Global Warming Images
 
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20130311_B18A3342.jpg A forwarder, a specialist machine for cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3347.jpg A forwarder, a specialist machine for cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3351.jpg A forwarder, a specialist machine for cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3359.jpg A forwarder, a specialist machine for cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3389.jpg A forwarder, a specialist machine for cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3402.jpg A forwarder, a specialist machine for moving timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3406.jpg A forwarder, a specialist machine for moving timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3408.jpg A forwarder, a specialist machine for cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3420.jpg A forwarder, a specialist machine for cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3423.jpg A forwarder, a specialist machine for cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3434.jpg A forwarder, a specialist machine for cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3449.jpg A forwarder, a specialist machine for cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_B18A3465.jpg A forwarder, a specialist machine for cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130311_IMG_4464.jpg A forwarder and operator cutting timber in Grizedale Forest, Lake District, UK, that is destined to be used as biofuel in a biofuel power station.
 
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20130223_P2230192.jpg The original steam engine pump in the old sewage pumping station museum in Leicester, UK.
 
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20130223_P2230193.jpg The original steam engine pump in the old sewage pumping station museum in Leicester, UK.
 
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20130223_P2230198.jpg The original steam engine pump in the old sewage pumping station museum in Leicester, UK.
 
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20121229_B18A6198.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6204.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6207.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6211.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6218.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6221.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6224.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_PC290076.jpg A gaping hole left where a massive block of ice detached causing an avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_PC290080.jpg A gaping hole left where a massive block of ice detached causing an avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121230_B18A6778.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121230_PC300115.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121230_PC300117.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121230_PC300122.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121231_B18A6978.jpg Debris from an avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121231_B18A6979.jpg Debris from an avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121223_B18A4561.jpg A man with a huge heavy load in Kathmandu, Nepal.
 
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20121226_B18A5573.jpg Nepalese porters crossing a suspension bridge in the Himalayan foothills, Nepal.
 
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20121229_B18A6210.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6216.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6220.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6222.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6227.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121230_PC300116.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121230_PC300121.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121231_B18A7009.jpg A Porters carying a heavy load of timber on the Annapurna Base Camp Trek, Himalayas, Nepal.
 
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20121231_B18A7014.jpg A Porters carying a heavy load of timber on the Annapurna Base Camp Trek, Himalayas, Nepal.
 
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20121223_B18A4551.jpg A man with a huge heavy load in Kathmandu, Nepal.
 
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20121223_B18A4563.jpg A man with a huge heavy load in Kathmandu, Nepal.
 
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20121231_B18A6955.jpg Nepalese porters at Annapurna Base Camp in the Himalayas, Nepal.
 
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20121231_B18A7020.jpg A Porters carying a heavy load of timber on the Annapurna Base Camp Trek, Himalayas, Nepal.
 
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20130102_B18A7244.jpg An old nepalese woman carrying a heavy load in the Himalayan foothills.
 
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20120807IMG_0451.jpg A V8 RAM truck in Fort McMurray, Alberta, Canada.
 
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20120807IMG_0452.jpg A V8 RAM truck in Fort McMurray, Alberta, Canada.
 
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20120514_IMG_9874.jpg Motorbikes at a road junction in London, UK.
 
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20120508_IMG_7000.jpg The tide rip at Glenelg between the Isle of Skye and the mainland. The tide rip here is vey powerful, and there are plans to site a tidal energy device to generate electricity from this natural, reliable renewable energy source.
 
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20120508_IMG_7002.jpg The tide rip at Glenelg between the Isle of Skye and the mainland. The tide rip here is vey powerful, and there are plans to site a tidal energy device to generate electricity from this natural, reliable renewable energy source.
 
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20120508_IMG_7005.jpg The tide rip at Glenelg between the Isle of Skye and the mainland. The tide rip here is vey powerful, and there are plans to site a tidal energy device to generate electricity from this natural, reliable renewable energy source.
 
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20120508_IMG_7026.jpg The tide rip at Glenelg between the Isle of Skye and the mainland. The tide rip here is vey powerful, and there are plans to site a tidal energy device to generate electricity from this natural, reliable renewable energy source.
 
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20120508_IMG_7029.jpg The tide rip at Glenelg between the Isle of Skye and the mainland. The tide rip here is vey powerful, and there are plans to site a tidal energy device to generate electricity from this natural, reliable renewable energy source.
 
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IMG_8566_helmet.jpg The jack up barge, The Goliath lifting a transition pieces into place on the Walney Offshore windfarm project, off Barrow in Furness, Cumbria, UK. When finished it will have 102, 3.6 MW turbines, giving a total capacity of the Walney project of 367.2 MW, enough to power 320,000 homes. The rotor diameter of the turbines is 107m for Walney 1 and 120 m for Walney 2. The wind farm is owned and constructed by Dong Energy.
 
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IMG_8593_high vis.jpg A crane on the jack up barge, Goliath.
 
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IMG_8659_life vest.jpg A massive crane lifts a 320 tonne transition piece onto the deck of the jack up barge, The Goliath ready to take out to the Walney Offshore windfarm project, off Barrow in Furness, Cumbria, UK. When finished it will have 102, 3.6 MW turbines, giving a total capacity of the Walney project of 367.2 MW, enough to power 320,000 homes. The rotor diameter of the turbines is 107m for Walney 1 and 120 m for Walney 2. The wind farm is owned and constructed by Dong Energy.
 
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IMG_9070_male.jpg The Walney offshore wind farm consists of 102, 3.6 MW turbines, giving a total capacity of the Walney project of 367.2 MW, enough to power 320,000 homes. The rotor diameter of the turbines is 107m for Walney 1 and 120 m for Walney 2. The wind farm is owned and constructed by Dong Energy. Cumbria, UK.
 
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IMG_9222_man.jpg A blade on a turbine at the Walney offshore wind farm consists of 102, 3.6 MW turbines, giving a total capacity of the Walney project of 367.2 MW, enough to power 320,000 homes. The rotor diameter of the turbines is 107m for Walney 1 and 120 m for Walney 2. The wind farm is owned and constructed by Dong Energy. Cumbria, UK.
 
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IMG_9531_sunglasses.jpg Airplane contrails over the Walney offshore wind farm consists of 102, 3.6 MW turbines, giving a total capacity of the Walney project of 367.2 MW, enough to power 320,000 homes. The rotor diameter of the turbines is 107m for Walney 1 and 120 m for Walney 2. The wind farm is owned and constructed by Dong Energy. Cumbria, UK.
 
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IMG_9930_shades.jpg A turbine at the Walney offshore wind farm which consists of 102, 3.6 MW turbines, giving a total capacity of the Walney project of 367.2 MW, enough to power 320,000 homes. The rotor diameter of the turbines is 107m for Walney 1 and 120 m for Walney 2. The wind farm is owned and constructed by Dong Energy. Cumbria, UK.
 
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IMG_9981_PPE.jpg The Ormonde Offshore Wind Farm is currently being built in the Irish Sea, 10km off Barrow-In-Furness. On completion the wind farm will comprise 30 RePower 5M wind turbines with the capacity of 150 megawatts and expected to produce around 500 gigawatt hours of electricity every year. These turbines are some of the most powerful wind turbines in the world,
 
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