W West Java is one of the regions that has a high disaster vulnerability, this condition is influenced by a complex geological order that is prone to geological disasters, faults can be identified by morphotectonic studies. By means of morphometric analysis it is used to identify the character of the shape of an area and its relation to the level of tectonic activity. Comparison of morphotectonic aspects in Quaternary and Tertiary rocks will involve active tectonic processes in them. The study was conducted with three methods, namely the studio method by measuring data Rb, Dd, Smi, Smf, and Fault Fracture Density field methods by means of geological mapping of field photographs, laboratory methods by analyzing interventions to prove field data with studio data and the linkages between active faults in the research area. The activity of faults and geomorphological parameters can be known by various morphotectonic approaches. Morphometric and morphotectonic parameters such as Rb, Dd, Smi, Smf and Fault Fracture Density are the references in determining activeness. The geological structure in the study area is in the form of a solid and a fault that is relatively northwest - southeast. The fault is evidenced by the existence of lines from the DEM image and the solid data found in the field. Keywords: Morphometry, Morphotectonic, watershed, active Tectonics