| Summary: | Subglacial tills play an important role in glacier dynamics but are difficult to characterize in situ. Amplitude Variation with Angle (AVA) analysis of seismic reflection data can distinguish between stiff tills and deformable tills. Subglacial tills play an important role in glacier dynamics but are difficult to characterize in situ. Amplitude Variation with Angle (AVA) analysis of seismic reflection data can distinguish between stiff tills and deformable tills. However, AVA analysis in mountain glacier environments can be problem- atic: reflections can be obscured by Rayleigh wave energy scattered from crevasses, and complex basal topography can impede the location of reflection points in 2-D acquisitions. We use a forward model to produce challenging synthetic seismic records in order to test the efficacy of AVA in crevassed and geo- metrically complex environments. We find that we can distinguish subglacial till types in moderately cre- vassed environments, where ‘moderate’ depends on crevasse spacing and orientation. The forward model serves as a planning tool, as it can predict AVA success or failure based on characteristics of the study glacier. Applying lessons from the forward model, we perform AVA on a seismic dataset col- lected from Taku Glacier in Southeast Alaska in March 2016. Taku Glacier is a valley glacier thought to overlay thick sediment deposits. A near-offset polarity reversal confirms that the tills are deformable. The Taku 2016 survey was made possible by input and assist- ance from Thomas Hart (blaster), Aurora Roth, and Andy Aschwanden. IRIS PASSCAL provided seismic recording equipment for the Taku 2016 seismic survey. Thanks to Peter Burkett, Sridhar Anandakrishnan and Kiya Riverman for instrument support, and to Bernard Coakley, Bernard Hallet, Esther Babcock and some anonymous reviewers for their input and advice. Also thanks to the Consortium for Research in Elastic Wave Exploration Seismology (CREWES) for providing Matlab scripts that facilitated the seismic forward modeling. ...
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