Zalaegerszeg, Hungary

Zalaegerszeg (Egersee in German, Jegersek or Jagersek in Croatian; common abbreviation: “Zeg”) is the seat of Zala County, a town with county status. As the center of the Zalaegerszeg district, many settlements belong to its catchment area. It is the 17th most populated city in Hungary.

Its first written mention dates from 1247 as Egurscug, and in 1293 it is already called Egerszeg.

After the fall of Kanizsa in 1600, its role grew, it gradually became the center of Zala County, and in today's terms it became a county seat in the 18th century. The prosperity of the city began in the 1920s, under the office of Mayor Mátyás Czobor, nearly 40 new streets were opened, a new public cemetery, a row of love houses and rental flats were built, and the public hospital was expanded. In 1929, Zalaegerszeg became a county town.

One of the most flowery, greenest cities in Hungary, in 2008 it won the highest prize of the Organizing Committee for a Flowery Hungary, the Golden Rose Prize.

 

Location

Geographical coordinates of Zalaegerszeg é. s. 46.84538 ° and k. h. 16.84721 °. It is the seat of Zala county, a city with county status. It is located in Western Transdanubia, on both banks of the river Zala, at approximately equal distances (50–70 km) from the Austrian, Slovenian and Croatian borders, in the Zala Hills region, on the edge of the Göcsej micro-region. It has an average elevation of 156 meters above sea level. Lake Balaton is 45 km east of it. Its distance from Budapest is 213 kilometers by road and 239 kilometers by rail. The nearest motorway exit is 50 km away, next to Nagykanizsa on the M7 motorway.

 

Its natural geographical features

The thickness of the earth's crust here is 25-27 km, that of the lithosphere 60-80 km. Throughout the history of the earth, marine and terrestrial sedimentation in the area have alternated during periods of ascent and descent. The most important event of the Pliocene age was the formation of gravel areas from river embankment. During the Pleistocene, loess covered large areas. Almost exclusively the youngest rocks are found on the surface, but upper Pannonian rocks can also appear on the valley bottoms.

The city is located in the northern part of the Zala Hills, on the border of three micro-regions. The south-western parts of the city already extend into the territory of Göcsej, so there are characteristic “mountains” of 200-250 meters high, with varying exposures. The north-eastern and eastern slopes are the steepest, descending to the south-southwest, gradually decreasing, formed by derasis and gel solifluction. The northern and central parts are located in the tectonically predicted and funnel-like widening to the east in the Upper Zala Valley. On the right side of the valley were deep, narrow valleys, hard-to-recognize terraces, Old Holocene sediments associated with Pannonian clay, and sloping, sloping slopes covered on the left. However, human activity has almost completely transformed them into more suitable forms for settlement. The eastern parts of the city stretch on smaller meridional lines connecting to the Söjtöri ridge of the East Zala Hills.

The duration of sunlight varies between 1950 and 2000 hours / year, which is the lowest value compared to Hungarian areas in the same latitude. This is due to the average annual cloud cover of 56-62% caused by the strength of the Atlantic impact. Among the wind directions, the most common are north and south, totaling approx. 30%, the meridional valleys help to maintain their direction. Windless periods are also common, about 25%.

The annual rainfall is around 800 mm. The average number of snow-covered days is 45.

 

In the clayey, clayey parts there are opportunities for the formation of a dense water network, which is one of the densest in Hungary. In this context, the valley density is also very high. The formation of the valleys was also facilitated by the loose surface rock and the Quaternary uplift of the area. However, the fragmentation of the topography is not conducive to the formation of large watercourses, so the largest one, Zala, is only in the vicinity of the stream-sized Zalaegerszeg. As the erosion base of the area, it collects water from smaller ditches. These include Válicka, which flows from the south to Zala. There are several small and large lakes in the city. The most significant is Lake Gébárti, artificially created in 1975. Pose in a part of town after the abandonment of gravel mines, fishing lakes were established.

Around Zalaegerszeg, there are two types of plant associations: the valleys are characterized by waterfront meadows, willow and alder groves. In the higher areas there are hornbeam and sessile oaks, Zala beeches, and oak trees, and the occurrence of sweet chestnuts is common. Within the city, only parks show the memory of the old rich forests. (Peace Park, Dózsa Park, Park Forest)

The livestock associated with the Zala flora is not different from the Hungarian average, it typically consists of large game (deer, roe deer, wild boar) and is home to few special animal species. This game is of economic importance, both for game meat and for hunting. The deer trophies of Zala are famous, they have already won several world championship medals.

Poor quality soils have developed around the city, the most significant of which are clay-washed brown forest soils. Due to this feature, large areas are utilized even within the city limits for vineyards, where more undemanding varieties are created.

 

History

Prehistory and Ancient Times
Archaeological evidence shows human presence in the area as far back as the Upper Paleolithic, with the oldest finds in Zala County coming from local excavations. Stone tools and other artifacts indicate early hunter-gatherer activity. The region was later inhabited by Celts before Roman influence reached nearby areas (though Zalaegerszeg itself has limited direct Roman ruins, evidence of Roman settlements exists in the broader vicinity).

Medieval Period (13th–15th Centuries): Founding and Growth
The first written records appear in 1247 (Egerscug) and 1293 (Egerszeg), referring to a settlement in the river angle. In 1266, King Béla IV donated the town to the Diocese of Veszprém, making it church property. Because it was distant from Veszprém, local oligarchs (such as the Kőszegi family) often diverted its taxes.
By the 14th century, Egerszeg was the largest settlement in the area. It briefly held royal town status (1368–1389) before Sigismund I transferred it to the Kanizsai family, who traded it back to the bishop of Veszprém; the Kanizsai retained ownership until 1848. A stone church was built in 1381, and in 1421 the town gained oppidum status (market town privileges: annual lump-sum taxes and the right to elect its own judge). Population grew rapidly, and by the early 16th century it was the de facto center of Zala Comitatus (county).

Ottoman Wars and Frontier Defense (16th–17th Centuries)
The Battle of Mohács (1526) and the Ottoman advance halted development. Local landowners raided the town in the 1530s amid weakened royal authority. From 1568, Egerszeg was fortified with a palisade castle to serve as a Habsburg border stronghold. The Ottomans first attacked in the late 1570s but failed to capture it permanently. After the fall of nearby Kanizsa to the Turks, Egerszeg’s strategic importance grew, though the castle was badly damaged in 1616 and briefly held by the Ottomans in 1664. The town endured repeated raids, plagues, and heavy taxes but was never permanently occupied by the Ottomans—unlike many other Hungarian settlements.

18th–Early 19th Century: County Seat and Baroque Development
In the 18th century, despite lying on the periphery of the comitatus, Egerszeg became the county capital—largely because county councils met there, it had gained importance during the Ottoman era, and it was not the private estate of a local lord. The Baroque County Hall (1730–1732) was the town’s first major building. In the 1760s, a large church and barracks were added. Most residents still lived in wooden houses vulnerable to frequent fires; stone construction became widespread only after 1826.
Economically, the town lagged because citizens paid taxes directly to the bishop. By the 1830s, about 10% of the (mostly Catholic) population was Jewish, but trade remained limited. Culturally and economically, Nagykanizsa and Keszthely overshadowed it. Zalaegerszeg played only a minor role in the 1848–49 Hungarian Revolution and War of Independence.

Late 19th–Early 20th Century: Modernization and Jewish Community
In 1870 the town temporarily lost its municipal status (becoming a village), but regained it on 31 May 1885. The village of Ola was annexed in 1887. The railway arrived in 1890 (Ukk–Csáktornya line), spurring growth. New buildings in the 1890s–1900s included a secondary school, town hall, hotel, nursery, and brick factory. A prominent local politician, József Farkas de Boldogfa, helped secure permission for the Zalaegerszeg Synagogue (completed 1904 in Baroque style), which served the growing Jewish community (first documented in the early 18th century).
The 1920s brought further prosperity: a new post office, railway station, fire department, police headquarters, Notre Dame monastery, and the synagogue’s full operation. The Jewish population reached about 1,221 by the 1940s (roughly 10–15% of the town at various points).

World War II and the Holocaust
Zalaegerszeg suffered relatively little physical destruction but catastrophic human loss. In 1944, the entire Jewish community—1,221 people—was deported to Auschwitz. The synagogue stood empty and damaged for decades afterward. The Red Army liberated the city on 28 March 1945 (some sources cite 29 March).

Communist Era (1945–1989): Industrialization and Revolution
In the 1949 local elections, the Communist Party received only about 10% of the vote but still took control. The 1950s transformed the town into an industrial center with a new textile factory and the 1952 discovery of oil (leading to a refinery and the later Museum of Oil Industry). Railway lines expanded. Housing shortages forced many residents to commute from villages; some “class enemies” were forcibly relocated.
The 1956 Hungarian Revolution reached Zalaegerszeg on 26 October. The local Communist leadership fled to Körmend, and a Revolutionary Council governed until Soviet troops arrived on 4 November. The 1960s–1970s saw explosive population growth through new apartment blocks and the absorption of nearby villages (Csácsbozsok, Botfa, Zalabesenyő, Bazita, Andráshida, Pózva). Expansion continues today toward Bocfölde and Bagod.
Zalaegerszeg hosted international events such as the 1983 World Orienteering Championships, reflecting growing cultural prominence.

Post-Communist Era (1989–Present)
Unlike many Hungarian cities, Zalaegerszeg weathered the post-Socialist economic transition relatively well and experienced dynamic development in the 1990s. The former synagogue was repurposed as a concert hall in the 1980s and later restored with a permanent exhibit on local Jewish history. The Göcsej Museum (with Paleolithic artifacts, Bronze Age finds, and ethnographic collections) and the adjacent open-air Göcsej Village Museum (30+ relocated traditional buildings, including a working water mill) preserve the region’s folk heritage. The city also maintains an Oil Industry Museum tied to its 1950s petroleum boom.
Today, Zalaegerszeg blends its medieval roots, Baroque landmarks (twin-spired parish church 1750–60, County Council House Chapel 1761–77), 19th–20th-century civic buildings, and modern infrastructure. It remains a regional center known for its thermal baths, cultural festivals, and proximity to the Slovenian and Austrian borders.