Global Warming Images
 
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366W0741_electric.jpg Loch Dubh hydro electric power station in the north West Highlands near Ullapool, Scotland
 
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366W0745_sub station.jpg Loch Dubh hydro electric power station in the north West Highlands near Ullapool, Scotland
 
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366W0752_sign.jpg Loch Dubh hydro electric power station in the north West Highlands near Ullapool, Scotland
 
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366W0865_power plant.jpg A hydro electric power station at lochluichart in the North West highlands of scotland
 
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366W0866_pylon.jpg A hydro electric power station at Grudie in the North West highlands of scotland
 
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366W0868_service.jpg Maintanance work on one of the generators at Achanalt hydro electric power station, North West highlands of scotland
 
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366W0869_sign.jpg Achanalt hydro electric power station, North West highlands of scotland
 
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366W0741_hydro.jpg Loch Dubh hydro electric power station in the north West Highlands near Ullapool, Scotland
 
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366W0745_HEP.jpg Loch Dubh hydro electric power station in the north West Highlands near Ullapool, Scotland
 
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366W0752_hydro.jpg Loch Dubh hydro electric power station in the north West Highlands near Ullapool, Scotland
 
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366W0865_HEP.jpg A hydro electric power station at lochluichart in the North West highlands of scotland
 
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366W0866_hydro.jpg A hydro electric power station at Grudie in the North West highlands of scotland
 
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366W0868_hydro.jpg Maintanance work on one of the generators at Achanalt hydro electric power station, North West highlands of scotland
 
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366W0869_hydro.jpg Achanalt hydro electric power station, North West highlands of scotland
 
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366W0873_hydro.jpg The intake dam for Achanalt hydro electric power station, North West highlands of scotland
 
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366W2533_climate change_marine diesel.jpg Refuelling a fishing vessel with marine diesel in Obasn scotland UK
 
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366W2520_global warming_marine diesel.jpg Refuelling a fishing vessel with marine diesel in Obasn scotland UK
 
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366W2638_global warming_raised beach.jpg Evidence of past climate change and glaciation. Raised beach platforms and old raised sea cliffs caused by isostatic rebound near Oban Scotland UK. During an ice age the weight of ice on the land depresses it. Isostatic rebound is caused when the weight of ice is removed by melting. This causes the land to rebound and rise up leaving coastal features raised above the present day sea level.
 
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366W2475_climate change_sea cave.jpg Evidence of past climate change and glaciation. Raised beach platforms and an old raised sea cave caused by isostatic rebound near Oban Scotland UK. During an ice age the weight of ice on the land depresses it. Isostatic rebound is caused when the weight of ice is removed by melting. This causes the land to rebound and rise up leaving coastal features raised above the present day sea level.
 
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366W2472_global warming_sea cave.jpg Evidence of past climate change and glaciation. Raised beach platforms and an old raised sea cave caused by isostatic rebound near Oban Scotland UK. During an ice age the weight of ice on the land depresses it. Isostatic rebound is caused when the weight of ice is removed by melting. This causes the land to rebound and rise up leaving coastal features raised above the present day sea level.
 
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366W2460_climate change_uplift.jpg Evidence of past climate change and glaciation. Raised beach platforms and old raised sea cliffs caused by isostatic rebound on the Isle of Kerrera off Oban Scotland UK. During an ice age the weight of ice on the land depresses it. Isostatic rebound is caused when the weight of ice is removed by melting. This causes the land to rebound and rise up leaving coastal features raised above the present day sea level.
 
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366W2455_global warming_uplift.jpg Evidence of past climate change and glaciation. Raised beach platforms and old raised sea cliffs caused by isostatic rebound on the Isle of Kerrera off Oban Scotland UK. During an ice age the weight of ice on the land depresses it. Isostatic rebound is caused when the weight of ice is removed by melting. This causes the land to rebound and rise up leaving coastal features raised above the present day sea level.
 
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366W2454_climate change_palaeo climate.jpg Evidence of past climate change and glaciation. Raised beach platforms and old raised sea cliffs caused by isostatic rebound on the Isle of Kerrera off Oban Scotland UK. During an ice age the weight of ice on the land depresses it. Isostatic rebound is caused when the weight of ice is removed by melting. This causes the land to rebound and rise up leaving coastal features raised above the present day sea level.
 
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366W2450_global warming_palaeo climate.jpg Evidence of past climate change and glaciation. Raised beach platforms and old raised sea cliffs caused by isostatic rebound on the Isle of Kerrera off Oban Scotland UK. During an ice age the weight of ice on the land depresses it. Isostatic rebound is caused when the weight of ice is removed by melting. This causes the land to rebound and rise up leaving coastal features raised above the present day sea level.
 
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366W2446_climate change_isostatic rebound.jpg Evidence of past climate change and glaciation. Raised beach platforms and old raised sea cliffs caused by isostatic rebound on the Isle of Kerrera off Oban Scotland UK. During an ice age the weight of ice on the land depresses it. Isostatic rebound is caused when the weight of ice is removed by melting. This causes the land to rebound and rise up leaving coastal features raised above the present day sea level.
 
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366W2439_global warming_isostatic rebound.jpg Evidence of past climate change and glaciation. Raised beach platforms and old raised sea cliffs caused by isostatic rebound on the Isle of Kerrera off Oban Scotland UK. During an ice age the weight of ice on the land depresses it. Isostatic rebound is caused when the weight of ice is removed by melting. This causes the land to rebound and rise up leaving coastal features raised above the present day sea level.
 
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366W2435_climate change_raised beach.jpg Evidence of past climate change and glaciation. Raised beach platforms and old raised sea cliffs caused by isostatic rebound on the Isle of Kerrera off Oban Scotland UK. During an ice age the weight of ice on the land depresses it. Isostatic rebound is caused when the weight of ice is removed by melting. This causes the land to rebound and rise up leaving coastal features raised above the present day sea level.
 
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366W2433_global warming_raised beach.jpg Evidence of past climate change and glaciation. Raised beach platforms and old raised sea cliffs caused by isostatic rebound on the Isle of Kerrera off Oban Scotland UK. During an ice age the weight of ice on the land depresses it. Isostatic rebound is caused when the weight of ice is removed by melting. This causes the land to rebound and rise up leaving coastal features raised above the present day sea level.
 
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366W2516_climate change_fish stocks.jpg Fishing boats in Oban harbour Scotland UK. As seas warm fish species are migrating further north forcing fishermen to alter their practices.
 
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366W2511_global warming_fish stocks.jpg Fishing boats in Oban harbour Scotland UK. As seas warm fish species are migrating further north forcing fishermen to alter their practices.
 
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366W2486_global warming_fishing.jpg Fishing boats in Oban harbour Scotland UK. As seas warm fish species are migrating further north forcing fishermen to alter their practices.
 
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366W2480_climate change_fishing.jpg Fishing boats in Oban harbour Scotland UK. As seas warm fish species are migrating further north forcing fishermen to alter their practices.
 
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