IDENTIFICATION AND MAPPING OF FERRIC-OXIDE AND OXYHYDROXIDE MINERALS IN IMAGING SPECTROMETER DATA OF SUMMITVILLE, COLORADO, USA, AND THE SURROUNDING SAN-JUAN MOUNTAINS
Wh. Farrand, IDENTIFICATION AND MAPPING OF FERRIC-OXIDE AND OXYHYDROXIDE MINERALS IN IMAGING SPECTROMETER DATA OF SUMMITVILLE, COLORADO, USA, AND THE SURROUNDING SAN-JUAN MOUNTAINS, International journal of remote sensing, 18(7), 1997, pp. 1543-1552
Fe3+ bearing minerals and poorly crystalline mineraloids can host pern
icious trace metals released by mining activities. Such mineral phases
are readily detectable in imaging spectrometer data such as is collec
ted by NASA's Airborne Visible/Infrared Imaging Spectrometer (AVIRIS).
Laboratory measured reflectance spectra of fluvial sediment samples g
athered downstream from the Summitville mining district in southwest C
olorado, U.S.A., have been compared with AVIRIS data collected over Su
mmitville and the surrounding San Juan mountains. Spectra from the AVI
RIS image cubes over Summitville match with the laboratory measured re
flectance of several Fe3+ bearing mineral phases including a ferrihydr
ite produced in an acid water environment.