Abstract
Glacial earthquakes are slow slip-events located under major outlet glaciers. These peculiar events were first discovered by Ekstrom et al in 2003 using teleseismic data and a global detection algorithm based on surface waves. The waveforms are consistent with a landslide-type focal mechanism, thus indicating that the seismological signals are linked to glacier movements.
| Original language | English |
|---|---|
| Article number | EGU2007-A-03541 |
| Number of pages | 1 |
| Journal | Geophysical Research Abstracts |
| Volume | 9 |
| Publication status | Published - 2007 |
| Event | EGU General Assembly 2007 - Vienna, Austria Duration: 16 Apr 2007 → 20 Apr 2007 |
Programme Area
- Programme Area 3: Energy Resources
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