Morphology of large-scale debris avalanche deposits in Cianjur Plains, West Java, Indonesia
Abstract Large-scale debris avalanche deposit (DAD) processes rarely occur, but the impact is catastrophic. Large-scale flank collapse from ancestral Gede volcano resulted in the deposition of debris avalanche deposits that manifested as prominent hummocky hill landforms covering 192 km2 of the Cianjur Plains, West Java, Indonesia. Although the deposit covers large areas and shows unique volcanic landscape morphology, studies on debris avalanche deposits are limited. Here, we show the results of field reconnaissance, satellite photography and digital elevation model analysis to understand the morphology of large-scale debris avalanche deposits, including their distribution and morphological characteristics. The interpreted thickness of the deposit ranges from 200-500 m, although the hummocky hill with a well-rounded texture is only 50-100 m high due to intense erosion in the tropical region with the remaining portion of the megaclast blocks buried. The distribution of hummocky hills indicates that the flow was constrained by the pre-existing basin configuration. The debris avalanche deposit shows fan-like morphology that characterizes block facies located near the fan mouth, while the matrix facies has matrix-supported smaller blocks in the distal part. The mouth of the debris avalanche deposit is located just south of Cianjur township, with the highest concentration of megaclast block as block facies, which is interpreted as the main depositional axis. The block facies apparently stopped by lineament of the SW-NE-oriented Cimandiri valley to the southeast and NNE-SSW-oriented Cisokan River lineament to the east, which was interpreted as a buried normal fault that was considered a barrier to confine the flow of block facies deposition.