Taku Glacier seismic reflection survey, Alaska, 2016

The purpose of this experiment was to image sediment deposits beneath the Taku Glacier terminus, to determine their thickness and geometry, and to perform Amplitude Variation with Offset (AVO)
analysis of seismic reflection returns from the glacier bed to learn the nature of the sediments (dilatant
and soft vs. dewatered and stiff). This seismic reflection survey was part of a larger glacier monitoring
project aiming to characterize the relationship between subglacial sediments and the unusual dynamics
of the advancing Taku Glacier terminus. Data report can be found at: https://ds.iris.edu/data/reports/2017/17-006/ Data can be requested at: https://ds.iris.edu/ds/nodes/dmc/forms/assembled-data/?dataset_report_number=17-006