Yogyakarta : trip to Jomblang cave and Pindul cave

We provide tour that will have great experience to explore jomblang cave where we can see light from the sun. After tour jomblang continues to pindul cave
These mountains are a unique karstic landscape, characterized by the phenomenon being present on the surface (eksokarst) and subsurface (endokarst). Surface phenomena include positive formations such as karst hills totalling ± 40,000 conical hills, negative formation of karstic valleys and karstic lake. The subsurface phenomenon includes karst caves consisting of no less than 119 caves with stalactites and stalagmites, and underground rivers. Because of the uniqueness of its ecosystem, the 1993 International Union of Speleology proposed the Karst Area of the Sewu Mountains to be classed as a natural world heritage site. In the caves are also found human fossils from the early stone age about 1.8 million years old, along with stone tools for hunting.[3] Sewu mountains were formed with the lifting of the seabed thousands of years ago. Limestone rocks are characteristic of these mountains. The limestone hills are reported to contain hundreds of caves. These are classified locally as vertical caves (known as luweng in Javanese) and horizontal caves. Jomblang cave(id) (Luweng Jomblang) and Grubug Cave (Luwung Grubug), located in the Semanu subdistrict in Gunungkidul, as well as other caves in the area, are well-known to local caver (speleological) groups. Some of the caves are quite long; Cerme cave, for example, has an entrance in Bantul Regency and stretches for quite a distance eastward into Panggang subdistrict in Gunung Kidul Regency.

为了保证可用性，请尽早预订。特别是在公共假期或周末等旺季期间计划旅行时，提前预订是值得考虑的。

此游览您可以在旅行开始前24小时内免费取消。如果您在24小时后取消或未出现在游览中，您仍将被收取活动的全额费用。迟到接送或出发将被视为未出现。