Global Warming Images
 
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IMG_3771_high voltage.jpg Electricity pylons traversing over Bwlch Y Ddeufaen on the edge of the Snowdonia Mountains, North Wales, carrying electricity from Dolgarrog hydro electric power station.
 
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IMG_3774_transmission.jpg Electricity pylons traversing over Bwlch Y Ddeufaen on the edge of the Snowdonia Mountains, North Wales, carrying electricity from Dolgarrog hydro electric power station.
 
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IMG_3776_electricity.jpg Electricity pylons traversing over Bwlch Y Ddeufaen on the edge of the Snowdonia Mountains, North Wales, carrying electricity from Dolgarrog hydro electric power station.
 
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IMG_3779_pylon.jpg Electricity pylons traversing over Bwlch Y Ddeufaen on the edge of the Snowdonia Mountains, North Wales, carrying electricity from Dolgarrog hydro electric power station.
 
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IMG_3781_Snowdonia.jpg Electricity pylons traversing over Bwlch Y Ddeufaen on the edge of the Snowdonia Mountains, North Wales, carrying electricity from Dolgarrog hydro electric power station.
 
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IMG_3783_pylon.jpg Electricity pylons traversing over Bwlch Y Ddeufaen on the edge of the Snowdonia Mountains, North Wales, carrying electricity from Dolgarrog hydro electric power station.
 
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IMG_3786_energy distribution.jpg Electricity pylons traversing over Bwlch Y Ddeufaen on the edge of the Snowdonia Mountains, North Wales, carrying electricity from Dolgarrog hydro electric power station.
 
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IMG_3788_power distribution.jpg Electricity pylons traversing over Bwlch Y Ddeufaen on the edge of the Snowdonia Mountains, North Wales, carrying electricity from Dolgarrog hydro electric power station.
 
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IMG_3797_national grid.jpg Electricity pylons traversing over Bwlch Y Ddeufaen on the edge of the Snowdonia Mountains, North Wales, carrying electricity from Dolgarrog hydro electric power station.
 
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IMG_4600_electricity.jpg Electricity pylons traversing over Bwlch Y Ddeufaen on the edge of the Snowdonia Mountains, North Wales, carrying electricity from Dolgarrog hydro electric power station.
 
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IMG_4601_pylon.jpg Electricity pylons traversing over Bwlch Y Ddeufaen on the edge of the Snowdonia Mountains, North Wales, carrying electricity from Dolgarrog hydro electric power station.
 
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IMG_3262_coastal protection.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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IMG_3268_Kinmel Bay.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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IMG_3275_caravan park.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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IMG_3369_pumping station.jpg A sign for a pumping station at Talacre on the North Wales coast. This section of coast is reclaimed salt marsh and is only kept dry by pumping. It is increasingly threatened by climate change driven sea level rise.
 
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IMG_3408_coastal pumping.jpg A pumping station at Talachre on the North Wales coast. This section of coast is reclaimed salt marsh and is only kept dry by pumping. It is increasingly threatened by climate change driven sea level rise.
 
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IMG_3414_Talacre.jpg A pumping station at Talachre on the North Wales coast. This section of coast is reclaimed salt marsh and is only kept dry by pumping. It is increasingly threatened by climate change driven sea level rise.
 
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IMG_3416_Point of Ayr.jpg A pumping station at Talachre on the North Wales coast. This section of coast is reclaimed salt marsh and is only kept dry by pumping. It is increasingly threatened by climate change driven sea level rise.
 
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IMG_3418_pumping.jpg A pumping station at Talachre on the North Wales coast. This section of coast is reclaimed salt marsh and is only kept dry by pumping. It is increasingly threatened by climate change driven sea level rise.
 
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IMG_3440_dune restoration.jpg A dune restoration project at the Point of Ayr on the North Wales coast. Sand dunes are important for natural coastal protection, and increasingly important due to climate change driven sea level rise.
 
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IMG_3442_point of ayr.jpg A dune restoration project at the Point of Ayr on the North Wales coast. Sand dunes are important for natural coastal protection, and increasingly important due to climate change driven sea level rise.
 
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IMG_3445_sand dune.jpg A dune restoration project at the Point of Ayr on the North Wales coast. Sand dunes are important for natural coastal protection, and increasingly important due to climate change driven sea level rise.
 
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IMG_3456_sand dunes.jpg A dune restoration project at the Point of Ayr on the North Wales coast. Sand dunes are important for natural coastal protection, and increasingly important due to climate change driven sea level rise.
 
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IMG_3554_bungalow.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These bungalows in Prestatyn are part of the area at risk.
 
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IMG_3556_insurance risk.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These bungalows in Prestatyn are part of the area at risk.
 
IMG_3556_insurance risk
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IMG_3557_Prestatyn.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These bungalows in Prestatyn are part of the area at risk.
 
IMG_3557_Prestatyn
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IMG_3559_flood risk.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These bungalows in Prestatyn are part of the area at risk.
 
IMG_3559_flood risk
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IMG_3566_bungalow.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These bungalows in Prestatyn are part of the area at risk.
 
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IMG_3575_flood evacuation.jpg A flood evacuation sign on a caravan park in Towyn, which is very susceptible to coastal flooding.
 
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IMG_3582_holiday park.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay.
 
IMG_3582_holiday park
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IMG_3584_caravan park.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay.
 
IMG_3584_caravan park
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IMG_3593_sea wall.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These rocks have been placed to try and re-inforce the sea wall.
 
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