Kula (District)

Kula district is located in the eastern part of Manisa Province, within the Inner Western Anatolia region of the Aegean Region. The district is known for its volcanic structure and geological features, situated in an area historically called Katakekaumene (Burnt Land). Kula is a settlement where agriculture, animal husbandry, and small-scale industrial activities are carried out.

Kula (District) - (Anadolu Agency)

History

Kula district, affiliated with Manisa Province, has been under the rule of various civilizations throughout its historical development and is one of the settlements with a deep-rooted past. In antiquity, it was known as Katakekaumene (Burnt Land). Ancient authors, including the Amasya geographer Strabo, provided detailed descriptions of the region’s ash-covered terrain, black rock formations, and volcanic centers. These volcanic formations and lava flows continue to define Kula’s distinctive geography today.

Although the early settlement history of Kula cannot be definitively established, ancient sources refer to the region by names such as Koloe, Opsukion, Clanudda, Katake, and Kamene. These names reflect the area’s history under the dominion of Ancient Lydia, Persia, Hellenistic, Roman, and Byzantine powers. However, archaeological evidence revealing urban structures from these periods remains limited. Historical records indicate that during the Byzantine era, Kula lay within the boundaries of the Opsikion Theme, one of the administrative-political units of Anatolia. Established in the 7th century, the Opsikion Theme was divided into two separate administrative regions by the 9th century. Byzantine historians such as Pachymeres noted that Kula was a fortified position frequently changing hands between Byzantine and Turkish forces.

The region came under Turkish rule in the early 14th century during the period of the Germiyanids. Historical records state that after the death of Germiyanid ruler I. Yakup Bey, his son Mehmet Bey recaptured Kula from the Catalan forces and incorporated it into the beylik. A stone endowment deed issued by Germiyanid II. Yakup Bey explicitly states that Kula was endowed as territory “recovered from the infidels.” In the final period of the Germiyanid Beylik, Süleyman Şah formed an alliance with the Ottomans due to political conflicts with the Karamanids, marrying his daughter Devlet Hatun to Yıldırım Bayezid to establish a familial bond. As part of the dowry, Süleyman Şah ceded Kütahya, Tavşanlı, Simav, and Emet to the Ottomans, relocated to Kula, and made it the capital of the beylik. He died in Kula in 1388 and was buried in the Gürhane Medrese he had built there.

Ottoman rule began during the reign of Yıldırım Bayezid. After the Battle of Ankara in 1402, the territories of the Germiyanid Beylik were temporarily returned to II. Yakup Bey with Timur’s support. However, in accordance with II. Yakup Bey’s will in 1429, the Germiyanid lands were permanently annexed to the Ottoman State. During this period, Kula became a kaza (subdistrict) under the Sanjak of Kütahya. In the 19th century, upon the proposal of the governor of İzmir, Kula was attached to the Sanjak of Saruhan in 1852.

During the Ottoman period, Kula developed into an important industrial and commercial center. It reached advanced levels in crafts such as textiles, pottery, carpet weaving, and shoemaking, with its economic structure defined by these production-based activities. The municipal organization was among the earliest established within the Ottoman Empire’s borders; sources vary on its founding year, citing either 1866 or 1877. Municipal services continuously expanded, with basic infrastructure projects such as pavement laying, road construction, and street lighting implemented. The first municipal building was constructed in 1903 on Yeni Hamam Street.

Electricity was first supplied to the district between 1924 and 1926 using diesel generators, later sourced from the Kula Textile Factory. In 1937, the first scientific slaughterhouse was built by the municipality. Kula’s water network was completed in 1954, providing the population with safe drinking water. Municipal services moved to a new building in 1963 and operated from various facilities over time to meet changing needs. Today, services are provided from a modern municipal building.

With the establishment of the Republic, significant transformations occurred in Kula’s political and administrative structure. During the Greek occupation following World War I, the district was occupied on 28 June 1920 and was liberated on 4 September 1922 following the Turkish army’s victory, subsequently integrated into the administration of the Republic of Türkiye.

Geographical Features

Kula district is located in the eastern part of Manisa Province, within the Inner Western Anatolia region of the Aegean Region. Its geographical coordinates lie between 38°53′ north latitude and 28°68′ east longitude, at an elevation of approximately 720 meters above sea level. The district covers an area of 917 km², accounting for approximately 6.95% of Manisa Province’s total area. Kula is bordered by Eşme district of Uşak to the east, Salihli to the west, Demirci and Selendi to the north, and Alaşehir to the south. Its strategic location along the İzmir-Ankara State Highway (D300), a major transportation corridor connecting the Aegean Region to Central Anatolia, enhances its strategic importance.

The district generally features a mountainous and rugged topography. Areas south of Divlit Mountain and surrounding volcanic hills reinforce this geographical character. Kula is built upon one of Türkiye’s youngest volcanic regions and possesses a highly dynamic geological structure. The soils of the district exhibit great diversity as a result of volcanic activity and long-term geological processes, primarily shaped by basaltic lava flows and tuff layers.

The fairy chimneys prevalent in the Kula region were formed by the erosion of Miocene, Pliocene, and Quaternary-aged sediments by the Gediz River and its tributaries. These geomorphological formations are defining elements of the district’s unique natural landscape and lie within the volcanic area known as Katakekaumene (Burnt Land). This area holds significant potential not only geologically but also in terms of tourism, education, and geoheritage.

The high plateaus within the district generally decrease in elevation from east to west. Among these plateaus, Ulucak, Şehitler, and Encekler are the most prominent. The Gediz River, along with the Selendi, Söğüt, and Hacılar streams, constitute the main watercourses of the district. Although river flows diminish during summer months, increased winter rainfall ensures strong and sustained flow during colder seasons.

In terms of climate, Kula lies in a transitional zone between Mediterranean and continental climate types. Its high elevation and distance from the sea result in a pronounced continental character. This climatic structure directly influences the natural vegetation. The region features a mosaic of maquis and shrubland formations dominated by light-loving, drought-resistant hard-leaved plant species, interspersed with forested areas.

Soil composition is highly varied. Alluvial soils are common in the district center and along river courses, while basaltic soils predominate in the northern and western areas. Wider areas are covered by calcareous brown forest soils and rendzina-type Mediterranean soils. This diversity enhances the district’s agricultural potential and natural vegetation.

Geologically, Kula lies within the Anatolid Belt, one of Anatolia’s major tectonic zones. The district contains rock formations of various ages and origins, from the Precambrian to the present. Metamorphic and crystalline structures belonging to the Menderes Massif are overlain by Pliocene and Quaternary volcanic rocks, creating a broad geological diversity. Kula’s volcanic rocks, represented by basalt, tuff, and agglomerates, are young formations indicating three main phases of volcanic activity occurring in different periods.

Demographic Structure

Kula district, located in the eastern part of Manisa Province, had a total population of 43,361 as of 2023. With an area of 917 km², the district’s average population density is approximately 44.2 persons/km². This figure is below the provincial average of 110.62 persons/km², reflecting the district’s rural character and relatively sparse settlement pattern.

Kula district’s median age is 42.20, higher than Türkiye’s national median of 34.00 and close to Manisa Province’s median of 37.33. This indicates a relatively older population. When examining dependency ratios by age group, the child dependency ratio is 23.78% and the elderly dependency ratio is 22.63%. The total dependency ratio stands at 46.42%, consistent with the averages for Manisa Province (46.99%) and Türkiye (46.34%).

The district’s population structure has remained relatively stable over the years, but the decline in the youth population and relative increase in the elderly population signal a demographic transition. This trend is associated with declining fertility rates, rural-to-urban migration, and the movement of young people toward large cities.

Economic Structure

The economy is largely based on agriculture, animal husbandry, and to a lesser extent tourism, preserving the district’s rural character. Trade, the service sector, and small-scale industry also serve as complementary economic components.

Agriculture

Kula district possesses significant agricultural production potential. According to TÜİK data from 2011–2019, 35,563 hectares are used for agricultural activities. Of this land, 81.6% is dedicated to cereal production, 5.13% to vegetables, and 13.81% to fruits. The volcanic terrain significantly influences Kula’s agricultural output; the mineral richness of volcanic soils enhances the productivity of certain fruits and vegetables.

Cereal Production

Cereal farming forms the backbone of Kula’s economy. In 2019, a total of 161,404 tons of cereals were produced. Major cereal crops include maize (for silage), fava beans (yeşilot), barley, and durum wheat. Fava beans and durum wheat hold notable shares in both Manisa and national production. For instance, Kula contributes 62% of Manisa’s fava bean production and 6.36% of Türkiye’s total. Similarly, in sesame seed production, Kula accounts for 45.71% of Manisa’s output and 9.24% of Türkiye’s total.

Vegetable Production

Vegetable cultivation, though more limited than cereal production, plays a significant role in the district’s economy. In 2019, 35,922 tons of vegetables were produced. The most prominent vegetables include watermelon (14,149 tons), processing tomatoes (4,677 tons), table tomatoes (4,651 tons), and cantaloupe (3,695 tons). Kula also holds notable shares in national and provincial production of cauliflower, pickling cucumbers, fresh broad beans, and spinach.

Fruit Production

Fruit production is another important component of Kula’s economy. According to 2019 data, a total of 10,031 tons of fruit were produced. Major fruit crops include walnut, almond, strawberry, and wine grapes. Walnut production, covering 36.5% of cultivated land, is a major income source for the district. Strawberry production, once conducted at high volumes, has declined in recent years.

Animal Husbandry

Animal husbandry, alongside agriculture, constitutes the second major pillar of Kula’s economy. According to TÜİK 2019 data, the district has 47,833 head of large livestock and 119,087 head of small livestock. Large livestock accounts for 19.23% of Manisa’s total, while small livestock represents 8.35%. Nationally, Kula contributes 0.27% of Türkiye’s large livestock and 0.15% of its small livestock production.

Large livestock farming focuses on milk and meat production, while small livestock farming centers on goat and sheep rearing. Additionally, beekeeping, poultry farming, and partially sericulture are practiced as supplementary activities. Animal products such as milk, wool, and honey are important for both local consumption and market supply.

Industry and Trade

Industrial activity in Kula is limited but includes small-scale, agriculture-based processing facilities. Packaging and processing plants for walnuts, grapes, and cereals, as well as some flour and feed mills, operate in the district. Traditional handicrafts and ceramics also form part of small-scale production and trade.

Kula’s commercial life primarily revolves around the trade of agricultural products with the district center and neighboring districts. Weekly markets established in the district serve as vital sales points for local producers. In recent years, cooperative initiatives have gained momentum, with producer associations established for products such as walnuts and grapes.

Tourism and Service Sector

Following agriculture and animal husbandry, tourism represents the most significant potential sector in Kula’s economy. Historic Kula houses, the Kula Volcanic Geopark, and the region’s rich geological heritage make the district attractive to tourists. With the growth of tourism, activity has increased in accommodation, food and beverage services, and souvenir trade.

Tourism

Historic Kula Houses and Urban Fabric

Kula is one of the rare settlements that has preserved the characteristic urban structure of the Ottoman period to the present day. The Kula houses, dating from the 18th and 19th centuries, are among the most original and best-preserved examples of Ottoman architecture in Anatolia. Constructed using a wooden frame with adobe infill on stone foundations, these houses typically feature two stories, with upper floors projecting over the street and covered by tiled, ornate roofs. Wooden shutters, decorated ceilings, finely crafted wooden cabinets, and hearths are distinctive features of these homes.

Historic Kula Houses (Anadolu Agency)

Kula houses reflect the Ottoman lifestyle emphasizing privacy, with wide courtyards and high walls. Ground floors contain service areas such as stables, storage, and kitchens, while upper floors serve as living and reception spaces. The main room, known as the “baş oda,” is reserved for guests and enriched with detailed wooden ornamentation.

Kula’s dense street layout, developed according to a castle-centered settlement logic, is a classic example of organic urban planning. Narrow, winding streets are typically wide enough for a loaded animal to pass. This unique urban structure has earned Kula the title of “Monumental Town” and necessitates the preservation of its historical fabric.

Kula-Salihli UNESCO Global Geopark

Kula hosts Türkiye’s and the Turkish World’s first and only UNESCO-recognized global geopark. The Kula-Salihli UNESCO Global Geopark covers an area of 2,320 km² and includes the Gediz Graben and the western sections of the Western Anatolian plateaus.

Global Geopark (Anadolu Agency)

The geopark is distinguished by rock formations, volcanic structures, and tectonic features dating back over 200 million years. As one of Türkiye’s youngest volcanic areas, it hosts numerous geological formations including lava flows, basalt columns, lava caves, fault lines, and alluvial fans. Archaeological and prehistoric finds such as human footprints in the Çakallar region and rock carvings at Kanlıkaya further enrich the region’s geological heritage with cultural significance.

The geopark is not merely a geological site; it also holds great potential for nature hiking, geological photography, scientific research, and environmental education. The Kula Geopark Visitor Center and the Geopark Research Center (JARUM) offer visitors scientifically enriched experiences.

Kula Fairy Chimneys and Natural Formations

The Kula Fairy Chimneys are among the district’s most striking natural heritage features. These formations, located within the Burgaz Volcanite Zone, resulted from the interaction of lava flows with fluvial sediments. On this plateau, where basaltic lava reaches thicknesses of 30–40 meters, extraordinary shapes have been sculpted by rain and wind erosion.

Fairy Chimneys (Kula Subdistrict Office)

The fairy chimneys, together with the surrounding badlands-type eroded terrain, create an impressive landscape. These natural formations offer a unique visual spectacle for photographers and nature enthusiasts. The ancient sediments on either side of the valley form extraordinary geomorphological shapes shaped by natural processes, and the region continues to undergo active geological change.