Journal of Agricultural Science www.agrivita.ub.ac.id This eruption also damaged some regions in the Cangkringan district Sleman Regency. Moreover, Iguchi, Ishihara, Surono, & Hendrasto (2011) reported that the eruption that occurred on October 26 th , 2010, damaged the mountain cliff (dome) formed in 2006. More significant destruction was recorded from the eruptions on November 3 rd and 5 th, 2010, as the opened cliffs emitted the flow of pyroclastic materials and ash. The volcanic eruption was followed by pyroclastic flows, surges, debris avalanches, and lahars, which could damage the ecosystem, plantation, and settlements (Kadavi, Lee, & Lee, 2017; Sadono, Hartono, Machfoedz, & Setiaji, 2017). Its adverse effects may lead to forest degradation (vegetation loss), the decline of land fertility (an increase of damaged lands), and disruption of the local water cycle (streamflow, water table, and available water) (