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Abstract: Flaring up: discrete magma bodies within a deep, vertically extensive transcrustal magmatic system fueled the Tuff of Elevenmile Canyon supereruption (AGU25)

Flaring up: discrete magma bodies within a deep, vertically extensive transcrustal magmatic system fueled the Tuff of Elevenmile Canyon supereruption

Anna C Ruefer, Stanford University, Earth & Planetary Sciences, Stanford, United States, Ayla S Pamukcu, Stanford University, Department of Earth & Planetary Sciences, Stanford, United States, Genna Chiaro, U.S. Geological Survey, Moffett Field, United States, Madeline J Lewis, University of Wyoming, Laramie, United States, Michael Patterson Eddy, Purdue University, Earth, Atmospheric, & Planetary Sciences, West Lafayette, United States, Karrie L Weaver, Stanford University, Stanford, CA, United States and Joel William DesOrmeau, University of Nevada Reno, Department of Geological Sciences and Engineering, Reno, NV, United States