Rivers in the High Andes
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 (ferri
Picture No
13628187
Media ID
43067728
Size
5115px x 3418px
(9.9MB)
Credit
Fletcher & Baylis /Science Source/ www.ardea.com
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NA
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Available in UK only. No agents
Ardea Picture Library
Picture No
13628187
Contributor Ref
SCS-90077421
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Acid Acidic Andes Barrier Clear Confluence Convergence Converging Deposit Drainage Geomorphology Gold Hydrothermal Iron Joining Laden Landform Leaching Meeting Merging Mixing Muddy Neutral Oxidation Precipitate Precipitation Science Sediment Silt Silty Suspended Volcanic Weathering
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