Global seismographic networks (GSNs) emerged during the late nineteenth and early
twentieth centuries, facilitated by seminal international developments in theory, technology …

The discovery of slow-slip phenomena has revolutionized our understanding of how faults
accommodate relative plate motions. Faults were previously thought to relieve stress either …

The last decade witnessed an explosion in yearly number of publications on passive glacier
seismology. The seismic signals from a wide range of glacier‐related processes fill a broad …

Environmental seismology consists in studying the mechanical vibrations that originate from,
or that have been affected by external causes, that is to say causes outside the solid Earth …

Two ice-dynamic transitions of the Antarctic ice sheet–the boundary of grounded ice features
and the freely-floating boundary–are mapped at 15-m resolution by participants of the …

Ocean tides are the main source of high‐frequency variability in the vertical and horizontal
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …

The slip of glaciers over the underlying bed is the dominant mechanism governing the
migration of ice from land into the oceans, with accelerating slip contributing to sea-level …

Advances in machine learning (ML) techniques and computational capacity have yielded
state‐of‐the‐art methodologies for processing, sorting, and analyzing large seismic data …

Glaciological observations of under‐flooding suggest that fluid‐induced hydraulic fracture of
an ice sheet from its bed sometimes occurs quickly, possibly driven by turbulently flowing …

Seismic source and wave propagation studies contribute to understanding structure,
transport, fracture mechanics, mass balance, and other processes within glaciers and …