Presented at the 3rd International Symposium on Innovative Approaches in Scientific Studies (Engineering and Natural Sciences) (ISAS2019-ENS), Ankara, Turkey, Apr 19, 2019

SETSCI Conference Proceedings, 2019, 4, Page (s): 260-267 , https://doi.org/

Published Date: 01 June 2019    | 616     11

For many years, biggest problem in the preparation of landslide susceptibility maps has been experienced in the selection of parameters. Each parameter gives different results in different fields. Some of these parameters can be generally evaluated while others reflect the characteristics of the areas. In this study, the effect of linear parameters on the landslide was investigated. For this purpose, 64 of the 1 / 25.000 scale and 2945 landslide sheet prepared by MTA (Mineral Research and Exploration) were selected. Among these, the maps with landslides were chosen. The cell size was digitized with ArcGis 10.4 by setting to 28 pixels. Landslide inventory maps are prepared and overlapped with the parameter map for each area. After the reclassification, the maps were analyzed. For each parameter, landslide areas are determined by class ranges. Class ranges were chosen in accordance with the literature. Scatter graphs are prepared in% of the areas and it is determined that landslides occur between the values. The compatibility of the parameters with the literature was checked. As a result, the distance from the road to landslide areas were tried to be determined. It was revealed that landslides were formed in class ranges. Since it isn’t encountered in every area, it isn’t generally preferred in the literature. Although it is easy to prepare, the researchers avoid this parameter because they are evaluated together with other parameters. As a result, it is tried to determine the distance to the road to landslide areas. It was revealed that landslides were formed in class ranges.

Keywords - Landslide, susceptibility, road, parameter, lineament

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