Abstract

The most recent major earthquake series struck near Petrinja (December 29th 2020 M 6.2), and triggered extensive ground failures in the wider area of Petrinja, Sisak and Glina. Coseismic ground failures including subsidence dolines, liquefaction and landslides have been documented over a large area by various experts and teams. These data are stored in the newly created inventory, which is openly presented in this paper. This inventory is administered and updated by the Croatian Geological Survey, and will be available online via a Web Map Service (WMS) (www.hgi-cgs.hr). The aim of the inventory is to not only provide data for the development of susceptibility maps and more detailed exploration for possible remediation measures, but also to define the priorities for immediate action. The earthquake triggered the rapid development of dropout dolines which endanger the local populations of the villages of Mečenčani and Borojevići. This is still an ongoing process in the vicinity of the houses and therefore in-situ exploration started immediately. Liquefaction related to alluvial sediments of the Sava, Kupa and Glina rivers occurred almost exclusively in loose and pure sands, and was accompanied by sand boils, subsidence and lateral spreading. Liquefaction also presents a greater hazard because settlement of houses and river embankments occurred. Lateral spreading caused failures of river flood embankments and natural river banks. According to the data known to date, the majority of the coseismic landslides were reactivated with minor displacements. Despite that, it has been recognised that houses at the edge, or in landslide colluvium suffered greater damage than other houses located outside the landslide impact zone.

Highlights

  • Ground shaking during an earthquake usually causes major dama­ge to structures

  • “The term ground failure is a general reference to landslides, liquefaction, lateral spreads, and any other consequence of shaking that affects the stability of the ground” (USGS Earthquake Glossary, 2021)

  • Most of such databases in the literature are related to landslides (KEEFER, 1984; RODRÍGUEZ et al, 1999, BOMMER & RODRÍGUEZ, 2002; GORUM et al, 2011) or liquefaction (YOUD & HOOSE, 1978), but there are more recent examples of inventories comprising all the typical forms of ground failure caused by earthquakes (PRESTININZI & ­ROMEO, 2000)

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Summary

INTRODUCTION

Ground shaking during an earthquake usually causes major dama­ge to structures. earthquakes induce ground failures that can significantly contribute to total earthquake loss. The absence of ground failure data may lead to unrealistic projections of losses caused by a particular earthquake Evidence of such processes/phenomena represent an important input into the production of reliable susceptibility maps and microzoning, which are important in the proper evaluation of seismic hazard in a particular region. The database would enable more realistic estimations of the total earthquake damage and loss For this reason, the complete table of inputs collected so far is presented here in order to transparently provide information that can be further used to develop susceptibility maps, identify the most critical surface damage zones and ensure data for seismic microzoning and hazard assessment. The up to date database is presented online via Web Map Service (WMS), and will be continuously maintained and updated by the HGI (www.hgi-cgs.hr)

Geology
Tectogenesis of the research area
Seismicity
THE PRELIMINARY INVENTORY
Subsidence dolines
Liquefaction
Landslides
Other ground effects
DISCUSSION AND CONCLUSIONS
Subsidence dolines area
Liquefied areas
Full Text
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