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![(a) Rijeka at the time of the earthquake of 1750. A reproduction from Gigante (1913) of part of Metzinger’s painting from the cathedral in Rijeka at the altar of St. Philip Neri, the patron saint against earthquakes. (b) A plaque (from 1801) on the City Tower of Rijeka commemorating its restoration in 1753 after damage caused by the earthquake (photo: D. Herak, 2016).The color version of this figure is available only in the electronic edition.]()
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![(a) Summary of seismic intensities for the 1750 Croatia earthquake by Herak et al. (2017). Intensities range up to VIII (Medvedev–Sponheuer–Karnik scale) according to the percentage of black filling in circles. Gray (red in the online version) and white stars indicate the new and older estimates of the epicenter. The simplified trace of the Bakar–Vinodol fault (in gray, in red in the online version, ticks on upthrown side) is after Benac et al. (2008). Rectangular box indicates the horizontal projection of the finite‐fault model derived from inversion of the amount of tectonic subsidence in marine notches in the wider Rijeka area; a continuous line indicates predicted surface faulting. Seismic uplift is expected to the northwest, seismic subsidence to the southeast of the fault (see panel b and Stiros and Moschas, 2012). (b) Projection of the depth of marine notches, formed at mean sea level during the post‐Roman period (last 2000 yrs) along an axis normal to the mean trend of the Bakar–Vinodol thrust (see panel a). Two different groups of notch depth are evident, notches with a uniform depth of 55 cm at the wider part of the Rijeka Gulf, indicative of effects associated with a global sea‐level rise, and notch depths increasing to 115 cm in the vicinity of the Bakar area, conspicuously because of tectonic activity. Observed and model‐predicted tectonic subsidence and notch depth is also shown. Based on Stiros and Moschas (2012).The color version of this figure is available only in the electronic edition.]()
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Rijeka earthquake 1750
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(a) Rijeka at the time of the earthquake of 1750. A reproduction from Giga... Available to Purchase
in Historical Seismicity of the Rijeka Region (Northwest External Dinarides, Croatia)—Part I: Earthquakes of 1750, 1838, and 1904 in the Bakar Epicentral Area
> Seismological Research Letters
Published: 12 April 2017
Figure 2. (a) Rijeka at the time of the earthquake of 1750. A reproduction from Gigante (1913) of part of Metzinger’s painting from the cathedral in Rijeka at the altar of St. Philip Neri, the patron saint against earthquakes. (b) A plaque (from 1801) on the City Tower of Rijeka commemorating
Journal Article
Historical Seismicity of the Rijeka Region (Northwest External Dinarides, Croatia)—Part I: Earthquakes of 1750, 1838, and 1904 in the Bakar Epicentral Area Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 12 April 2017
Seismological Research Letters (2017) 88 (3): 904–915.
...Figure 2. (a) Rijeka at the time of the earthquake of 1750. A reproduction from Gigante (1913) of part of Metzinger’s painting from the cathedral in Rijeka at the altar of St. Philip Neri, the patron saint against earthquakes. (b) A plaque (from 1801) on the City Tower of Rijeka commemorating...
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Includes: Supplemental Content
Journal Article
Comment on “Historical Seismicity of the Rijeka Region (Northwest External Dinarides, Croatia)—Part I: Earthquakes of 1750, 1838, and 1904 in the Bakar Epicentral Area” by Davorka Herak, Ivica Sović, Ina Cecić, Mladen Živčić, Iva Dasović, and Marijan Herak Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 20 September 2017
Seismological Research Letters (2017) 88 (6): 1534–1536.
...Stathis C. Stiros Sites of high seismic intensities (VI–VIII) during the 1750 Rijeka, Croatia, earthquake correlate first with the Bakar–Vinodol thrust (or fault zone), one of the main features accommodating convergence in northern Adria; and second, with a fault derived from inversion/elastic...
FIGURES
Journal Article
Reply to “Comment on ‘Historical Seismicity of the Rijeka Region (Northwest External Dinarides, Croatia)—Part I: Earthquakes of 1750, 1838, and 1904 in the Bakar Epicentral Area’ by Davorka Herak, Ivica Sović, Ina Cecić, Mladen Živčić, Iva Dasović, and Marijan Herak” by Stathis C. Stiros Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 20 September 2017
Seismological Research Letters (2017) 88 (6): 1537–1538.
..., will be found in future investigations. REFERENCES Herak D. Sović I. Cecić I. Živčić M. Dasović I. , and Herak M. 2017 . Historical seismicity of the Rijeka region (northwest external Dinarides, Croatia)—Part I: Earthquakes of 1750, 1838, and 1904 in the Bakar epicentral...
Image
(a) Summary of seismic intensities for the 1750 Croatia earthquake by Hera... Available to Purchase
in Comment on “Historical Seismicity of the Rijeka Region (Northwest External Dinarides, Croatia)—Part I: Earthquakes of 1750, 1838, and 1904 in the Bakar Epicentral Area” by Davorka Herak, Ivica Sović, Ina Cecić, Mladen Živčić, Iva Dasović, and Marijan Herak
> Seismological Research Letters
Published: 20 September 2017
Figure 1. (a) Summary of seismic intensities for the 1750 Croatia earthquake by Herak et al. (2017) . Intensities range up to VIII (Medvedev–Sponheuer–Karnik scale) according to the percentage of black filling in circles. Gray (red in the online version) and white stars indicate the new
Journal Article
Three-dimensional Stability Assessment of a Complex Landslide in the Rječina Valley, Croatia Available to Purchase
Published: 01 February 2017
Environmental & Engineering Geoscience (2017) 23 (1): 13–21.
...., 2012 ; Mihalić and Arbanas, 2013 ). These historical documents indicate that the Grohovo landslide was caused by an earthquake in 1750, with its epicenter in Rijeka. A recent large displacement was observed on December 5, 1996 ( Benac et al., 2005 ). After the initial landslide displacement...
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Journal Article
Historical Seismicity of the Rijeka Region (Northwest External Dinarides, Croatia)—Part II: The Klana Earthquakes of 1870 Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 30 May 2018
Seismological Research Letters (2018) 89 (4): 1524–1536.
... area (S. Slovenia) , J. Earthq. Eng. 13 , 50 – 67 . Herak D. Sović I. Cecić I. Živčić M. Dasović I. , and Herak M. 2017 . Historical seismicity of the Rijeka region (northwest External Dinarides, Croatia)—Part I: Earthquakes of 1750, 1838, and 1904 in the Bakar...
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Includes: Supplemental Content
Journal Article
The Međimurje (Croatia) Earthquake of 1738 Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 29 January 2020
Seismological Research Letters (2020) 91 (2A): 1042–1056.
.../2019TC005524 . Herak D. Sović I. Cecić I. Živčić M. Dasović I. , and Herak M. 2017 . Historical seismicity of the Rijeka region (northwest External Dinarides, Croatia)—Part I: Earthquakes of 1750, 1838, and 1904 in the Bakar epicentral area , Seismol. Res. Lett. 88 , no. 3...
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Journal Article
Geometry of the Subducting Indian Plate and Local Seismicity in the Andaman Region from the Passive OBS Experiment Available to Purchase
Publisher: Seismological Society of America
Published: 29 January 2019
Bulletin of the Seismological Society of America (2019) 109 (2): 797–811.
... earthquakes are identified from the OBS network. The data are integrated with the available earthquake data from the Andaman ISLANDS (Investigation of Seismicity and Lithospheric Structure beneath the Andaman–Nicobar Subduction Zone) network and some global seismic stations. The minimum 1D velocity model...
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