Morphotectonic Control of Land Movements at Wundulako Region, Kolaka Regency, Southeast Sulawesi Province, Indonesia

Martono, Hasria, S. Asfar, M. Azzaman, L. Ngkoimani, A. Okto, L. Hamimu, Irawati, Sawaludin, La Ode Muhammad Iradat Salihin, Wahab
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引用次数: 1

Abstract

This research is located at Wundulako District, Kolaka Regency, Southeast Sulawesi Province. The purpose of this study are to determine the level of tectonic activity and the effect of tectonic activity on the land movement of the study area. Based on the DEM (Digital Elevation Model) analysis, geomorphology of the study area is dominated by mountains unit that indicate the influence of tectonic activity. Geomorphological aspects were analyzed to determine the tectonic classes in the study area such as watershed and non-watershed analysis. The results showed that, tectonic class of the study area is classified as very high and moderate tectonic class. The effect of tectonic class level on land movement in the study area shows a least correlation. This interprets that the cause of land movement at study area is not only influenced by tectonic factors but is also influenced by other factors such as rainfall, lithological conditions, geomorphology, earthquakes, and human activities. This shows that morphotectonic control has little effect on the land movements at Wundulako District, Kolaka Regency, Southeast Sulawesi Province, but is also influenced by other factors such as rainfall, lithological conditions, geomorphology, earthquakes, and human activities.
印度尼西亚苏拉威西省东南部Kolaka Regency Wundulako地区陆块运动的形态构造控制
本研究位于苏拉威西省东南部Kolaka Regency的Wundulako区。本研究的目的是确定研究区构造活动水平和构造活动对陆地运动的影响。基于DEM (Digital Elevation Model)分析,研究区地貌以山地单元为主,反映了构造活动的影响。对研究区进行了地貌分析,确定了流域和非流域的构造分类。结果表明,研究区构造等级可分为非常高和中等构造等级。构造等级水平对研究区陆地运动的影响相关性最小。这说明研究区陆地运动的成因不仅受构造因素的影响,还受到降雨、岩性、地貌、地震、人类活动等因素的影响。这表明,在苏拉威西省东南部Kolaka Regency的Wundulako地区,形态构造控制对陆地运动的影响不大,但也受到降雨、岩性条件、地貌、地震和人类活动等其他因素的影响。
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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