Marine Geological and Geophysical Research - Mid-Ocean Ridge and Subduction Zone Processes
We examine the flow of energy and materials from the Earth's interior, through the ocean crust and its associated hydrothermal systems, and into the deep sea. The School of Oceanography's proximity to the Juan de Fuca/Gorda Ridge system and Cascadia subduction zone provides ready access to an ideal natural laboratory for study of the active components of a geological plate. This local focus is complemented by additional work along the global mid-ocean ridge.
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