Tornillo event
Seismic event associated with volcanoes
A tornillo event is a low-frequency seismic event associated with volcanoes. The term, which means "screw" in Spanish, was coined in the mid-1990s at the Observatorio Vulcanológico y Sismológico de Pasto (OVSP) in Pasto, Colombia to describe seismic events seen at the Galeras volcano.
A tornillo has the following characteristics that distinguish it from other seismic events:
- very limited distribution of frequencies (monochromatic)
- a long coda that decays slowly
- small amplitude
Like volcanic tremor, tornillos are thought to be caused by magma moving at depth.
References
- Tornillo-type seismic signals at Galeras volcano, Colombia, 1992−1993
External links
- Observatorio Vulcanológico y Sismológico de Pasto - INGEOMINAS
