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3 dimensional surface motion will be calculated from several InSAR velocity fields with one dimensional line of sight (LOS) view angles. In order to find a model of dike propagation and closing, it is possible to calculate the three dimensional surface motion from multi-geometry data compilation (Fuhrmann and Garthwaite, 2019). By taking two Interferometric Synthetic Aperature Radar Images (InSAR) from different satellite look directions (Ascending and Descending) decompose the Line of Sight (LOS) value from both angles to create a vertical and east-west motion map.