Conclusion

Several studies have suggested that fault-controlled uplift movements of the Aravallis led to the westward migration of the rivers in this area. The faults have been and continue to be active, as a consequence, there was uplift and sinking or horizontal displacement of the ground. The rivers and streams were frequently forced to change their courses, sometimes gradually, sometimes abruptly (Mitra et al., 2012).

Although the radar data doesn’t work well in this study, the optical images also gives a good result showing high compatibility with the field observation. The use of micro-geomorphology in satellites images is definitely another powerful application of the satellites image. The result here shouldn’t be ruled out of ambiguity while the track of the buried channel is formed by connecting the suggested river segments so a more strict examination is needed.

To get a more accurate result of the buried channel the higher resolution and deeper penetration radar images are required and Ground Penetration Radar (GPR) will be a good solution in this study.