Supplemental Material: Linking exhumation, paleo-relief, and rift formation to magmatic processes in the western Snake River Plain, Idaho, using apatite (U-Th)/He thermochronology

Table S1: Calculations of footwall exhumation and basin extension magnitudes in the western Snake River Plain. Figure S1: Figure illustrating regions of high-elevation, low-relief topography in the southern Idaho batholith.