We measure electric charge in the atmosphere near sea level to detect anomalies that may indicate impending seismic activity in specific regions in the world. Estimated regions are marked at a thin line, which is perpendicular to the plane of the ecliptic. The strength of an anomaly indicates seismic potential whereby 2.0-2.5 mV ≤ M 6 (strong), and 3.0-5.0 mV ≥ M 7 (major) approximately. Actual seismic activity depends on local tectonic stress levels, which is an unknown factor. There is no guarantee that a larger earthquake will occur.

Atmosphere broadcast channels
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Earthquake broadcast channels
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