Urang Cave Karst Environmental Development, as Tourism Object

Srijono Srijono(1*), Nisa Nadia(2)

(1) Laboratorium Geologi Dinamik, Jur. T.Geologi FT UGM, e-mai
(2) Sarjana Teknik Geologi bekerja di PT Aneka Tambang, Tbk.
(*) Corresponding Author


Karst environment become an alternative tourist destination as well as to boost local revenues. In karst environments in Grobogan District, Central Java Province, formed Urang Cave, with an interesting endokarst phenomenon. This study aims to do zoning district Urang Cave as tourist sites. The research method is using contour maps as a base map of Urang Cave karst environment geomorphological mapping. Geomorphological data processing is using ArcView GIS 3.3 program. Land use map refers to RBI, scale 1:25.000. Geomorphological analysis refers to the Ministry of Energy and Mineral Resources No. 1456.K/20/MEM/2000, and petrography. Each development zone is analyzed its geophysical environmental element, then set scoring and value summation. For comprehensive environmental element analysis, chemical analysis of rocks, and water-soil chemistry. In reference to Minister of Energy Mineral Resource decrees No. 1456/K/20/MEM/2000, Urang Cave zoning defined into 3 (three) zone, as follow: the Protected Zone, Cultivation Zone 1, and Cultivation Zone 2. Protected Zone, consists of Urang Cave tunnel/hallway with a unique spheleothem in it. This zone as a cave tracking site tourism, potential to produce karst water as a decent drinking water while maintaining hardness. Cultivation Zone 1 is spreading about 200 m in distance from outer appearance of spring around the cave hallway. In this zone mining of cave sediments may be done in the inactive form caves, without changing the state of the existing major exokarst morphology. Cultivation Zone 2, an outer zone, located farthest from the tunnel/hallway Urang Cave. Utilization of this zone as a limestone mining quarry, although only on a small scale.


karst environment;Urang Cave;tourism

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Anonimous, 1999, Peta Rupabumi Digital Indonesia Lembar Tambakromo Nomor 1569-111, Badan Koordinasi dan Pemetaan Nasional, Bogor, Indonesia

Anonimous, 2000, Keputusan Menteri Energi dan Sumber Daya Mineral Nomor 1456/K/20/MEM/2000, tentang Pedoman Pengelolaan Kawasan Kars, Dept. ESDM, Jakarta

Bloom, A. L., 1978, Geomorphology : A systematic Analisys of Late Cenozoic Landforms, Prentice Hall Englewood Cliffs, New Jersey

Badri, I., Djarwoto, A., Sutarjan, W., dan Suhari, 1999, Selection of Settlement Area Based on Environmental Geological Aspects, Proceedings of Indonesian Association of Geologists - vol.IV, PP.33-39, The 28th Annual Convention, Jakarta 30 November – 1 December

Moore, G.W., 1969, Speleothem, in: Fairbridge, R.W. (Ed), 1969, The Encyclopedia of Geomorphology, pp.1040-1041, Reinhold Book Coorporation, New York.

Kusumayudha, S. B., 2004, Mengenal Hidrogeologi Kars, Pusat Studi Kars LPPM UPN “Veteran” Yogyakarta

Mukna, H.S., 2009, Kebijakan Nasional Pengelolaan Kawasan Kars, Kumpulan Makalah Workshop Nasional Kawasan Kars Indonesia

Pringgoprawiro, H., 1983, Biostratigrafi dan Paleografi Cekungan Jawa Timur Utara Suatu pendekatan Baru, Tesis untuk memperoleh gelar Doktor, ITB, Bandung

Ritter, D.F., 1978, Process Geomorphology, Wm. C. Brown Publisher, Iowa

Thornbury, W.D., 1969, Principles of Geomorphology, John Wiley & Sons, New york

Van Bemmelen, R.W., 1949, The Geology of Indonesia, Vol IA, Martinus Nijhoff, The Hague - Netherland

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