Detecting slope deformation using two-pass differential interferometry: implications for landslide studies on Earth and other planetary bodies

Landslide features have been identified on Earth and moon, Mars, Venus, as well on the Jovian moons. By focusing on a terrestrial landslide complex we test the operational parameters of RADARSAT-1 and the use of two-pass differential interferometry to detect change, to map its extent, and to measure the amount of movement over a given time period