Stanford geophysicists have compiled the most detailed maps yet of the geologic forces controlling the locations, types and magnitudes of earthquakes in Texas and Oklahoma.

These new “stress maps,” published in the journals Geophysical Research Letters and Bulletin of the Seismological Society of America, provide insight into the nature of the faults associated with recent temblors, many of which appear to have been triggered by the injection of wastewater deep underground.

“These maps help explain why injection-induced earthquakes have occurred in some areas, and provide a basis for making quantitative predictions about the potential for seismic activity resulting from fluid injection,” said study co-author Mark Zoback, the Benjamin M. Page Professor of Geophysics in Stanford’s School of Earth, Energy & Environmental Sciences.

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La influencia de las corporaciones que lucran con combustibles fósiles fue fuertemente cuestionada por los países en desarrollo en la reunión posterior a París de las negociaciones sobre el cambio climático en Bonn la semana pasada. Los seguidores del clima Pavlos Georgiadis, Renee Karunungan y Anna Pérez Català destacan las cuestiones clave que se debatieron.

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The Alps are steadily “growing” by about one to two millimeters per year. Likewise, the formerly glaciated subcontinents of North America and Scandinavia are also undergoing constant upward movement. This is due to the fact that at the end of the Last Glacial Maximum (LGM) about 18,000 years ago the glaciers melted and with this the former heavy pressure on the Earth’s surface diminished. The ice reacted rapidly to climate change at that time whereas the Earth’s crust is still responding today to this relatively sudden melting of ice. 

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Los Alpes están "creciendo" constantemente alrededor de uno a dos milímetros por año. Asimismo, los antiguos subcontinentes glaciares de Norteamérica y Escandinavia también están experimentando constantes movimientos ascendentes. 

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The dramatic decline of Iran’s Lake Urmia—once the second-largest hypersaline lake in the world—has both direct human and climatic causes, according to a new study published in the Journal of Great Lakes Research.   The study was the first to compare the relative impact of climate and water management on the water flowing into the lake.

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A medida que aumentan los niveles de dióxido de carbono atmosférico (CO2), muy pocos ecosistemas de arrecifes de coral podrán evitar el impacto de la acidificación de los océanos o la subida de la temperatura de la superficie del mar, según un nuevo análisis. El daño causará las amenazas más inmediatas y serias donde la dependencia humana de los arrecifes es más alta.

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