1. INTRODUCTION
Geological interpretation and mapping are based on direct and indirect interaction of information on types and distributions of material found at the surface, geomorphologic and structural characteristics, drainage systems and vegetation. Multispectral (MS) and synthetic aperture radar (SAR) remote sensed data provide capabilities to support geological mapping and mineral exploration [4], [8], [9], [10]. MS images contain information on spectral characteristics of land cover, while SAR backscatter detects morphology, structures and soil moisture. The interpretation of multisensor and multiresolution remotely sensed data are significantly improved by recent research and development using various image fusion techniques [2], [12], [13]. The potential of information extraction is increased by integrating remotely sensed data with ancillary data (DEM, geophysical, etc) [3], [7]. In this paper, we present a mapping technique to further enhance the interpretation potential of fused data for terrain/surficial geology. The study area is located in the Upper Mackenzie River Valley, North West Territories, Canada. The area incorporates uplands and low areas covered by thick morainal deposits, which consists mostly of till and related glacial features. Glacial lacustrine sediments are also widespread. The Mackenzie Mountains, located in the western part of the area, are characterized by presence of valley deposits of glacial outwash, lacustrine sediments, and till and post-glacial alluvial terraces, fans, and colluvium.