Emilie Hooft, Department of Earth Sciences
Emilie Hooft is an academic expert in how magma is transported from Earth’s mantle to the surface. She also studies the structure of the Cascadia subduction zone. Emilie has investigated the entire spectrum of the volcanic activity on Earth. To do this she collects and analyzes geophysical data. She has led research expeditions to the Cascadia margin, oceanic spreading centers, and volcanic hotspots (Galapagos and Iceland). Current research includes imaging the magma plumbing pathways beneath subduction zone volcanoes (Newberry, OR, and Santorini, Greece) using dense geophysical data and inverse modeling on high performance computers. At the University of Oregon, she is an associate professor in the Department of Earth Sciences.
Contact: email@example.com | 541-346-1455
Quack Chats explores the insides of the world’s great volcanoes (Around the O, May 17, 2019)
We probed Santorini’s volcano with sound to learn what’s going on beneath the surface (The Conversation, June 24, 2019)
Pieces of mantle found rising under north and south ends of Cascadia fault (EurekAlert!, July 24, 2018)
Earthquake hazard report reflects a compromise (Around the O, April 19, 2019)
UO-led expedition probes undersea magma system (Around the O, Jan. 11, 2016