Columbia geophysical hazards scientist says evidence shows dam reservoir likely triggered China’s great quake of 2008

(January 26, 2009) Christian Klose, a geophysical hazards research scientist from Columbia University in New York, says geophysical data suggests that the Zipingpu dam reservoir — just a few kilometers from the epicenter of China’s great quake of 2008 — likely triggered the deadly quake and explains how it happened.

Papua New Guinea and China’s New Empire

(January 3, 2009) In less than a decade, China has spun a web of strategic investments that stretches from Latin America to the former Soviet Union, from the remotest islands of the South Pacific to the huge oil fields of Angola and Sudan. In a range of resource-rich countries, China is diligently cultivating its interests. The Globe and Mail’s Geoffrey York

Water brief: Three Gorges Dam

(January 1, 2009) In The World’s Water 2008-2009, the Pacific Institute’s Dr. Gleick examines the usual anticipated benefits of the Three Gorges Dam: power, navigation and flood control and the growing list of problems — serious impacts on fisheries, coastal erosion due to vastly lower sediment flow in the Yangtze, landslides, earthquakes and social unrest due to the displacement of millions of people.

Ecuador hangs tough

(January 1, 2009) After months of threats, the government of Ecuador has made good on its promise to forego payment of foreign loans deemed illegitimate by the country’s debt audit commission. Ecuadorian President Rafael Correa announced that his country would not be paying $30.6 million interest due Dec. 15 on its 2012 global bonds after the commission claimed the debt had been ‘illegally’ acquired by past administrations.

China quakes, but the dams don’t break

(December 28, 2008) The biggest potential disaster, Pearce reports, was averted at the Zipingpu dam, just 17 kilometres from the quake’s epicenter. “Holding back more than a cubic kilometer of water … the hydroelectric dam was the largest of a new, cheap design with a rock core and concrete face. As the tight valley sides juddered, the structure was squeezed and ended up 18 centimeters downstream, and 70 cm lower. … The concrete was ripped apart but the core of the dam survived.”