The confluence of a near neutral stream, on the left, with a strongly acidic stream (pH around 3) that drains an oxidizing high-sulfidation epithermal gold deposit in Argentina. The brown color of the acidic stream is caused by precipitates of iron (ferric) hydroxides. The ridge in the distance is the crest of the Andes and the boundary between Argentina and Chile.
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Details
Creative#:
TOP22076417
Source:
達志影像
Authorization Type:
RM
Release Information:
須由TPG 完整授權
Model Release:
N/A
Property Release:
No
Right to Privacy:
No
Same folder images:
earthsciencevolcanic-hydrothermaldeposithighsulfidationepithermalgolddepositleachateleachingoxidationweatheringaciddrainageferrichydroxidesironprecipitateprecipitationbarriergeochemistrymixingdifferentcolorsandesmountainshighandesargentinasouthamericansceniclandscapelandformgeomorphologygeographygeologyconvergenceconvergingmergingjoiningmeetingsuspendedsedimentsilt-ladensiltystreammuddyriverbrownwaterclearwaterconfluenceneutralstreamacidicstream
acidacidicamericanandesandesargentinabarrierbrownclearcolorsconfluenceconvergenceconvergingdepositdepositdifferentdrainageearthepithermalferricgeochemistrygeographygeologygeomorphologygoldhighhighhydroxidesironjoininglandformlandscapeleachateleachingmeetingmergingmixingmountainsmuddyneutraloxidationprecipitateprecipitationriverscenicsciencesedimentsilt-ladensiltysouthstreamstreamstreamsulfidationsuspendedvolcanic-hydrothermalwaterwaterweathering
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