Taku Glacier seismic reflection survey, Alaska, 2015

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...

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Bibliographic Details
Main Authors: Martin Truffer, Chris Larsen, Roman Motyka, Alessio Gusmeroli, Jason Amundson, Jeffrey Kavanaugh
Format: Dataset
Language:unknown
Published: Arctic Data Center
Subjects:
Taku
glacier
Alaska
Online Access:https://doi.org/10.18739/A2125Q848
Description
Summary: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 solid). 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/2016/16-007/ Data can be requested at: https://ds.iris.edu/ds/nodes/dmc/forms/assembled-data/?dataset_report_number=16-007

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