Phase D, an elastically anisotropic hydrous mineral, is stable around cold subducting slabs at depths of mid mantle, potentially being the source of seismic anisotropy.

To figure out just where that earthquake happened, you need recordings from seismic stations in other places. While earthquake locations are normally done with a computer that can quickly determine ...

Ground motion is registered in several seismic stations across Finland. Data are automatically processed at Institute of Seismology: signals caused by explosions, earthquakes and collapses are ...

The impact of a large section of a cliff collapse at St Peter's Pool, Delimara late on Wednesday night, has been recorded on the University of Malta's seismic stations. The Seismic Monitoring and ...

Seismic events in Finland and adjacent areas on map Institute of Seismology monitors the seismicity of Finland and adjacent areas using an observation station network. In addition, the institute ...