
The Yellowstone Plume, Columbia River flood basalts, and the making of the Pacific NW
The geologic hotspot that causes the volcanic activity in Yellowstone National Park was responsible for making most of the outstanding landscapes we see in the Pacific NW. This is largely due to what it initiated in Earth's crust and upper mantle that was ripe for reconstruction. Our presentation will focus on the Columbia River flood basalt event. By imaging structures in the upper mantle, we get clues that tell a fascinating story of plume-lithosphere interaction. But more than this, the imaging reveals the history of the subduction of the ancient Farallon plate that sets the stage for the Columbia River basalts, and we are drawn into the story of the entire Pacific NW.
Register for the Zoom event here (no charge for registration). Note: Zoom will open at 7:00 to allow participants to visit, the program will begin at 7:30.
Speaker Bio:
Dr. Gene Humphries grew up on the Columbia River basalts in eastern Washington, but didn't know it. After attending many schools, he ended up at Caltech where he earned his PhD in 1985. He has been working at the University of Oregon ever since. His main interest is in continental tectonics; his main technical skill is in seismic imaging.