Testing the Environmental Seismic Intensity Scale on Data Derived from the Earthquakes of 1626, 1759, 1819, and 1904 in Fennoscandia, Northern Europe

Earthquake environmental effects (EEEs) were compiled for the earthquakes of 1626, 1759, 1819, and 1904 in the Fennoscandian Peninsula, northern Europe. The principal source of information was the contemporary newspaper press. Macroseismic questionnaires collected in 1759 and 1904 were also consulte...

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Main Authors: Päivi Mäntyniemi, Mathilde B. Sørensen, Ruben E. Tatevossian
Format: Article
Language:English
Published: MDPI AG 2021-12-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/11/1/14
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spelling doaj-68535f920798499d8c02dfc29ef91bf92020-12-30T00:04:30ZengMDPI AGGeosciences2076-32632021-12-0111141410.3390/geosciences11010014Testing the Environmental Seismic Intensity Scale on Data Derived from the Earthquakes of 1626, 1759, 1819, and 1904 in Fennoscandia, Northern EuropePäivi Mäntyniemi0Mathilde B. Sørensen1Ruben E. Tatevossian2Institute of Seismology, University of Helsinki, 00014 Helsinki, FinlandDepartment of Earth Science, University of Bergen, 5020 Bergen, NorwayInstitute of Physics of the Earth, Russian Academy of Sciences, 123242 Moscow, RussiaEarthquake environmental effects (EEEs) were compiled for the earthquakes of 1626, 1759, 1819, and 1904 in the Fennoscandian Peninsula, northern Europe. The principal source of information was the contemporary newspaper press. Macroseismic questionnaires collected in 1759 and 1904 were also consulted. We prepared maps showing newly discovered EEEs together with previously known EEEs and analyzed their spatial distribution. We assigned intensities based on the 2007 Environmental Seismic Intensity (ESI) scale to 27 selected localities and compared them to intensities assigned based on the 1998 European Macroseismic Scale. While the overall agreement between the scales is good, intensities may remain uncertain due to the sparsity of written documentation. The collected data sets are most probably incomplete but still show that EEEs are not unprecedented cases in the target region. The findings include landslides and rockfalls as well as cascade effects with a risk potential and widespread water movements up to long distances. The winter earthquake of 1759 cracked ice over a large area. This investigation demonstrates that the ESI scale also has practical importance for regions with infrequent EEEs.https://www.mdpi.com/2076-3263/11/1/14historical seismologyearthquake environmental effectenvironmental seismic intensity scalemacroseismic intensitynewspaperKattegat earthquake of 1759
collection DOAJ
language English
format Article
sources DOAJ
author Päivi Mäntyniemi
Mathilde B. Sørensen
Ruben E. Tatevossian
spellingShingle Päivi Mäntyniemi
Mathilde B. Sørensen
Ruben E. Tatevossian
Testing the Environmental Seismic Intensity Scale on Data Derived from the Earthquakes of 1626, 1759, 1819, and 1904 in Fennoscandia, Northern Europe
Geosciences
historical seismology
earthquake environmental effect
environmental seismic intensity scale
macroseismic intensity
newspaper
Kattegat earthquake of 1759
author_facet Päivi Mäntyniemi
Mathilde B. Sørensen
Ruben E. Tatevossian
author_sort Päivi Mäntyniemi
title Testing the Environmental Seismic Intensity Scale on Data Derived from the Earthquakes of 1626, 1759, 1819, and 1904 in Fennoscandia, Northern Europe
title_short Testing the Environmental Seismic Intensity Scale on Data Derived from the Earthquakes of 1626, 1759, 1819, and 1904 in Fennoscandia, Northern Europe
title_full Testing the Environmental Seismic Intensity Scale on Data Derived from the Earthquakes of 1626, 1759, 1819, and 1904 in Fennoscandia, Northern Europe
title_fullStr Testing the Environmental Seismic Intensity Scale on Data Derived from the Earthquakes of 1626, 1759, 1819, and 1904 in Fennoscandia, Northern Europe
title_full_unstemmed Testing the Environmental Seismic Intensity Scale on Data Derived from the Earthquakes of 1626, 1759, 1819, and 1904 in Fennoscandia, Northern Europe
title_sort testing the environmental seismic intensity scale on data derived from the earthquakes of 1626, 1759, 1819, and 1904 in fennoscandia, northern europe
publisher MDPI AG
series Geosciences
issn 2076-3263
publishDate 2021-12-01
description Earthquake environmental effects (EEEs) were compiled for the earthquakes of 1626, 1759, 1819, and 1904 in the Fennoscandian Peninsula, northern Europe. The principal source of information was the contemporary newspaper press. Macroseismic questionnaires collected in 1759 and 1904 were also consulted. We prepared maps showing newly discovered EEEs together with previously known EEEs and analyzed their spatial distribution. We assigned intensities based on the 2007 Environmental Seismic Intensity (ESI) scale to 27 selected localities and compared them to intensities assigned based on the 1998 European Macroseismic Scale. While the overall agreement between the scales is good, intensities may remain uncertain due to the sparsity of written documentation. The collected data sets are most probably incomplete but still show that EEEs are not unprecedented cases in the target region. The findings include landslides and rockfalls as well as cascade effects with a risk potential and widespread water movements up to long distances. The winter earthquake of 1759 cracked ice over a large area. This investigation demonstrates that the ESI scale also has practical importance for regions with infrequent EEEs.
topic historical seismology
earthquake environmental effect
environmental seismic intensity scale
macroseismic intensity
newspaper
Kattegat earthquake of 1759
url https://www.mdpi.com/2076-3263/11/1/14
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