Earthquakes occurring on the territory of Poland release relatively small amounts of energy. Epicentres of these earthquakes cluster along fault zones in the Sudetes, in the Carpathian Mountains in the region of Cieszyn, Pieniny Klippen Belt, Zakopane and Krynica, as well as along the Teisseyre-Tornquist Zone. In the last decade a dozen or so weak events have been marked. For the reference of neotectonic processes, seismological information has some limitation, the fundamental of which is the low quality of the evaluation of focal depth.
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