Robert Harding
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Atlantic cliffs pounded by surf in stormy winter weather, at Pendeen, with the ruins of old tin mines, part of the UNESCO World Heritage Site Cornwall and West Devon Mining Landscape, near St. Just, Cornwall, England, United Kingdom, Europe https://images.robertharding.com/zoom/RF/RH_RF/VERTICAL/1202-610.jpg1202-610https://www.robertharding.com/licenses-explained/https://www.robertharding.com/preview/1202-610/atlantic-cliffs-pounded-surf-stormy-winter-weather-pendeen/
1202-610 - Atlantic cliffs pounded by surf in stormy winter weather, at Pendeen, with the ruins of old tin mines, part of the UNESCO World Heritage Site Cornwall and West Devon Mining Landscape, near St. Just, Cornwall, England, United Kingdom, Europe
Salt dump, potash mining, railway tracks, Kolonnenweg, Lochplattenweg, Gruenes Band, border trail, former German-German border, Philipsthal, Werratal, Hersfeld-Rotenburg district, Hesse, Germany, Europe https://images.robertharding.com/zoom/RF/RH_RF/HORIZONTAL/832-393312.jpg832-393312https://www.robertharding.com/licenses-explained/https://www.robertharding.com/preview/832-393312/salt-dump-potash-mining-railway-tracks-kolonnenweg-lochplattenweg/
832-393312 - Salt dump, potash mining, railway tracks, Kolonnenweg, Lochplattenweg, Gruenes Band, border trail, former German-German border, Philipsthal, Werratal, Hersfeld-Rotenburg district, Hesse, Germany, Europe
Clay loaded with iron oxides and dried out, Rio Tinto, Andalusia, Spain *** Local Caption *** R?o 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. https://images.robertharding.com/zoom/RM/RH/HORIZONTAL/860-288801.jpg860-288801https://www.robertharding.com/licenses-explained/https://www.robertharding.com/preview/860-288801/clay-loaded-iron-oxides-dried-out-rio-tinto/
860-288801 - Clay loaded with iron oxides and dried out, Rio Tinto, Andalusia, Spain *** Local Caption *** R?o 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.
Reflections on Rio Tinto, near its source, Andalusia, Spain *** Local Caption *** R?o 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. https://images.robertharding.com/zoom/RM/RH/HORIZONTAL/860-288798.jpg860-288798https://www.robertharding.com/licenses-explained/https://www.robertharding.com/preview/860-288798/reflections-rio-tinto-near-source-andalusia-spain-local/
860-288798 - Reflections on Rio Tinto, near its source, Andalusia, Spain *** Local Caption *** R?o 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.
R?o Tinto, Andalucia, Spain *** Local Caption *** R?o 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. https://images.robertharding.com/zoom/RM/RH/HORIZONTAL/860-288800.jpg860-288800https://www.robertharding.com/licenses-explained/https://www.robertharding.com/preview/860-288800/ro-tinto-andalucia-spain-local-ro-tinto-red/
860-288800 - R?o Tinto, Andalucia, Spain *** Local Caption *** R?o 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.
R?o Tinto, Andalucia, Spain *** Local Caption *** R?o 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. https://images.robertharding.com/zoom/RM/RH/VERTICAL/860-288799.jpg860-288799https://www.robertharding.com/licenses-explained/https://www.robertharding.com/preview/860-288799/ro-tinto-andalucia-spain-local-ro-tinto-red/
860-288799 - R?o Tinto, Andalucia, Spain *** Local Caption *** R?o 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.
Toxic pond formed from runoff of mine tailings at an abandoned copper mine in the Prescott National Forest near Perkinsville, Arizona, United States of America, North America https://images.robertharding.com/zoom/RF/RH_RF/HORIZONTAL/1311-250.jpg1311-250https://www.robertharding.com/licenses-explained/https://www.robertharding.com/preview/1311-250/toxic-pond-formed-runoff-mine-tailings-abandoned-copper/
1311-250 - Toxic pond formed from runoff of mine tailings at an abandoned copper mine in the Prescott National Forest near Perkinsville, Arizona, United States of America, North America
Toxic pond formed from runoff of mine tailings at an abandoned copper mine in the Prescott National Forest near Perkinsville, Arizona, United States of America, North America https://images.robertharding.com/zoom/RF/RH_RF/HORIZONTAL/1311-251.jpg1311-251https://www.robertharding.com/licenses-explained/https://www.robertharding.com/preview/1311-251/toxic-pond-formed-runoff-mine-tailings-abandoned-copper/
1311-251 - Toxic pond formed from runoff of mine tailings at an abandoned copper mine in the Prescott National Forest near Perkinsville, Arizona, United States of America, North America