Threat Existence to Limestone Formations Around Goa Peteng in South Bali Island, Indonesia

G. Putu, Eka Suryana, D. Atmaja, E. Pratiwi, I. G. Budiarta, Ida Bagus, Arya Yoga Bharata, Ni Ketut, Catur Wulandari, Ni Nyoman, Tri Wulandari
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Abstract

The limestone formations are a unit of geological rock formations that are important for the formation of unique Karst landscapes but are often threatened by development interests, one of which is in the environment around Goa Peteng, whose existence is threatened. This research aims to investigate: 1) the conditions of limestone formations  around Goa Peteng, 2) identified threats to the existence of limestone formations  around Goa Peteng, and 3) potential opportunities for protecting the existence of limestone formations  around Goa Peteng. The methods used in this research include field observation, literature review, and assistance with map digitization. This assistance involves utilizing literature studies, both scientific articles and reports containing maps that also cover the study location. The results of the research show that the limestone formations in the Goa Peteng environment exist at of a level of karst development in the Goa Peteng environment, which is Mesokarst and parts of the surrounding area are Non-Karst apart from that there is Exokarst Potential and Endokarst though not much exists at the study location. The real threat to the existence of the karst landscape in the Goa Peteng environment is the development of mass tourism in the form of tourist accommodation such as hotels and villas, which has developed rapidly over the last 14 years, as seen from Satellite Image data. The limestone formations in the Goa Peteng environment themselves has the opportunity to be a place for education and further studies need to be carried out on the limestone formations and karst development in South Bali.
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印度尼西亚南巴厘岛 Goa Peteng 附近石灰岩地层面临的威胁
石灰岩地层是地质岩层的一个单元,对形成独特的喀斯特地貌非常重要,但经常受到开发利益的威胁,果阿佩腾周围环境就是其中之一,其存在受到威胁。本研究旨在调查:1)果阿佩滕周围石灰岩地层的状况;2)果阿佩滕周围石灰岩地层面临的威胁;3)保护果阿佩滕周围石灰岩地层的潜在机会。本研究采用的方法包括实地观察、查阅文献和协助地图数字化。这种协助包括利用文献研究,既包括科学文章,也包括包含研究地点地图的报告。研究结果表明,果阿佩腾环境中的石灰岩地层在果阿佩腾环境中的岩溶发育程度为中喀斯特,周边部分地区为非喀斯特,除此之外,还有外喀斯特潜力和内喀斯特,但在研究地点存在的不多。对果阿佩腾环境中喀斯特地貌的存在构成真正威胁的是以酒店和别墅等旅游住宿形式出现的大众旅游业的发展,从卫星图像数据中可以看出,这种旅游业在过去 14 年中发展迅速。Goa Peteng 环境中的石灰岩地貌本身有机会成为教育场所,因此需要对南巴厘岛的石灰岩地貌和岩溶发展进行进一步研究。
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