Naslov
Earthquakes of 1838 and 1839 in the Slovene Hills (Slovenia) – Međimurje (Croatia) area

Autori
Herak, Marijan ; Herak, Davorka ; Živčić, Mladen ; Vrkić, Iva

Izvornik
Geofizika (1846-6346) 38 (2021), 1; 37-59

Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni

Ključne riječi
Earthquakes, 1838, 1839, Međimurje (Croatia), Slovene Hills (Slovenia)

Sažetak
Analyses of available data (newspaper reports, historical and church chronicles, chronical earthquake overviews, travel books, monographies, research papers, etc.) on effects of the earthquakes that shook the greater Ormož area at the Slovenian–Croatian border in the 1838 and 1839 revealed that one of them, recorded in a number of regional and global catalogues, is in fact a fake – the earthquake of 26 August 1838 never happened. This error creeped into various reports and studies, and then into many relevant catalogues, so this event should by systematically erased from the catalogues used to estimate seismicity rates in the neighbourhoods of north-western Croatia, north-eastern Slovenia, and south-western Hungary. Regarding the earthquake of 31 July 1838, we used important new sources of information that have not been consulted in any previous study. This made inversion of macroseismic parameters more robust. Our estimates of the macroseismic local and moment magnitudes (MLm = 4.8 ; Mwm = 4.8) are mostly higher than the values reported in the available catalogues. Reliable information on the effects of the smaller event of 22 March 1839 were found for two localities only, so its epicentre was placed into the town of Ormož where the maximum intensity was observed. Its estimated magnitudes (MLm = 4.4, Mwm = 4.4) are close to the median of values found in the six consulted catalogues that listed this event. The macroseismic epicentre of the 1838 earthquake lies close to the junction of surface traces of the Donat strike-slip fault and the reverse Čakovec fault. Based on their assumed geometry and the location of the macroseismic hypocentre, we give slight preference to the Donat fault as the seismogenic source.

Izvorni jezik
Engleski

Znanstvena područja
Geofizika

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