...Annie E. Jerkins; Hasbi Ash Shiddiqi; Tormod Kværna; Steven J. Gibbons; Johannes Schweitzer; Lars Ottemöller; Hilmar Bungum ABSTRACT The M w 4.5 southern Viking graben earthquake on 30 June 2017 was one of the largest seismic events in the Norwegian part of the North Sea during the last century...

... earthquakes of the Mediterranean, serving as TSP for the ICG/NEAMTWS. We focus on the lessons learned from past events occurring in the Mediterranean Sea, including the Kos‐Bodrum in 2017 ( M w  6.6) and the Samos‐Izmir in 2020 ( M w  7.0) earthquakes, which generated moderately damaging...

...Roey Shimony; Zohar Gvirtzman; Michael Tsesarsky ABSTRACT The Dead Sea Transform (DST) dominates the seismicity of Israel and neighboring countries. Whereas the instrumental catalog of Israel (1986–2017) contains mainly M < 5 events, the preinstrumental catalog lists 14 M 7 or stronger events...

...Minhee Choi; David W. Eaton; Eva Enkelmann Abstract The Denali fault, a transcurrent fault system that extends from northwestern Canada across Alaska toward the Bering Sea, is partitioned into segments that exhibit variable levels of historical seismicity. A pair of earthquakes (M 6.2 and 6.3) on 1...

..., respectively, and the M  6.4 event in 2016 located offshore in the southern Alboran sea ( Buforn et al. , 2017 ; Gràcia et al. , 2019 ; Stich et al. , 2020 ) to the northwest of Melilla. These events are the largest earthquakes recorded in the instrumental period in this area. Furthermore, from mid‐2021...

... dashed line represents the Sahel blind fault ( Meghraoui, 1991 ; Maouche et al., 2011 ). To the north of the Mitidja Basin, the 70 km long Sahel fold extends to the west of Algiers, bounded to the south by a typical blind reverse fault that has probably generated several earthquakes ( Maouche et...

.... , 2013 ), it is crucial to estimate source parameters of small‐to‐moderate events in regions with high seismic hazard to better assess the risk potential of pending large earthquakes. Along the western portion of the North Anatolian fault zone (NAFZ), the Sea of Marmara region is adjacent to the Istanbul...

... . Maximum earthquake magnitudes along different sections of the North Anatolian fault zone , Tectonophysics 674 , 147 – 165 . Bohnhoff M. Wollin C. Domigall D. Küperkoch L. Martínez‐Garzón P. Kwiatek G. Dresen G. , and Malin P. E. 2017 . Repeating Marmara Sea...

...., Goldfinger et al. , 2012 ; Hill et al. , 2022 ). Studies of past CSZ earthquakes have used the geographic distribution of paleoseismic evidence and their age correlations to develop “maximum rupture” models ( Goldfinger et al. , 2012 , 2017 ; Hutchinson and Clague, 2017 ; Nelson et al. , 2021...

... of the Pyramid’s surroundings section) south of the epicenter. This location is also confirmed by the macroseismic data inversion solution by Pettenati et al. (2017) . North of PYR, in the Tibetan region (western Xizang), the seismicity is deeper and the events generally reach a depth of more than 60 km...

...., United Nations Office for Disaster Risk Reduction, 2017). These forecasts provide site- specific hazard estimates that guide decision- making processes. Sea- level change forecasts, based on the combined effects of climate- induced sea- level rise and continuous tectonic vertical land motions (VLMs...

... in the north–west direction as also proposed by Watkinson and Hall (2017) . The focal mechanisms of Tobelo earthquakes were calculated for the foreshock, mainshock, and four largest aftershocks. The top left corner is the inset of the Tobelo fault and the focal mechanisms. (b) Geological map in north Molluca...

... et al. , 2006 ; Barth et al. , 2012 ; Boulton et al. , 2017 ). These observations provide a multiscale context for understanding the conditions under which earthquakes nucleate and propagate. Second, an unusually extensive paleoseismic database provides firm constraints on the chronology of past...

... and published in The Geographical Journal in 1898, which is quoted in full below ( Little, 1898 ): New Island near Kudat, British North Borneo.—A short note by Mr. R. M. Little, describing a visit to a small island which rose from the sea during the earthquake of last year, appears in The British North...

... by sand in the south and mud in the north of the Main Channel. The FRD’s susceptibility to hazards necessitates protective measures, with approximately 250 km of dykes shielding the delta plain from river floods and storm surges. Subsidence amplifies the impact of rising sea levels. Earthquakes...

... fault system (PFS; see Fig.  1 ), in the northeast sector, and the Ragalna fault (RF; Fig.  1 ) in the southwestern one, with seismicity primarily concentrated within 6 km below sea level. The most important deformation occurred on the lower southeastern flank due to an M w  4.9 earthquake along...

... Gold Open Access: This paper is published under the terms of the CC-BY-NC license. Holocene coastal geomorphology is often used in paleo-sea level and paleoseismic research to understand the magnitude and frequency of past earthquakes and the rates and impacts of sea-level variations in coastal...

... are channeled efficiently through the low‐attenuation North Australian craton (NAC), with moderate‐sized ( M w ≥ 5.0 ) earthquakes in the Banda Sea commonly felt in northern Australia. A far‐field ground‐motion model (GMM) has been developed for use in seismic hazard studies for sites located within the NAC...

... as to the area of slow slip triggered by the Kaikōura earthquake (Fig.  1 ) ( Wallace et al. , 2017 ). The long‐duration motions observed onshore and offshore were distributed within epicentral distances between 580 and 730 km along the east coast of the North Island, where an extremely low‐velocity...