Abstract

Focusing on the Eastern Adriatic region, from Zadar in the north to Corfu in the south, the background information supporting our knowledge of the seismicity in the time-span 14th to early 19th century is discussed from the point of view of the historical earthquake records. The late 19th century seismological compilations turn out to be those responsible for the uneven spatial and temporal distribution of seismicity suggested by current parametric earthquake catalogues. This awareness asked for a comprehensive reappraisal of the reliability and completeness of the available historical earthquake records. This task was addressed by retrieving in the original version the information already known, by putting the records in the historical context in which they were produced, and finally by sampling historical sources so far not considered. Selected case histories have been presented in some detail also. This material altogether has shown that i) current parameterisation of past earthquakes in the Eastern Adriatic should be reconsidered in the light of a critically revised interpretation of the available records; ii) collecting new evidence in sources and repositories, not fully exploited so far, is needed. This should aim mostly at overcoming another limitation affecting the evaluation of full sets of earthquake parameters, that is the few observations available for each earthquake. In this perspective, an optimistic assessment of the potential documentation on this area is proposed.

Highlights

  • Despite the efforts of many researchers dating back to the UNESCO project in early seventies (Shebalin, 1974; Shebalin et al, 1974), the seismicity of the Balkan area is still poorly known

  • For historical Dalmatia, that is for territories today in contribution focuses on Eastern Adriatic from Zadar (Croatia), Bosnia and Herzegovina, Serbia and Montenegro, the catalogues included in Shebalin et al (1974) do not explicitly mention their sources of information. That they were partly derived from the seismological compilation by Kispatic (18911892) had to be inferred by an accurate reading of the text

  • The material presented in this paper aims at contributing to a review of the existing knowledge of the seismicity of the Eastern Adriatic from the point of view of historical records, and those made available from seismological compilations and from the result of recent investigations

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Summary

Introduction

Despite the efforts of many researchers dating back to the UNESCO project in early seventies (Shebalin, 1974; Shebalin et al, 1974), the seismicity of the Balkan area is still poorly known. This contribution focuses on Eastern Adriatic from Zadar (Croatia) in the north to Corfu (Greece) in the south; it deals mainly with the seismicity of the islands and coastal area of Croa-. Selected case histories will allow the author to highlight some sub-regional conditions which have determined both production and transmission of historical earthquake records and which still affect the knowledge of the seismicity of the Eastern Adriatic region.

Seismicity of the Eastern Adriatic according to current parametric catalogues
Previous catalogues and seismological compilations
Behind the seismological compilations
Geopolitical features
Observation points and documents
Up to early 16th century
25 June 1407
March 1544 14 hours
Feb 1547
South of Dubrovnik
Albania
Discussion and conclusions
Full Text
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