Geographia Technica, Vol 15, Issue no.1/2020, pp. 70-79
ANALYSIS OF STATIC MORPHOSTRUCTURE CONDITIONS WITH DYNAMIC MORFOSTRUCTURE (LANDSLIDE TYPE)
SUWARNO 
, MISNAH, MUJIARTO
ABSTRACT: Landslides occur in many types of Tuff rocks and Tertiary-aged andesite sandstones which can cause changes in the shape of the earth's surface, which shows the development of dynamic morphostructure. The purpose of this study was to determine the relationship of static morphostructure with dynamic morphostructure landslide type in Pekuncen Banyumas District. The research method used a survey method which included fieldwork (for inventory of static morphostructure and dynamic morphostructure landslide type) and laboratory work (for interpretation of aerial and satellite photo, and analysis of static morphostructure relationships with dynamic morphostructures landslide type). The results of the study found many observable landslides and geological structures. The geological structure that contained are in the structure of folds, fractures, and volumes. There is a relationship between landslide and geological structures. In fault structures, folds and layers sloping with patterns of clustered landslide, while in volcanic structures, the patterns of landslide are spread.
Keywords: Static morphostructure, Dynamic morphostructure, Landslide, Indonesia
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