“…However, only very recent developments of portable seismic rotation and strain sensors made the direct observations of seismic wavefield gradients possible for a broad range of applications, such as volcanology [ 5 , 6 , 7 ], ocean bottom seismology [ 8 , 9 , 10 ], structural health monitoring [ 11 , 12 , 13 ], seismic exploration [ 14 , 15 , 16 , 17 ], microzonation in urban environments [ 18 ], and glaciology [ 19 ]. The most commonly used technologies for seismic ground rotation sensing are fiber-optic Sagnac interferometry [ 20 ], micro-electro mechanical systems [ 21 ], small-scale finite differencing within a rigid configuration of translation sensors [ 22 ], and liquid-based electrochemical transducers [ 23 ]. The technology of distributed acoustic sensing (DAS) makes the observation of seismically induced axial strain in temporary field experiments possible [ 24 , 25 , 26 , 27 ].…”