APPLICATION OF REMOTE SENSING TECHNIQUES FOR GYPSUM KARST GEOHAZARD ASSESSMENT IN THE GYPSUM PLAIN, WEST TEXAS
Gypsum karst geohazard detection in West Texas relies heavily on LIDAR (light detection and ranging) derived elevation models to: 1) develop overland flow models for drainage of monsoonal storms from infrastructure; 2) delineation of major karst interfaces for groundwater recharge and potential shallow macro-porosity; and 3) delineation of subtle, shallow depressions that have been filled with gypsic soils mantling buried karst features. CIR-image analyses have been employed for Gypsum Plain geohazard assessment to develop classified geologic maps for spatial prediction of regions favorable for karst development; NDVI (normalized difference vegetation index) analyses have proven useful for delineation of regions of high moisture flux, including filled sinkholes, filled solution valleys, and non-confined hypogene manifestations. Thermal-infrared (TIR) imagery analyses have significant potential for geohazard detection, but rely heavily on high thermal and barometric pressure differences for effective phenomena detection which requires more extensive planning to maximize the benefits of local ambient conditions at the time of image capture. UAV platforms have widespread potential for economical, high resolution data collection of CIR and TIR imagery as well as accurate elevation models.