IDENTIFIKASI GERAKAN TANAH DI DESA KEBONHARJO DAN SEKITARNYA, KABUPATEN KULON PROGO, YOGYAKARTA

Ade Tiyas Nurhaja Tiyas, Suherman Dwi Nuryana, M. Amri
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Abstract

The village of Kebonharjo and neighborhoods is zone of relatively high ground movement. In the western part of Indonesia, it was formed due to the influence of the collision two tectonic plates. Kebonharjo and neighborhoods  are earthquake and volcanic zone. With a steep slope and high rainfall data, one of the biggest factors for landslides. This study aims to fins out what potential couse the area to become a landslide-prone area and there indications of anything in the research area. There are several obstacles to the development of the Kebonharjo village are and suggroundings. In its study using the DVMBG method qhich combines several parameters, on of which is rainfall parameter data, geology, slope, land use and soil types. The potential for landslides in Kebonharjo village really needs attention because the are is very high and the rainfall is high, the potential for large landslides. After counducting the research, it can be seen the types of landslides according to (Varnes, 1978), type of landslides Earth Spread and Earth Flow.   Keywords: Soil Movement, DVMBG method, tectonic.  
Kebonharjo村及其周边地区是地势相对较高的地区。在印度尼西亚西部,它是由于两个构造板块碰撞的影响而形成的。Kebonharjo及其邻近地区是地震和火山带。具有陡峭的坡度和高降雨量的数据,是造成山体滑坡的最大因素之一。这项研究的目的是找出该地区成为滑坡易发地区的潜在路线,并在研究区域中有任何迹象。Kebonharjo村的发展有几个障碍。在研究中采用了DVMBG方法,该方法结合了降雨参数数据、地质、坡度、土地利用和土壤类型等多个参数。Kebonharjo村发生山体滑坡的可能性确实需要引起注意,因为海拔很高,降雨量也很大,发生大型山体滑坡的可能性很大。经过研究,可以看到(Varnes, 1978)滑坡类型、滑坡类型Earth Spread和Earth Flow。关键词:土壤运动,DVMBG法,构造。
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