MORFOTEKTONIK DAS CITARIK HULU KAITAN DENGAN TATA GUNA LAHAN, DI WILAYAH CICALENGKA, KAB. BANDUNG

Mochamad Aufar Muttaqin, Murni Sulastri, N. Sulaksana, P. P. R. Rendra
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Abstract

The Upper Citarik sub-watershed area is part of the Citarum watershed. Most of the surrounding land is used as agricultural areas, gardens, rice fields, forests, and settlements. With most of the people working as farmers, it causes land degradation due to agricultural extensification. Because the Cicalengka area is estimated to be the final part of the Lembang Fault, and an area that has experiencing changes of land use, this study aims to examine the relationship between the morphotectonic aspects of the Upper Citarik watershed and land use around the Citarik River. The approach used to identify morphotectonic influences in the research area is the analysis of the ridge lineament pattern as well as geomorphic analysis in the form of bifurcation ratio (Rb), drainage density (Dd), mountain front sinousity (Smf), and valley floor width to height ratio (Vf). The dominant pattern of ridge lineaments in the study area is northeast-southwest, resulting in mountains oriented northwest-southeast. The average Rb value is 3.64, Dd ranges from 0.25-10, Vf with an average of 0.62, and the Smf value ranges from 1.11-1.64 in the north and 1.3-2.39 in the south. It can be interpreted that the tectonic activity of the surrounding area is classified as moderately active tectonic, and there are differences in tectonic classes between the northern and southern parts.
上citark流域是Citarum流域的一部分。周围的大部分土地被用作农业区、花园、稻田、森林和定居点。由于大多数人都是农民,农业推广导致土地退化。由于Cicalengka地区被认为是Lembang断裂的最后一部分,并且是一个经历了土地利用变化的地区,因此本研究旨在研究上Citarik流域的形态构造方面与Citarik河周围土地利用之间的关系。识别研究区形态构造影响的方法是对脊线格局进行分析,并以分岔比(Rb)、排水密度(Dd)、山前正弦(Smf)和谷底宽高比(Vf)的形式进行地貌分析。研究区脊线的主导格局为东北—西南,形成了西北—东南走向的山脉。平均Rb值为3.64,Dd值为0.25 ~ 10,Vf值为0.62,Smf值北部为1.11 ~ 1.64,南部为1.3 ~ 2.39。可以解释,周边地区的构造活动属于中活动构造,南北构造等级存在差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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