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  1. Recorded in Zagreb, 51 km (32 mi) from epicenter. The earthquake had a magnitude of 6.4 M w and a depth of 10 kilometres (6.2 mi) according to Advanced National Seismic System (ANSS) [1] and European-Mediterranean Seismological Centre (EMSC), [14] while the Seismological Survey of Croatia recorded 6.2 ML.

  2. May 8, 2021 · This paper highlights the principal features of the Mw5.4 Zagreb earthquake. Located within the city limits at a depth of 10 km, the earthquake generated a peak ground acceleration of more than 0.2 g and a maximum spectral acceleration of about 0.6 g at 0.1 s in the historic downtown area. The situation was particularly challenging since the event occurred amid a partial Covid-19 lockdown at ...

    • Josip Atalić, Mario Uroš, Marta Šavor Novak, Marija Demšić, Miroslav Nastev
    • 2021
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  4. Dec 29, 2020 · The European Mediterranean Seismological Center said a magnitude 6.3 quake hit 28 miles southeast of Zagreb. It caused widespread damage in the hardest-hit town of Petrinja.

  5. Dec 29, 2020 · A magnitude 6.4 earthquake struck near Petrinja, Croatia, about 30 miles southeast of the capital of Zagreb, on December 29, 2020 at about 6:20 am Eastern Time (12:20 pm local time). Seismic instruments indicate the earthquake originated at a depth of about 6 miles (10 kilometers).

  6. Dec 30, 2020 · Zagreb, Croatia CNN —. At least seven people were killed and dozens were injured after a powerful 6.4 magnitude earthquake struck central Croatia on Tuesday, according to the US Geological ...

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  7. Mar 22, 2020 · In just over 24 h since the main shock, 57 earthquakes with magnitudes greater than or equal to 2.0 occurred in Zagreb. The M5.5 earthquake that struck Zagreb on 22 March 2020 caused more damage than would be expected for an earthquake of this magnitude.

  8. Jan 18, 2023 · Although strong and damaging earthquakes have hit Zagreb in the past, the 22 March 2020 earthquake (Mw 5.4) is the first one that was recorded by a modern digital local seismic network, and which could be analysed not only by macroseismic methods, but also by microseismic ones.

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