Image number: 2437403
© Jean-Philippe Delobelle / Biosphoto
Rights Managed
JPEG bitmap image
Image size: 8256x5504 pixels (27.5"x18.3" @300dpi)
Shooting date : 2019-05-23
Río Tinto ("Red River") is very acidic (Ph 2) and has a deep reddish hue due to iron dissolved in water. The acidity of the watercourse is linked to the drainage of pyrite, which is very present in the subsoil. Extremophilic and endemic bacteria and algae colonize the river bed, forming a fragile biofilm that evokes the hot springs of Yellowstone Park in the USA.
Keywords
Area / Freshwater wetland area / Body of water / River
Matter (substance) / Water (matter) / Water surface
Microorganism / Bacterium / Archaea
Matter (substance) / Mineral matter / Sulphur
Area / Organic formation and populating
Europe / European Union / Spain / Andalusia Autonomous community
Area / Freshwater wetland area / Freshwater spring
Matter (substance) / Mineral matter / Iron
Matter (substance) / Mineral matter / Copper
Economic activity / Mining industry / Mine