Abstract
This article investigates the properties of small-scale fluctuations of the probability density formeasurements of the X, Y, and Z-components of the Earth’s magnetic field that were carried out both in aseismically active region and in an area with a complete absence of seismic activity. In the first case, a muchgreater intensity of the occurrence of statistical phenomena considered as earthquake precursors was revealed.At an interval of several days before the earthquake with a magnitude of 5.3 in Metsavan (Armenia), whoseepicenter was located near the magnetic variation station in a seismically active region, a sharp increase in thefrequency of these phenomena was found. This effect was absent in the seismically quiet region
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