Abstract
At Damascus Sulcus area within SPT (South Polar Terrain) there were interpreted a series of images where it was analyzed the distribution of different size particles that are ejected by distinct criovolcanic sources based on the analysis of the morphology, tectonic, reflectance and spectral signature of the surface material. This work shows these observations by comparing high resolution images of VIMS and ISS in combination with a Digital Elevation Model.
