Global Warming Images
 
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IMG_9979_raised beach.jpg Remains of a raised beach near Sennen Cove, Cornwall, UK. Raised beaches are evidence of higher sea levels than today caused by isostatic rebound after tyhe weight of cie was removed from the land when it melted after the last ice age.
 
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IMG_9982_raised beach.jpg Remains of a raised beach near Sennen Cove, Cornwall, UK. Raised beaches are evidence of higher sea levels than today caused by isostatic rebound after tyhe weight of cie was removed from the land when it melted after the last ice age.
 
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IMG_9983_raised beach.jpg Remains of a raised beach near Sennen Cove, Cornwall, UK. Raised beaches are evidence of higher sea levels than today caused by isostatic rebound after tyhe weight of cie was removed from the land when it melted after the last ice age.
 
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IMG_9985_raised beach.jpg Remains of a raised beach near Sennen Cove, Cornwall, UK. Raised beaches are evidence of higher sea levels than today caused by isostatic rebound after tyhe weight of cie was removed from the land when it melted after the last ice age.
 
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366W8385_science.jpg Scientists Anthony Long and Sarah Woodroffe of Durham University geography department looking at glacial marine sediments near Ilulissat on Greenland. For the last 4 years they have been studying isostatic rebound or how the land is rising after the weight of ice is taken off it. If they can understand how the relative sea levels were affected by the changeing climate of the past they should be able to greater understand how the melting of the Greenland ice sheet will affect global sea levels. This understanding is crucial as the Greenland ice sheet contains enough warter to raise global sea levels by nine metres.
 
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366W8390_scientist.jpg Scientists Anthony Long of Durham University geography department looking at glacial marine sediments near Ilulissat on Greenland. For the last 4 years they have been studying isostatic rebound or how the land is rising after the weight of ice is taken off it. If they can understand how the relative sea levels were affected by the changeing climate of the past they should be able to greater understand how the melting of the Greenland ice sheet will affect global sea levels. This understanding is crucial as the Greenland ice sheet contains enough warter to raise global sea levels by nine metres.
 
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366W8394_geographer.jpg Scientists Anthony Long of Durham University geography department looking at glacial marine sediments near Ilulissat on Greenland. For the last 4 years they have been studying isostatic rebound or how the land is rising after the weight of ice is taken off it. If they can understand how the relative sea levels were affected by the changeing climate of the past they should be able to greater understand how the melting of the Greenland ice sheet will affect global sea levels. This understanding is crucial as the Greenland ice sheet contains enough warter to raise global sea levels by nine metres.
 
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366W8406_deposits.jpg Scientists Anthony Long of Durham University geography department looking at glacial marine sediments near Ilulissat on Greenland. For the last 4 years they have been studying isostatic rebound or how the land is rising after the weight of ice is taken off it. If they can understand how the relative sea levels were affected by the changeing climate of the past they should be able to greater understand how the melting of the Greenland ice sheet will affect global sea levels. This understanding is crucial as the Greenland ice sheet contains enough warter to raise global sea levels by nine metres.
 
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366W8431_carbon dating.jpg Scientists Sarah Woodroffe of Durham University geography department looking at seeds of Arctic Crowberry near Ilulisat on Greenland. These fossil seeds found in salt marsh can be carbon dated to measure sea level rise from isostatic rebound. For the last 4 years they have been studying isostatic rebound or how the land is rising after the weight of ice is taken off it. If they can understand how the relative sea levels were affected by the changeing climate of the past they should be able to greater understand how the melting of the Greenland ice sheet will affect global sea levels. This understanding is crucial as the Greenland ice sheet contains enough warter to raise global sea levels by nine metres.
 
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IMG_1739_expedition.jpg Scientific equipment belonging to Scientists Anthony Long and Sarah Woodroffe of Durham University geography department on a boat at Ilulissat on Greenland. For the last 4 years they have been studying isostatic rebound or how the land is rising after the weight of ice is taken off it. If they can understand how the relative sea levels were affected by the changeing climate of the past they should be able to greater understand how the melting of the Greenland ice sheet will affect global sea levels. This understanding is crucial as the Greenland ice sheet contains enough warter to raise global sea levels by nine metres.
 
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366W8427_moraine.jpg A 9000 year old moraine left when the Jacobshavn glacier was much higher than it is today. The ice sheet at Ilulissat on Greenland has retreated rapidly due to global warming
 
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IMG_8305_scientist.jpg.jpg Scientists Anthony Long and Sarah Woodroffe of Durham University Geography Department study maps of Greenland where they are going to study the impact of global warming induced ice sheet melt and isostatic rebound.
 
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IMG_8308_greenland.jpg.jpg Scientists Anthony Long and Sarah Woodroffe of Durham University Geography Department study maps of Greenland where they are going to study the impact of global warming induced ice sheet melt and isostatic rebound.
 
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IMG_8311_research.jpg.jpg Scientists Anthony Long and Sarah Woodroffe of Durham University Geography Department study maps of Greenland where they are going to study the impact of global warming induced ice sheet melt and isostatic rebound.
 
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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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366W2174_global warming_Luing.jpg An interpretation board on the isle of Luing near Oban Scotland UK describing the geology of the ilsand and glaciation
 
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