In 2020, two significant earthquakes were registered in the south of the Republics of North Ossetia-Alania and Ingushetia: on January 26 with KR=11.2 and on May 24 with KR=10.6. The earthquakes occurred in different seismotectonic conditions. The source of the first event was formed within the Adaykom Kazbek fault, and the source of the second event – within the Karmadon zone of occurrence of earthquake sources. The January 26 earthquake, named the Verkhne-Fiagdon, became the strongest instrumentally recorded earthquake in North Ossetia since the beginning of seismological observations on this territory. It was felt in 19 settlements with the intensity from 2 to 4–5. The calculated intensity in the epicenter is estimated as I0=5. According to the focal mechanism solution, the Verkhne-Fiagdon earthquake occurred under the influence of prevailing compres sive stress. The type of movement in the focus is reverse fault with significant strike-slip component. The earth quake on May 24, named the Jeyrakh earthquake, was felt in 12 settlements with intensity from 2 to 4. Tensile stresses oriented in a south-west direction prevailed in the focus. The type of movement is a normal fault on both planes, with minor strike-slip components. Information on historical seismicity in the focal zones of both earth quakes is given for the last 150 years.
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