CONSTRAINING THE GEOMORPHOLOGY OF THE RICO DOME IN SOUTHWESTERN COLORADO WITH GIS AND FIELD STUDIES
The digital models are derived from published geologic maps at 1:24,000. We first established points along several prominent geologic contacts within the study area and assigned elevation values to them using a 30 m elevation model. For each contact, Esri ArcGIS software was applied to build a 3D surface fitting between each point. The result is a series of digital 3D surfaces which represent the subsurface stratigraphy of the structure. Strike and dip measurements of strata at several stations throughout the study area were measured in the field to confirm the data presented on the geologic maps.
The results of this study show that the structure’s longest dimension is oriented ~218°, contrary to the originally suggested direction. Due to the discrepancy between this direction and the dominantly east-west striking faults, we argue that the faults were not dominant controls on the position and geometry of the dome. Results from this investigation invite a new interpretation of factors which could have influenced the dome’s formation. This opens the possibility of previously unexplored controls such as weak stratigraphic zones or deep, unexposed fractures.