Collision course: A geological mystery in the Himalayas
MIT geologists use paleomagnetism to determine the chain of events that resulted in the Himalayan mountains, with the support of MISTI-India.
MIT geologists use paleomagnetism to determine the chain of events that resulted in the Himalayan mountains, with the support of MISTI-India.
Results show a rupture of the San Andreas Fault could generate three times more shaking in Los Angeles than surrounding regions.
Researchers find immense heating at high pressures helps spread intermediate-depth quakes.
Created by OEIT's ARTEMiS group, the Plate Tectonics interactive visualization challenges students to interpret a 3-D globe of tectonic data, providing animations of the opening and closing of ocean basins and the splitting of Pangaea.
Research points to large reservoirs of material deep in the mantle that may help to explain Earth’s origins.
New timeline suggests India’s size before this collision was much smaller than generally assumed.
Deformation caused by colliding tectonic plates may threaten Azerbaijani capital, oil supplies to Europe.
New data finds regions of North America have remained extremely stable for more than one billion years.