印度尼西亚日惹省班图尔县伊莫吉里区Wukirsari村吉里约火山教育型自然旅游设计

S. Mulyaningsih
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摘要

先前的研究确定吉里洛约是第三纪古火山。岩脉、熔岩和安山岩角砾岩构成了该地区的地质条件,但古火山的中心相已经与许多裂缝相联系,因此需要进一步的地质技术处理。需要岩土工程的设计技术来支撑它。本研究旨在发展潜在滑坡管理背景下的岩土工程规划设计。另一方面,吉里洛约有潜在的以火山教育为基础的旅游,有美丽的风景支持。土工规划设计以教育型自然旅游开发的形式进行包装。与此相关的研究已经进行,并辅以岩土测绘来描述承载能力。结果发现西南-东北正断层(n290 ~ 320oe)、南北-南北剪切断层(0 ~ 15oe)和斜向正断层(西北-东南)。所有这些都有可能引发山体滑坡。在预测岩石活动运动的情况下,设计了坡度为25 ~ 300度的坡地,其安全系数至少为1.5 ~ 1.8。因此,减少潜在的群众运动的技术设计,以获得自然的巡航旅游。阶地设计出5个古火山地层,即中央相地层、岩脉地层、熔岩带水火山地层、熔岩带柱状节理地层和砾岩带自裂角砾岩地层。每一层都有多层教育通道连接,以减轻土地负担。
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Design of Volcanic Educational-based Natural Tourism at Giriloyo, Wukirsari Village, Imogiri District, Bantul Regency, Yogyakarta-Indonesia
Previous study determined Giriloyo was Tertiary ancient volcano. Dyke, lava, and andesitic breccia which comprise this region strongly support the geological conditions, but the central facies of the ancient volcano had already associated with so many cracks, so that need further geotecnical handlings. Design technic for the geotecnical engineering is required to support it. This study aims to develop a geotechnical planning design in the context of a potential landslide management. On the other hand, Giriloyo has a potential volcanic educational-based tourism, supported with beautiful landscapes. The geotechnical planning design was packaged in the form of educational-based natural tourism development. Research related to the purpose has been carried out supported with geotechnical mapping to describe the carrying capacity. The results found southwest-northeast normal faults (N290-320oE), north-south shear faults (0-15oE), and oblique normal faults (northwest-southeast). All of them have potentially move to generate landslides. In anticipate the active rock movements, sloping terraces into 25-30o to obtain safety factors of at least 1.5-1.8 have been designed. Thus, the technical design to reduce the potential mass movements is addressed to obtain the natural cruising tourism. The terraces are designed to expose 5 ancient volcanic stratums, i e. Central Facies Stratum, Dyke Stratum, Lava with Hydrovolcanic Stratum, Lava with Collumnar Joints Stratum, and Agglomerates with Autoclastic Breccia Stratum. Each of these stratums is connected with a multilevel educational pathway to reduce burden on the land.
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