Abstract
DOI: 10.17014/ijog.6.1.103-113
In 2015, the number of international tourists who visited Borobudur temple declined and did not reach the government target. It was because there was only one attraction in the temple. After visiting Borobudur, most of tourists move to another place such as Yogyakarta. They know about the temple, but not its past environment when the temple was built. The history and past environment of Borobudur temple could be developed as additional tourist attractions to make them stay longer in that area. Geological condition and the evidences of an ancient lake could be developed as tourist objects. It is very interesting and could be developed to educate visitors in geo-archeology. The aim of this research is to develop archeological (temple) tourism based on geology and past environment. Although many researches on geo-archeology have been done, the results which relate to tourism are still not widely applied yet. The methods used are secondary data analysis and a field survey to investigate the potential of tourist stop sites. The potential tourist attractions were determined by geomorphology, lithology outcrops, stratigraphy, environment, and accessibility. The result is ten stop sites which could be used to describe the paleoenvironment in Borobudur based on geosciences. These tourist objects could explain the environment in the past related to the temple reliefs and ancient human activities.
References
Coulthard, T. J., Lewin, J., Macklin, MG (2005). Modelling differential catchment response to environmental change. Geomorphology, 69(1–4), 222–241.
Cox, S.C., Menzies, C.D., Sutherland, R., Denys, P.H., Chamberlain, C., and Teagle, D.A.H., 2016. Changes in hot spring temperature and hydrogeology of the Alpine Fault hanging wall, New Zealand, induced by distal South Island earthquakes. Geofluids, p.228-248. DOI:10.1002/9781119166573.ch19.
Dietze, E., Wünnemann, B., Diekmann, B., Aichner, B., Hartmann, K., Herzschuh et al (2010). Basin morphology and seismic stratigraphy of Lake Donggi Cona, north-eastern Tibetan Plateau, China. Quaternary International, 218(1–2), 131–142.
Fletcher, W.J., Boski, T., and Moura, D., 2007. Palynological evidence for enviromental and climate change in the lower
Guadiana valley, Portugal, during the last 13,000 years. The Holocene, 17, p.481-494. DOI:10.1177/0959683607077027
Gomez, C., Janin, M., Lavigne, F., Gertisser, R., Charbonnier, S.,et al (2010). Borobudur , a basin under volcanic in fl uence : 361 , 000 years BP to present. Journal of Volcanology and Geothermal Research, 196(3–4), 245–264.
https://doi.org/10.1016/j.jvolgeores.2010.08.001
Gunarto, H., 2007. Preserving Borobudur’s Narrative Relief Wall of UNESCO Cultural WorldHeritage. Ritsumeikan Center for Asia Pacific Studies (RCAPS) Occas Journal Paper.
Murwanto H (1996) Pengaruh Aktivitas Gunungapi Kuarter Terhadap Perubahan Lingkungan Danau di Daerah Borobudur dan Sekitarnya, Jawa Tengah, (The influence of quatenarry volcano activity to lake environment changes in Borobudur area and surrounding, central java), Thesis, Faculty of Geography, Gadjah Mada University.
Murwanto H, Gunnell Y, Suharsono S, Sutikno S, Lavigne F (2004). Borobudur monument (Java, Indonesia) stood by a natural lake: chronostratigraphic evidence and historical implications. The Holocene, 14(3), 459–463. https://doi.org/10.1191/0959683604hl721rr
Murwanto H (2014). Trace of lake environment in around Borobudur temple with paleogeomorphological approach, Disertation, Faculty of Geography, Gadjah Mada University, Yogyakarta, Indonesia
Murwanto H, Purwoarminta A (2015). Borobudur Ancient Lake Site; Borobudur as Cultural Landscape, Sub Chapter 3, Book, Kyoto University Press, Japan
Nieuwenkamp, WOJ. (1933). Het Boroboedoermeer, Algemeen Handelsblad, Denhaag, 9 September 1933.
Nossin, I,J. and Voute, C., 1986. Notes on the Geomorphology of The Borobudur Plain (Central Java Indonesia) in an archeological historical context). Simposium an Remote Sensing for Resources Development and Environmental Management/Enschede, Netherland
P.T. Taman Wisata Candi Borobudur, Prambanan, dan Boko, 2015. Annual Report 2015 Yrly.
Rodning, C., 2010. Place, landscape, and environment: Anthropological archaeology in 2009. American Anthropologist, 112 (2), p.180-190. DOI: 10.1111/j.1548-1433.2010.01217.x
Tanudirjo, D.A., 1991. Changing perspectives on the relationship between heritage, landscape and local communities: A lesson from Borobudur. Book Chapter: Transcending the Culture-Nature Divide in Cultural Heritage, DOI: 10.22459/TA36.12.2013.05
Wünnemann B, Yan D, Ci R (2015). Morphodynamics and lake level variations at Paiku Co, southern Tibetan Plateau, China. Geomorphology, 246, 489–501.
Zhang Y, Wünnemann B, Bezrukova EV, Ivanov EV, Shchetnikov AA, et al (2013). Basin morphology and seismic stratigraphy of Lake Kotokel, Baikal region, Russia. Quaternary International, 290–291, 57–67.
Zhu, Z., Zhang, H., Zhao, J., Guo, X., Zhang, Z., Ding, Y., and Xiong, T., 2018. Using toponyms to analyze the endangered Manchu language in Northeast China. Sustainability, 10 (2), p.563. DOI: 10.3390/su10020563.