
Overview
01Overview
Gunůngkidůl is a regency located in the Special Region of Yogyakarta, Indonesia. The administrative centre is the town of Wonosari. The name "Gunungkidul" comes from the Javanese language mountains in the south of Java Land, whose area is located in the Thousands Mountains range of the province.
The Regency covers an area of 1,475.15 km2, about 46.5% of the provincial area. It had a population of 675,382 at the 2010 Census and 747,161 at the 2020 Census; the official estimate as of mid-2023 was 751,011 - with 371,220 males and 379,800 females - and so the population density in this regency is relatively low compared to other regencies of the province.
This regency is bordered by Klaten Regency and Sukoharjo Regency in the north and northeast, Wonogiri Regency in the east, the Indian Ocean in the south, and Bantul Regency and Sleman Regency in the west and northwest. Gunungkidul Regency has 18 Districts (Kapanewon). Most of the regency is hills and limestone mountains, which are part of the Thousand Mountains. Gunungkidul is known as a relatively barren area and often experiences drought in the dry season, but it has a unique historical feature, in addition to its tourism, cultural and culinary potential.
The traditional dishes from Gunůngkidůl include "Gathot" and "Thiwul", made from fermented cassava and dry cassava.
Culture
01Culture
Walang goreng (fried grasshoppers) Gunungkidul Regency is located in the limestone uplands of Java, and a delicacy called walang goreng (fried grasshoppers).
History
01Prehistory
Statue menhirs from Gunungkidul From archaeological findings, the area of Gunungkidul Regency is thought to have been inhabited by humans (Homo Sapiens) from 700,000 years ago. Many find the instructions of human existence found in caves and niches in karst of Gunungkidul, especially in Ponjong District. The human propensity Gunung occupy the time it caused most of the lowland in Yogyakarta is still flooded. The arrival of the first humans in Gunungkidul occurred at the end of the Pleistocene epoch. At that time, the human race Australoid migrated from the Pegunungan Sewu in Pacitan, East Java passing Wonogiri karst valleys, Central Java until it reaches the southern coast of Gunungkidul through ancient, Bengawan Solo.
Geography
01Geography
As the name implies, Gunungkidul Regency is dominated by mountains which are the western part of the Sewu Mountains or the South Limestone Mountains (from this nickname, the name "Gunungkidul" is derived), which stretches across the southern part of Java Island starting from the area eastward to Tulungagung Regency.
The Mountains are formed from limestone, indicating that in the past it was a seabed. The findings of ancient marine animal fossils support this assumption. This area began to become land as a result of tectonic and volcanic uplifts since the Miocene.
Gunungkidul Regency is one of the regencies in the Daerah Istimewa Yogyakarta Special Province, with Wonosari as the capital city. The total area of Gunungkidul Regency is 1,475.15 km2 or about 46.5% of the total area of the Special Province of Daerah Istimewa Yogyakarta. The city of Wonosari is located southeast of the Yogyakarta City (the capital of Daerah Istimewa Yogyakarta Special Province), with a distance of ± 39 km. The Gunungkidul Regency area is divided into 18 Districts (Kapanewon) and 144 villages.
02Geography
Gunungkidul Regency is in a karst region. This leads to difficult geography for farmers and contributes to considerable poverty in the area because of water shortages. Much of the Regency is included in the Mount Sewu (literally "thousand mountains") collection of limestone hills which stretches across parts of southern Java from parts of Kebumen Regency in the west near the border with West Java across to close to the city of Malang in East Java. The Menoreh Hills in the area south of Yogyakarta in Kulonprogo Regency, for example, are part of this series of limestone hills.
03North Zone
The northern zone is called Agung Batur region, with an altitude of 200–700 m above sea level. The situation is hilly, there are sources of groundwater depth of 6m - 12m from the ground. Latosol soil types dominated by volcanic and sedimentary parent hurricane stones. This area includes the districts of Patuk, Gedangsari, Nglipar, Ngawen, Semin, and the northern part of the district of Ponjong.
04Central Zone
The Central Zone is called Ledok Wonosari development, with an altitude of 150–200 m above sea level. The soil type is dominated by Mediterranean association with the red and black grumusol limestone. So despite its long dry season, the water particles are still able to survive. There is a river on the land. Groundwater depth ranges between 60–120 m below the ground surface. This area includes the districts of Playen, Wonosari, Karangmojo and Ponjong, and the central and northern parts of Semanu.
05South Zone
The Southern Zone is called Pegunungan Sewu development area (Duizon gebergton or Zuider gebergton), with an altitude of 0–300 m above sea level. Constituent bedrock is limestone with characteristic conical hills (Conical limestone) and the karst area. Underground rivers are often found in this region. The southern zone includes the districts of Saptosari, Paliyan, Girisubo, Tanjungsari, Tepus, Rongkop, Purwosari and Panggang, and the southern parts of Ponjong and Semanu.