava and Drava river valleys.
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To the west and south of the Pannonian region, linking it with the Adriatic coast, is the central mountain belt, itself part of the Dinaric Alps. The karst plateaus of this region, consisting mostly of limestone, are barren at the highest elevations; lower down, they are heavily forested. The highest mountain in Croatia, Dinara (6,007 feet [1,831 metres]), is located in the central mountain belt.
Of the 26 rivers that flow for more than 30 miles (50 km) in Croatia, the Sava and the Drava, coursing through the Pannonian and para-Pannonian plains, are of particular importance—both because of their length and because, along with the Kupa River, they are in large part navigable. The Sava originates in Slovenia, passes Croatia’s capital city of Zagreb, and then forms most of the border between Croatia and Bosnia and Herzegovina along the inside of the Croatian crescent. The Drava enters Croatia from Slovenia and forms all but a small section of the border with Hungary before joining the Danube, which in turn forms most of the border between Croatia and the Vojvodina province of Serbia. The Kupa, which forms part of the frontier between Slovenia and Croatia, and the Una River, which meanders along part of the border between Croatia and Bosnia and Herzegovina, both flow into the Sava. In Dalmatia the Krka and Cetina rivers are of particular importance because of their hydroelectric potential and because they flow into the Adriatic Sea.
In addition, a great deal of water circulates in underground rivers and pools in the karstic regions of the central mountain belt and the littoral. These waters account for many of the unique geologic formations and the picturesque landscape of central and western Croatia.
The Pannonian and para-Pannonian plains are enriched with alluvial soil deposited by the Sava and Drava rivers. These plains are the most fertile agricultural regions of Croatia and form the country’s breadbasket. The soil of the central mountainous belt is rather poor but offers some cultivable land in the fields and meadows and some grazing land ...
Two main climatic zones dominate Croatia. The Pannonian and para-Pannonian plains and the mountain regions are characterized by a continental climate of warm summers and cold winters. In the plains, temperatures average in the low 70s F (low 20s C) in June and in the low 30s F (around 0 °C) in January—although they can range from a low of −5 °F (−20 °C) in the winter to a high of 105 °F (40 °C) in the summer. The central mountain regions of Lika and Krbava have slightly cooler summers and cold winters, with a milder climate in the valleys. The average temperature range is between about 65 °F (about 18 °C) in June and the upper 20s F (about −2 °C) in January. Considerable rainfall, turning to snow in winter, is characteristic of the region.
The Dalmatian coast, Istria, and the islands have a mild Mediterranean climate. In southern Dalmatia, where the sirocco winds (known there as the jugo) bring a moderating influence from Africa, summers are sunny, warm, and dry, and winters are rainy. In the north the winters are drier and colder as a result of the cold northeast wind known as the bora (bura). In the summer the mistral wind has a cooling effect on the coast and the islands. The average temperature ranges from the low 40s F (about 5 °C) in January to the low 70s F (low 20s C) in June. Rainfall is moderate and occurs mainly in the winter.
Reflecting the country’s diverse geography, the flora and fauna of Croatia are highly varied. On the Dalmatian coast, grapes and olives are grown to produce wine and oil, while Istria is dominated by firs, and Slavonia has many oak forests. In terms of animal life, lizards are found on the coast, while wolves and even bears can be found in the inla...
Mar 14, 2021 · Early in the 7th century, a Slavic people called the Croats migrated to the area. At first, they settled in Dalmatia. However, in the 8th century, they expanded northwards and inland. Two separate Croatian states emerged, one by the coast, the other inland.
History of Croatia. The territory of Croatia bridges the central European and Mediterranean worlds, and its history has been marked by this position as a borderland. It lay near the division between the two halves of the Roman Empire and between their Byzantine and Frankish successors.
An independent Croatian state developed in the 9th century and was ruled by native kings until 1102, when the crown passed into the hands of the Hungarian dynasty. Some institutions of separate Croatian statehood were maintained, however.
Nov 29, 2022 · 29 November 2022. Getty Images. An aerial view of the Croatian capital, Zagreb. A chronology of key events: 1918 - Croatian national assembly votes to join the new Kingdom of Serbs, Croats and...
Timeline of Croatian history. This is a timeline of Croatian history, comprising important legal and territorial changes and political events in Croatia and its predecessor states. Featured articles are in bold. To read about the background to these events, see History of Croatia. See also the list of rulers of Croatia and years in Croatia .
