Mantle transition zone topography and low-velocity zone locations in the Yellowstone Region

The data is provided as .xlsx and .csv files. If a cell in the file has a value of zero, no feature greater than one standard deviation was identified in this location. Here is a brief description of each table: Table S1. Seismic stations used in this study. All seismic stations were part of the EarthScope Transportable Array (TA). Table S2. Depths of the interpreted 410-km discontinuity. Table S3. Depths of the interpreted 660-km discontinuity. Table S4. Depths of the interpreted LVZs above the 410-km discontinuity. A zero values indicates no LVZ was interpreted. Table S5. Depths of the interpreted LVZs below the 660-km discontinuity at ~750 km depth. A zero values indicates no LVZ was interpreted. Table S6. Longitude values for grid points of used in Tables S2, Table S3, Table S4, and Table S5. Table S7. Latitude values for grid points of used in Tables S2, Table S3, Table S4, and Table S5. Please cite the article related to this data set as: Frazer, W. D., & Park, J. (2021). Seismic evidence of mid-mantle water transport beneath the Yellowstone region. Geophysical Research Letters, 48, e2021GL095838. https://doi.org/10.1029/2021GL095838 Updated with corrections to Table S3 and Table S4 on 7/14/22.