Global Warming Images
 

 
IMG_6300_winter.jpg Whitburn Windmill in Whitburn between Sunderland and Newcastle, North East, UK.
 
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IMG_6301_glow.jpg Whitburn Windmill in Whitburn between Sunderland and Newcastle, North East, UK.
 
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IMG_6303_grinding.jpg Whitburn Windmill in Whitburn between Sunderland and Newcastle, North East, UK.
 
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IMG_6304_North East.jpg Whitburn Windmill in Whitburn between Sunderland and Newcastle, North East, UK.
 
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IMG_6306_North Sea.jpg Whitburn Windmill in Whitburn between Sunderland and Newcastle, North East, UK.
 
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IMG_6310_sail.jpg Whitburn Windmill in Whitburn between Sunderland and Newcastle, North East, UK.
 
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IMG_6312_windmill.jpg Whitburn Windmill in Whitburn between Sunderland and Newcastle, North East, UK.
 
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IMG_2459_orkney.jpg The remains of an old Water mill near Stromness on Mainland Orkney, Scotland, UK.
 
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IMG_4017_heritage.jpg The Click Mill an ancient water mill for grinding grain on Orkney's Mainland, Scotland, UK.
 
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IMG_4022_water mill.jpg The Click Mill an ancient water mill for grinding grain on Orkney's Mainland, Scotland, UK.
 
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IMG_4024_click mill.jpg The Click Mill an ancient water mill for grinding grain on Orkney's Mainland, Scotland, UK.
 
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IMG_4027_mill.jpg The Click Mill an ancient water mill for grinding grain on Orkney's Mainland, Scotland, UK.
 
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IMG_4030_water mill.jpg The Click Mill an ancient water mill for grinding grain on Orkney's Mainland, Scotland, UK.
 
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IMG_4031_mill stone.jpg The Click Mill an ancient water mill for grinding grain on Orkney's Mainland, Scotland, UK.
 
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IMG_4032_grind stone.jpg The Click Mill an ancient water mill for grinding grain on Orkney's Mainland, Scotland, UK.
 
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IMG_4036_click mill.jpg The Click Mill an ancient water mill for grinding grain on Orkney's Mainland, Scotland, UK.
 
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IMG_4325_water mill.jpg The remains of an old Water mill near Stromness on Mainland Orkney, Scotland, UK.
 
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IMG_4328_water wheel.jpg The remains of an old Water mill near Stromness on Mainland Orkney, Scotland, UK.
 
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IMG_0081_volcanic cinder.jpg On 23 January 1973 a 2 km long fissure opened up spewing out lava forming a new vocanoe, Eldfell. The lava flow threatened Heimaey town, on Heimaey in the Westmand Islands off Iceland's south coast. The lava and ash buried and destroyed one third of the town and threatened the harbour, the life line for the islands. The whole island was evacuated. A novel technique of pumping sea water onto the lava front, solidified the flowing mass and diverted the lava flow away from the harbour. When the eruption ceased in June, Heimaey was 2km bigger. Recently an archaeological excavation has strted to uncover houses that were buried by the volcanic ash 37 years ago.
 
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IMG_0082_volcanic ash.jpg On 23 January 1973 a 2 km long fissure opened up spewing out lava forming a new vocanoe, Eldfell. The lava flow threatened Heimaey town, on Heimaey in the Westmand Islands off Iceland's south coast. The lava and ash buried and destroyed one third of the town and threatened the harbour, the life line for the islands. The whole island was evacuated. A novel technique of pumping sea water onto the lava front, solidified the flowing mass and diverted the lava flow away from the harbour. When the eruption ceased in June, Heimaey was 2km bigger. Recently an archaeological excavation has strted to uncover houses that were buried by the volcanic ash 37 years ago.
 
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IMG_0084_archaeology.jpg On 23 January 1973 a 2 km long fissure opened up spewing out lava forming a new vocanoe, Eldfell. The lava flow threatened Heimaey town, on Heimaey in the Westmand Islands off Iceland's south coast. The lava and ash buried and destroyed one third of the town and threatened the harbour, the life line for the islands. The whole island was evacuated. A novel technique of pumping sea water onto the lava front, solidified the flowing mass and diverted the lava flow away from the harbour. When the eruption ceased in June, Heimaey was 2km bigger. Recently an archaeological excavation has strted to uncover houses that were buried by the volcanic ash 37 years ago.
 
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IMG_0094_excavation.jpg On 23 January 1973 a 2 km long fissure opened up spewing out lava forming a new vocanoe, Eldfell. The lava flow threatened Heimaey town, on Heimaey in the Westmand Islands off Iceland's south coast. The lava and ash buried and destroyed one third of the town and threatened the harbour, the life line for the islands. The whole island was evacuated. A novel technique of pumping sea water onto the lava front, solidified the flowing mass and diverted the lava flow away from the harbour. When the eruption ceased in June, Heimaey was 2km bigger. Recently an archaeological excavation has strted to uncover houses that were buried by the volcanic ash 37 years ago.
 
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IMG_0108_buried.jpg On 23 January 1973 a 2 km long fissure opened up spewing out lava forming a new vocanoe, Eldfell. The lava flow threatened Heimaey town, on Heimaey in the Westmand Islands off Iceland's south coast. The lava and ash buried and destroyed one third of the town and threatened the harbour, the life line for the islands. The whole island was evacuated. A novel technique of pumping sea water onto the lava front, solidified the flowing mass and diverted the lava flow away from the harbour. When the eruption ceased in June, Heimaey was 2km bigger. Recently an archaeological excavation has strted to uncover houses that were buried by the volcanic ash 37 years ago.
 
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IMG_2001_well.jpg Sancreed Well at Sancreed, Cornwall, UK. It is probably pre christian in date.
 
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IMG_3484_sancreed.jpg Sancreed Well at Sancreed, Cornwall, UK. It is probably pre christian in date.
 
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IMG_3488_sancreed well.jpg Sancreed Well at Sancreed, Cornwall, UK. It is probably pre christian in date, with clouties hung on a nearby tree.
 
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IMG_0464_sunset.jpg Sunset over Cape Cornwall, Cornwall, UK.
 
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IMG_0480_Cape Cornwell.jpg Sunset over Cape Cornwall, Cornwall, UK.
 
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IMG_2377_double decker.jpg An open topped double decker bus travelling through the Cornish countryside and passing Bosigran tin mine, UK.
 
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IMG_0533_porlock weir.jpg Tree trunks preserved in a submarine forest revealed at low tide at Porlock Weir in Somerset, UK. The submarine forest is evidence of a lower sea level caused by water being locked on the land as ice during the last ice age. Since then the sea level has risen submeriging the forest remains which are only visible at low tides. As climate change accelerates, sea levels are rising around the world.
 
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IMG_0534_submarine forest.jpg Tree trunks preserved in a submarine forest revealed at low tide at Porlock Weir in Somerset, UK. The submarine forest is evidence of a lower sea level caused by water being locked on the land as ice during the last ice age. Since then the sea level has risen submeriging the forest remains which are only visible at low tides. As climate change accelerates, sea levels are rising around the world.
 
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IMG_0535_porlock weir.jpg Tree trunks preserved in a submarine forest revealed at low tide at Porlock Weir in Somerset, UK. The submarine forest is evidence of a lower sea level caused by water being locked on the land as ice during the last ice age. Since then the sea level has risen submeriging the forest remains which are only visible at low tides. As climate change accelerates, sea levels are rising around the world.
 
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