Marco Walter and Manfred Joswig present the results of an application of nanoseismic monitoring (see separate article by Joswig) in which seismic mini-arrays were deployed on the creeping Heumoes landslide (HL) in the Vorarlberg Alps, Austria in an attempt to detect seismic activity possibly generated by the unstable landmass, consisting of glacial sediments.
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Walter et al. (2008) studied this question.