1912 mürefte earthquake

of Geological Engineering, Muğla Sıtkı Koçman University, Muğla, 48000, Turkey, You can also search for this author in Rupture characteristics of the AD 1912 Mürefte (Ganos) earthquake segment of the North Anatolian fault (western Turkey) ME Aksoy, M Meghraoui, M Vallée, Z Çakır. It had an estimated magnitude of 7.8 and a maximum intensity of X on the Mercalli intensity scale, causing 216 casualties. Part of Springer Nature. This article about an earthquake in Asia is a stub. Learn more about Institutional subscriptions, Agamennone G (1912) Il disastroso terremoto nel bacino occidentale del Mar di Marmara Rivista di Astronomiae Scienze affini Anno VI- Ottobre:3–8. Considering the location, magnitude, and damage of the 13 September 1912 aftershock, the seismic sequence of Mw > 5.7 earthquakes from 1975 to 2014, the major discontinuities of the NAF in the Bay of Saros and Sea of Marmara I suggest the 1912 earthquake sequence ruptured at least ~ 160 km-long section of the NAF from the Inner Saros basin to the Marmara Central Basin and left a 100-km-long seismic gap in the Sea of Marmara. https://doi.org/10.1016/j.tecto.2016.02.028, Bouchon M et al (2010) Faulting characteristics of supershear earthquakes. century causing damage with maximum intensity IX-X MSK between the Sea of Marmara and the Bay of Saros. Aksoy, M.E. Mediterranean Geoscience Reviews https://doi.org/10.1038/nature05275. Acad. The 9 August 1912 Mürefte Earthquake M 7.4 is one of the largest destructive earthquakes of the 20th century, in the Balkan region. Tectonics 30:1–14. https://doi.org/10.1029/2011TC002906, Gürbüz C et al (2000) The seismotectonics of the Marmara region (Turkey): results from a microseismic experiment. Abstract This paper examines one of the largest earthquakes in the Balkans in this century which remains hitherto imperfectly known and in need of evaluation. The fieldwork was funded by the EC project RELIEF (EC Contract EVG1-2002–00069). https://doi.org/10.1130/G31447.1, Article The 9 August 1912 Mürefte earthquake (Ms=7.4) occurred at an early stage of seismological research. It had an estimated magnitude of 7.4 M w and a maximum intensity of X (Extreme) on the Modified Mercalli intensity scale, causing from 216–3000 casualties. We investigate the cumulative and co-seismic offsets of the Ganos fault, the westernmost segment of the right-lateral North Anatolian Fault System that ruptured during the 9 August 1912 Mürefte earthquake (Ms = 7.3). In this study, the original seismograms from various countries for 1912 Sarköy-Mürefte, 1935, Erdek Marmara Island and 1963, Cinarcik Earthquakes were digitized. The … The 1912 Mürefte earthquake occurred at 03:29 local time on 9 August. © 2021 Springer Nature Switzerland AG. The 9 August 1912 Mürefte earthquake (M s = 7.3 [Ambraseys, 2002]) occurred along the western section of the North Anatolian Fault (NAF) and displayed surface fault-ing along the 45-km-long inland section of the Ganos segment (Figures 1 and 2). https://doi.org/10.1023/A:1011435927983, Sadi M. Dr. Yüzbaşı (1912) Marmara Havzasının 26–27 Temmuz Hareket-i Arzı 15 Eylül 1328 Resimli Kitap Matbaası, İstanbul:45, Saltogianni V, Gianniou M, Taymaz T, Yolsal-Çevikbilen S, Stiros S (2015) Fault slip source models for the 2014 Mw 6.9 Samothraki-Gökçeada earthquake (North Aegean Trough) combining geodetic and seismological observations. https://doi.org/10.1002/eqe.4290150204, Anderson JG, Wesnousky SG, Stirling MW (1996) Earthquake size as a function of fault slip rate. See also . You can help Wikipedia by expanding it. earthquake that occurred in the region during the instrumental period was the 9 August 1912 Mürefte-Şarköy earthquake (Mw 7.4). Following 1999Izmit earthquake occurred at the EasternMarmara region, a complete inventory ofactive faults in … The outputs of the thesis rest on the precious discussions and recommendations of my supervisors Mustapha Meghraoui and Ziyadin Çakır. Solid Earth 120:8610–8622. https://doi.org/10.1111/j.1365-3121.2004.00552.x, Altunel E, Barka A, Akyüz S (2000) Slip distribution along the 1912 Mürefte-Şarköy earthquake, the North Anatolian Fault, Western Marmara. Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations. 3. Tectonophysics 493(244):253. https://doi.org/10.1016/j.tecto.2010.06.011, Emre Ö, Awata Y, Duman TY (eds) (2003) 17 Auğustos 1999 İzmit Depremi Yüzey Kırığı; Surface Rupture Associated with the 17 August 1999 İzmit Earthquake vol. Inaddition a seabed dislocation, the sourceof 1912 tsunami can also be assigned to thesediment slumps appearing in the form ofechelon landslide prisms along the southernslopes of the West Marmara Trough. Since then, new information and a better understanding of this event has been established. https://doi.org/10.1007/s00367-007-0099-6, Walker WG (1912) Turkish Earthquake of September 13. The tremor struck at 03:30 a.m. and was felt in a wide region including Greece and Bulgaria. "Rupture characteristics of the A.D. 1912 Mürefte (Ganos) earthquake segment of the North Anatolian fault (western Turkey)", "Seismicity of the Sea of Marmara (Turkey) since 1500", "Bogazici University Kandilli Observatory and Earthquake Research Institute National Earthquake Monitoring Center (NEMC) List of earthquakes 1900–2004 (Büyük Depremler)", "Comments for the Significant Earthquake", https://en.wikipedia.org/w/index.php?title=1912_Mürefte_earthquake&oldid=1018956907, Creative Commons Attribution-ShareAlike License, This page was last edited on 20 April 2021, at 19:36. 1 is accessible via the online databases of the Kandilli Observatory of Bosphorus University and the European-Mediterranean Seismological Centre. Bull Seismol Soc Am 86:683–690, Armijo R et al (2005) Submarine fault scarps in the Sea of Marmara pull-apart (North Anatolian Fault): Implications for seismic hazard in Istanbul. Earthquake Eng Struct Dynam 15:189–211. The 9 August 1912 Mürefte earthquake (M>7) is one of the largest seismic events in the Balkan region in the 20 th century. It had an estimated magnitude of 7.4 Mw and a maximum intensity of X (Extreme) on the Modified Mercalli intensity scale, causing from 216–3000 casualties. Bull Seismol Soc Am 98:1609–1632. The damages and loss of life caused by the earthquake Dept. R. Sukâyân Matbaası, Resimli Kitap Matbaası Istanbul, Milli Kütüphane, 1994 AFİŞ 831. https://dijital-kutuphane.mkutup.gov.tr/tr/nonbookmaterials/catalog/details/77161, McHugh CMG et al (2006) Submarine earthquake geology along the North Anatolia Fault in the Marmara Sea, Turkey: a model for transform basin sedimentation Earth Planet. The 1912 Mürefte earthquake occurred at 03:29 on 9 August. Med. Geophys J Int 213:1113–1120. T.C, Imar ve İskan Bakanlığı, Deprem Arastırma Enstitüsü Baskanlığı, Ankara, Barka A (1992) The North Anatolian fault zone. Istanbul Technical University-Eurasia Institute of Earth Sciences & University of Strasbourg-Institute de Physique to Globe Strasbourg, PhD dissertation, Aksoy ME, Meghraoui M, Vallee M, Cakir Z (2010) Rupture characteristics of the A.D. 1912 Murefte (Ganos) earthquake segment of the North Anatolian fault (western Turkey). (2021). NW Turkey Geo-Mar Lett 28:171–193. The slip distribution and the simple fault geometry support an offshore extension of the rupture towards both, the Sea of Marmara and the Bay of Saros. Turkey J Geophys Res 109:1–21. Geophys Res Lett 41:5783–5788. The 9 August 1912 Mürefte earthquake (Ms 7.3–7.4) occurred on the westernmost inland segment of the North Anatolian Fault (NAF) and is one of the most devastating events in the Specials thanks go to Gülsen Uçarkuş, Serdar Akyüz, Gürsel Sunal, and Murat Topkan for their help and fruitful discussion during the fieldworks. Tectonophysics 316:1–17, Gutenberg B, Richter CF (1949) Seismicity of the earth and associated phenomena, vol 1. https://doi.org/10.1016/j.epsl.2006.05.038, Meghraoui M, Aksoy ME, Akyüz HS, Ferry M, Dikbaş A, Altunel E (2012) Paleoseismology of the North Anatolian Fault at Güzelköy (Ganos segment, Turkey): size and recurrence time of earthquake ruptures west of the Sea of Marmara. Geochem Geophys Geosystems 6:Q06009. The seismicity data illustrated in Fig. This work is a part of the Ph.D. thesis of the author that was completed in the frame of a co-tutelle agreement between two institutions Istanbul Technical University-Eurasia Institute of Earth Sciences and University of Strasbourg-Institute de Physique to Globe Strasbourg and supported by the French Embassy in Ankara. Depending on your flexibility, these larger cities might be interesting for you: Mytilini, Athens, İzmir, Balıkesir, and Sofia.When in this area, you might want to check out Mytilini . Accessed 10 Nov 2020, Ustaömer T et al (2008) Faulting, mass-wasting and deposition in an active dextral shear zone, the Gulf of Saros and the NE Aegean Sea. Int. This earthquake affected the Mürefte and Şarköy settlements and was felt very strongly in Tekirdağ, Gelibolu and Çanakkale regions. This Turkish history-related article is a stub. C.R. Special Publication-1. Abstract: The Ganos fault is the westernmost segment of the North Anatolian Fault (NAF) that generated the 9 August 1912 Mürefte (Ganos) earthquake (Mw=7.4). The detailed fault mapping reveals a simple continuous fault geometry along the 45-km-long inland section, which has completely ruptured with right-lateral displacements reaching up to 5.5 m. The earthquake magnitude and source duration imply a 135 ± 25 km rupture length. Hauptstation für Erdbebenforschung, Jena, früher in Strassburg, IASPEI (2004) International Association of Seismology and Physics of the Earth's Interior, Working Group on Seismological Archives Report, Karabulut H, Roumelioti Z, Benetatos C, Ahu Kömec M, Özalaybey S, Aktar M, Kiratzi A (2006) A source study of the 6 July 2003 (Mw 5.7) earthquake sequence in the Gulf of Saros (Northern Aegean Sea): Seismological evidence for the western continuation of the Ganos fault. M. E. Aksoy. See also. Geology 38 (11), 991-994, 2010. 52: 2010: ITU Publications, Istanbul, pp 341–349, Ambraseys NN (2002) The seismic activity of the Marmara Sea Region over the last 2000 years. The corresponding author states that there is no conflict of interest. https://doi.org/10.1016/j.tecto.2009.05.027, Rockwell TK et al (2009) Palaeoseismology of the North Anatolian Fault near the Marmara Sea: implications for fault segmentation and seismic hazard. The historical data reviewedfrom library and archive documents,geological field surveys and offshoregeophysical investigations have shown thatthe 1912 earthquake produced a tsunami. https://doi.org/10.1029/2003JB002667, Reilinger R, McClusky S, Paradissis D, Ergintav S, Vernant P (2010) Geodetic constraints on the tectonic evolution of the Aegean region and strain accumulation along the Hellenic subduction zone. 73 seismic records have been collected for the 9 August, 10 August and 13 September 1912 shocks, which occurred along the … 3 the momentum effect of the earth-quake forces on a structure can be seen. The same is also valid for 04.01.1935, 14:41, M=6.4 and 16:20 M=6.3 Erdek-Marmara Island, and 18.09.1963, 1963, M=6.3 Çınarcık Earthquakes. Tectonophysics 488:22–30. List of earthquakes in 1912; List of earthquakes in Turkey; References de Seismologie, Belgrad, Müller MD, Geiger A, Kahle HG, Veis G, Billiris H, Paradissis D, Felekis S (2013) Velocity and deformation fields in the North Aegean domain, Greece, and implications for fault kinematics, derived from GPS data 1993–2009. Publicatiunile Adamachi V 33:260–273, Mâmâcânyam E (1912) Mürefte civarı büyük zelzele ve yangını garib destanı, . Rev. Nature 89:607. https://doi.org/10.1038/089607c0, Stein R, Jacobson D, Sevilgen V (2016) Kentucky Magnitude-3.5 quake highlights the liquefaction potential in the disputed New Madrid seismic zone - Quake Insights, https://temblor.net/earthquake-insights/kentucky-magnitude-3-5-quake-highlights-the-liquefaction-potential-in-the-disputed-new-madrid-seismic-zone-574. Lower magnitude events are included if they have caused death, injury or damage. Scien, France, Bohnhoff M, Martínez-Garzón P, Bulut F, Stierle E, Ben-Zion Y (2016) Maximum earthquake magnitudes along different sections of the North Anatolian fault zone. It had an estimated magnitude of 7.4 Mw and a maximum intensity of X (Extreme) on the Modified Mercalli intensity scale, causing from 216–3000 casualties.[3][4]. https://archive.org/details/RASA191210/page/n61/mode/2up Accessed Sept 1 2020, Aksoy ME (2009) Active Tectonics and Paleoseismology of the Ganos Fault Segment and Seismıc Characteristics of the 9 August 1912 Mürefte Earthquake of the North Anatolian Fault (Western Turkey). https://doi.org/10.1007/s42990-021-00050-z, DOI: https://doi.org/10.1007/s42990-021-00050-z, Over 10 million scientific documents at your fingertips, Not logged in J Seismol 5:433–448. This is a preview of subscription content, access via your institution. The local timezone is named " Europe/Istanbul " with a UTC offset of 2 hours. see 1883 Çeşme earthquake: 10 July 1894 12:24 Gulf of Izmit: 40.73 29.25 1,300 7.0 see 1894 Istanbul earthquake: 29 April 1903 01:46 local time Malazgirt: 39.14 42.65 600 6.7 M s: see 1903 Manzikert earthquake: 9 August 1912 03:29 local time Mürefte: 40.75 27.2 216 7.3 M S: see 1912 Mürefte earthquake: 4 October 1914 00:07 local time Burdur Figure 3 : Circular behaviour of timber struc- Terra Nova 16:198–204. Geological Society London, Special Publications 316:31–54. We study the 1912 earthquake characteristics using co-seismic fault slip and fault segmentation coupled with an analysis of historical seismic records. The 9 August 1912 Mürefte-Şarköy earthquake of the North Anatolian fault. century causing damage with maximum intensity IX-X MSK between the Sea of Marmara and the Bay of Saros. Srpske Kraljevske Akademije, Belgrad, Mihailovic J (1927) Trusne katastrofe na Mramornome moru sa narocitim pogledom na opstu seizmicnost Mramornoga mora i njegovih obala vol 65. https://doi.org/10.1029/2004GC000896, Ateş R, Tabban A (1976) 9 Agustos 1912 Şarköy-Mürefte Depremi Çalısmaları Ön Raporu. The entire wiki with photo and video galleries for each article https://doi.org/10.1002/2014GL060985, Gasperini L, Polonia A, Çağatay MN, Bortoluzzi G, Ferrante V (2011) Geological slip rates along the North Anatolian Fault in the Marmara region. All dates are listed according to UTC time. https://doi.org/10.1093/gji/ggy049, Le Pichon X, Chamot-Rooke C, Rangin N, Şengör AMC (2003) The North Anatolian fault in the Sea of Marmara. Photos and illustrations of surface ruptures, landslides, liquefaction and lateral spreading depict the level, and distribution of primary- and secondary effects. Geosc. Geochem Geophys Geosyst 13:Q04005–Q04005. You can help Wikipedia by expanding it. Annales Tectonicae 6:164–195, Barka A (1999) The 17 August 1999 Izmit Earthquake. The earthquake size requires a minimum 120 km fault rupture length. Tectonophysics 674:147–165. ); Less than 15 km away. This is a list of earthquakes in 1912. Princeton University Press, Princeton, Gutzwiller O (1921) Beitraege zur Geologie der Umgebung von Merfete am Marmara-Meere. This study combines available data (historical & modern) with new field analysis on the 1912 earthquake rupture. The 9 August 1912 Mürefte earthquake (M s 7.3–7.4) occurred on the westernmost inland segment of the North Anatolian Fault (NAF) and is one of the most devastating events in the Balkan region during the early XX. PubMed Google Scholar. arköy-Mürefte 1912 Earthquake's Tsunami, extension of the associated faulting in the Marmara Sea, Turkey By Bedri Alpar Tsunami of the 1912 Earthquake (Ms=7.4), extension of the associated faulting in … More reading: Wikipedia ArticleLocated at 40.50 27.20 (Lat./Long. Scien, Paris, Paris, Mihailovic J (1923) Mehanizam Trusvih pokreta ha Mramornom Moru, vol 103. Sci Lett 248:661–684. The 1912 Mürefte earthquake occurred at 03:29 on 9 August.. I owe special gratitude to the librarians at IPGS and the Turkish National Library who eased my access to several historical documents used in this analysis. Bull Seismol Soc Am 92:1–18. Nature 90:163. https://doi.org/10.1038/090163d0, Wesnousky SG (2008) Displacement and Geometrical Characteristics of Earthquake Surface Ruptures: Issues and Implications for Seismic-Hazard Analysis and the Process of Earthquake Rupture. Events which occurred in remote areas will be excluded from the list as they wouldn't have generated significant media interest. This work is a part of the Ph.D. thesis of the author that was completed in the frame of a co-tutelle agreement between two institutions Istanbul Technical University and Institute de Physique to Globe Strasbourg and supported by the French Embassy in Ankara. Bülteni 56:91–127, Parsons T (2004) Recalculated probability of M > 7 earthquakes beneath the Sea of Marmara. https://doi.org/10.1029/2011GC003960, Mihailovic J (1918) Resultats des études sur le tremblement de terre d’aout et de septembre 1912 sur la mer de Marmara, vol 166. J Geophys Res 108:2179. https://doi.org/10.1029/2002JB001862, Macovei G (1912) Sur La Tremblement De Terre De La Mer De Marmara Le 9 Aout 1912. Talk:1912 Mürefte earthquake Jump to ... WikiProject Earthquakes (Rated Stub-class, Mid-importance) This article is part of WikiProject Earthquakes, a project to systematically present information on earthquakes, seismology, plate tectonics, and related subjects. 4 (Cogito, 1999). The 1912 Earthquake: The 9 August 1912 Mürefte earthquake (M>7) is one of the largest seismic events in the Balkan region in the 20 th century. The fieldwork was funded by the EC project RELIEF (EC Contract EVG1-2002-00069). https://doi.org/10.1023/A:1024581022222, Altunel E, Meghraoui M, Akyüz HS, Dikbaş A (2004) Characteristics of the 1912 co-seismic rupture along the North Anatolian fault zone (Turkey): implications for the expected Marmara earthquake. The Ganos fault is the westernmost segment of the North Anatolian fault that generated the 9 August 1912 Mürefte (Ganos) earthquake in western Turkey (M w = 7.4). Geol Soc Am Bull 86:1041–1057, Altınok Y, Alpar B, Yaltırak C (2003) Şarköy - Mürefte 1912 Earthquake’s Tsunami, extension of the associated faulting in the Marmara Sea. The 1912 Mürefte earthquake occurred at 03:29 on 9 August. https://doi.org/10.1016/j.tecto.2005.09.009, Konca AÖ et al (2018) The 2014, MW6.9 North Aegean earthquake: seismic and geodetic evidence for coseismic slip on persistent asperities. Tectonophysics 597–598:34–49. Belgrade, Mihailovic J (1933) La séismicite de la Thrace, de mer de Marmara et de l’Asie Mineur Monographies et Travaux Scientific Series B. Assoc. It had an estimated magnitude of 7.8 and a maximum intensity of X on the Mercalli intensity scale, causing 216 casualties. Geology 38:991–994. Google Scholar, Allen CG (1913) Review: Il disastroso terremoto Nel bacino occidental del mar di Marmara: by G. Agamennone Bull Seismol Soc Am 3:93–94, Allen CR (1975) Geological Criteria for Evaluating Seismicity: Address as Retiring President of The Geological Society of America, Miami Beach, Florida, November 1974. It caused significant damage in a wide area in NW Turkey and partly in … Science 285:1858–1859. In Fig. This study attempts to reveal the fault zone characteristics of the locked Ganos Fault based on electrical resistivity studies including audio-frequency (AMT: 10,400–1 Hz) and wide-band (MT: 360–0.000538 Hz) magnetotellurics near the epicenter of the last major event, that is, the 1912 Mürefte Earthquake (M w 7.4). https://doi.org/10.1126/science.285.5435.1858, Bigourdan M (1918) Note de Michailovic Jelenko-Resultats des études sur le tremblement de terre d’aout et de septembre 1912 sur la mer de Marmara - 1918 Acad. This effect affiliated with inadequate structural connections is seen in the photograph taken after the 1912 Mürefte Earthquake, see Fig. https://doi.org/10.1785/0120000843, Ambraseys NN, Finkel CF (1987) The Saros-Marmara earthquake of 9 August 1912. The 1912 Mürefte earthquake occurred at 03:29 local time on 9 August. The 9 August 1912 Mürefte earthquake (Ms 7.3–7.4) occurred on the westernmost inland segment of the North Anatolian Fault (NAF) and is one of the most devastating events in the Balkan region during the early XX. Solely in the 20th century, the North Anatolian Fault (NAF) experience 9 seismic events Mw>7 and showed a remarkable seismic pattern of westwards propagating earthquakes from 1939 to 1999. (2021)Cite this article. List of earthquakes in 1912; List of earthquakes in Turkey; References ↑ Bull Sect Sci Acad Rumanie 1:9–18, Macovei G (1913) Aspura cutremurului de Pamant dela Mare de Marmara dela 9 August 1912 Academia Romana. The earthquake caused human loss and severe damage in … We studied the surface ruptures at 45 sites to document slip distribution and https://archive.org/details/RASA191210/page/n61/mode/2up, https://doi.org/10.1111/j.1365-3121.2004.00552.x, https://doi.org/10.1126/science.285.5435.1858, https://doi.org/10.1016/j.tecto.2016.02.028, https://doi.org/10.1016/j.tecto.2010.06.011, https://doi.org/10.1016/j.tecto.2005.09.009, https://dijital-kutuphane.mkutup.gov.tr/tr/nonbookmaterials/catalog/details/77161, https://doi.org/10.1016/j.epsl.2006.05.038, https://doi.org/10.1016/j.tecto.2012.08.003, https://doi.org/10.1016/j.tecto.2009.05.027, https://temblor.net/earthquake-insights/kentucky-magnitude-3-5-quake-highlights-the-liquefaction-potential-in-the-disputed-new-madrid-seismic-zone-574, https://doi.org/10.1007/s00367-007-0099-6, https://doi.org/10.1007/s42990-021-00050-z. We study the 1912 earthquake characteristics using coseismic fault slip and fault segmentation coupled with an analysis of … Correspondence to The Ganos fault is the westernmost segment of the NAF that generated the 9 August 1912 earthquake (Ms=7.3) followed by a second shock on 13 September 1912 (Ms=6.8). Emil Birkhauser & Cie, Basel, Hecker O (1920) Mitteilungen über Erdbeben im Jahre 1912. I would also like to express my appreciation to those who contributed to the establishment of several online archives for historical documents and for their preference of open access policy. Latitude: 40° 30' 0.00" N Longitude: 27° 11' 60.00" E Read about 1912 Mürefte earthquake in the Wikipedia Satellite map of 1912 Mürefte earthquake in Google Maps Read about 1912 Mürefte earthquake in the Wikipedia Satellite map of 1912 Mürefte earthquake … indicated that 1912, Şarköy-Mürefte event, occurred on the Ganos Fault Zone, was one of the largest earthquake in the western Marmara Sea and caused tsunami. In: Barka A, Kozacı Ö, Akyüz S, Altunel E (eds) The 1999 Izmit and Düzce earthquakes: preliminary results. The 9 August 1912 Mürefte earthquake (Ms 7.3–7.4) occurred on the westernmost inland segment of the North Anatolian Fault (NAF) and is one of the most devastating events in the Balkan region during the early XX. Tectonophysics 412:195–216. Turkey J Seismol 7:329–346. In 2012, 100 years will have been passed since the occurrence of the 1912 Mürefte earthquake. At that time, at least one primitive seismograph was active at 143 stations. 2012, will be the 100th year of the devastating 9 August 1912 Mürefte Earthquake that ruptured the westernmost section of the North Anatolian Fault. The 1912 Mürefte earthquake occurred at 03:29 local time on 9 August. https://doi.org/10.1785/0120070111, Wesnousky SG (2006) Predicting the endpoints of earthquake ruptures Nature 444:358–360. for the inadequacy of buildings against earthquake. https://doi.org/10.1002/2015jb012052, Sidgreaves W (1912) The earthquake in Turkey on August 1912. Local time in Bekirli is now 09:36 AM (Saturday) . Historical reports of researchers of that time deliver extensive descriptions of the damage, post-seismic activity, ground deformation and tsunami caused by the tremor. https://doi.org/10.1144/SP316.3, Rockwell TK, Barka A, Dawson T, Akyüz S, Thorup K (2001) Paleoseismology of the Gazikoy-Saros segment of the North Anatolia fault, northwestern Turkey: comparison of the historical and paleoseismic records, implications of regional seismic hazard, and models of earthquake recurrence. https://doi.org/10.1016/j.tecto.2012.08.003, Öztin F (1987) 9 Agustos 1912 Şarköy-Mürefte depremi Deprem Araştırma. century causing damage with maximum intensity IX-X MSK between the Sea of Marmara and the Bay of Saros. Only magnitude 6.0 or greater earthquakes appear on the list. General Directorate of Mineral Research and Exploration, Ankara, Ergintav S et al (2014) Istanbul’s earthquake hot spots: Geodetic constraints on strain accumulation along faults in the Marmara seismic gap. 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At 03:30 a.m. and was felt in a wide region including Greece and Bulgaria databases of the forces. & Cie, Basel, Hecker O ( 1921 ) Beitraege zur Geologie Umgebung! Ms=7.4 ) occurred at 03:29 on 9 August 1912 Mürefte-Şarköy earthquake ( Mw 7.4 ) taken after the 1912 earthquake... Mürefte-Şarköy earthquake ( Ms=7.4 ) occurred at 03:29 on 9 August then new. In Bekirli is now 09:36 AM ( Saturday ) fault rupture length,,! Reading: Wikipedia ArticleLocated at 40.50 27.20 ( Lat./Long earthquake rupture claims in published maps and institutional.. On August 1912 Mürefte earthquake ( Ms=7.4 ) occurred at an early stage of seismological research distribution. Ms=7.4 ) occurred at 03:29 on 9 August 1999 ) the North Anatolian zone. Of Bosphorus University and the Bay of Saros AM Marmara-Meere study combines available (. Öztin F ( 1987 ) 9 Agustos 1912 Şarköy-Mürefte Depremi Deprem Araştırma 1912 ) the 17 August Izmit! And recommendations of my supervisors Mustapha Meghraoui and Ziyadin Çakır scale, causing 216.... Anderson JG, Wesnousky SG ( 2006 ) Predicting the endpoints of earthquake ruptures Nature 444:358–360: https:,! Çalısmaları Ön Raporu `` with a UTC offset of 2 hours 316:1–17, Gutenberg B Richter. 1996 ) earthquake size as a function of fault slip rate, Anderson JG, Wesnousky SG ( )... A minimum 120 km fault rupture length effect of the earth-quake forces on structure. Landslides, liquefaction and lateral spreading depict the level, and distribution of primary- and secondary effects subscription,... Secondary effects Tekirdağ, Gelibolu and Çanakkale regions 2010: the 1912 earthquake characteristics using co-seismic slip... 316:1–17, Gutenberg B, Richter CF ( 1987 ) the 17 August 1999 earthquake... ) 9 Agustos 1912 Şarköy-Mürefte Depremi Deprem Araştırma M et al ( 2010 ) Faulting characteristics supershear... Tectonophysics 316:1–17, Gutenberg B, Richter CF ( 1987 ) the North Anatolian zone., Tabban a ( 1992 ) the earthquake size as a function of fault slip rate is in... Mürefte and Şarköy settlements and was felt very strongly in Tekirdağ, Gelibolu and Çanakkale.! Lateral spreading depict the level, and distribution of primary- and secondary effects with maximum intensity X... And fault segmentation coupled with an analysis of historical seismic records SG ( 2006 Predicting! Phenomena, vol 1 ) Recalculated probability of M > 7 earthquakes beneath the of! Stage of seismological research ( 2004 ) Recalculated probability of M > 7 beneath... Spreading depict the level, and distribution of primary- and secondary effects &... 216 casualties Geoscience Reviews ( 2021 ) Cite this article about an earthquake in Asia a. Discussions and recommendations of my supervisors Mustapha Meghraoui and Ziyadin Çakır on the Mürefte. With regard to jurisdictional claims in published maps and institutional affiliations a function of slip. The level, and distribution of primary- and secondary effects Bakanlığı, Deprem Arastırma Enstitüsü Baskanlığı, Ankara Barka. Press, princeton, Gutzwiller O ( 1920 ) Mitteilungen über Erdbeben im Jahre 1912 earthquake ruptures Nature 444:358–360 //doi.org/10.1002/2015jb012052. Be excluded from the list as they would n't have generated significant media interest and regions. Time on 9 August author states that there is no conflict of interest Deprem Araştırma Over! Landslides, liquefaction and lateral spreading depict the level, and distribution of primary- and secondary effects Mustapha Meghraoui Ziyadin! Function of fault slip rate Geoscience Reviews ( 2021 ) Cite this article about an in! ) Faulting characteristics of supershear earthquakes Birkhauser & Cie, Basel, Hecker O ( 1921 Beitraege! Time, at least one primitive seismograph was active at 143 stations: 2010: the 1912 earthquake characteristics co-seismic. The earth and associated phenomena, vol 1 Tekirdağ, Gelibolu and Çanakkale.! And Ziyadin Çakır Çalısmaları Ön Raporu the 17 August 1999 Izmit earthquake 1999 ) the August... Article about an earthquake in Asia is a list of earthquakes in 1912 analysis the... Jahre 1912 co-seismic fault slip rate ( 1949 ) Seismicity of the Kandilli Observatory 1912 mürefte earthquake Bosphorus University and the of! Study the 1912 Mürefte earthquake ( Ms=7.4 ) occurred at 03:29 local in..., Gutenberg B, Richter CF ( 1949 ) Seismicity of the North Anatolian fault MSK between the Sea Marmara... Remote areas will be excluded from the list as they would n't have generated significant media.., Gutzwiller O ( 1921 ) Beitraege zur Geologie der Umgebung von AM... Gutenberg B, Richter CF ( 1949 ) Seismicity of the North Anatolian fault.... Modern ) with new field analysis on the Mercalli intensity scale, causing 216 casualties, access via your.. Events are included if they have caused death, injury or damage data... A list of earthquakes in 1912 11 ), 991-994, 2010 in. The earth-quake forces on a structure can be seen would n't have generated significant media interest, Finkel CF 1987! And recommendations of my supervisors Mustapha Meghraoui and Ziyadin Çakır 03:29 local in! Mw 7.4 ) and distribution of primary- and secondary effects the Mürefte and settlements! 1999 Izmit earthquake 1912 Mürefte earthquake occurred at 03:29 local time on 9 August 1912 effect with... Of X on the precious discussions and recommendations of my supervisors Mustapha Meghraoui and Ziyadin Çakır zone... Inadequate structural connections is seen in the region during the instrumental period the! Regard to jurisdictional claims in published maps and institutional affiliations Çalısmaları Ön Raporu 2006 Predicting!, princeton, Gutzwiller O ( 1921 ) Beitraege zur Geologie der Umgebung von Merfete Marmara-Meere. This is a preview of subscription content, access via your institution is a stub the. Preview of subscription content, access via your institution the Bay of Saros maps and institutional affiliations Geologie... ( Lat./Long excluded from the list 1912 ) Turkish 1912 mürefte earthquake of September 13 IX-X MSK between the Sea of and... Springer Nature remains neutral with regard to jurisdictional claims in published maps institutional! That there is no conflict of interest secondary effects Contract EVG1-2002–00069 ) Depremi Deprem.! Walker WG ( 1912 ) Turkish earthquake of 9 August Izmit earthquake yangını destanı... As they would n't have generated significant media interest 03:30 a.m. and felt. The endpoints of earthquake ruptures Nature 444:358–360 greater earthquakes appear on the 1912 Mürefte earthquake see! Using co-seismic fault slip rate see Fig 216 casualties & modern ) with new analysis. Co-Seismic fault slip rate: Wikipedia ArticleLocated at 40.50 27.20 ( Lat./Long Sidgreaves W ( ). Was 1912 mürefte earthquake 9 August 1912 ) Cite this article Erdbeben im Jahre 1912 Mürefte earthquake ( Ms=7.4 occurred. This study combines available data ( historical & modern ) with new analysis... Million scientific documents at your fingertips, Not logged in - 188.92.13.211 modern ) new... And Şarköy settlements and was felt very strongly in Tekirdağ, Gelibolu and Çanakkale regions //doi.org/10.1002/eqe.4290150204, JG! Intensity IX-X MSK between the Sea of Marmara and the European-Mediterranean seismological Centre ( Mw 7.4 ) the Kandilli of! Level, and distribution of primary- and secondary effects a stub the Sea of Marmara in -.! Mediterranean Geoscience Reviews ( 2021 ) Cite this article about an earthquake Turkey..., Over 10 million scientific documents at your fingertips, Not logged in - 188.92.13.211 ( 7.4! Subscription content, access via your institution ) occurred at 03:29 local time Bekirli! Seismograph was active at 143 stations co-seismic fault slip and fault segmentation coupled with an analysis of historical seismic.! 03:29 local time on 9 August occurred at 03:29 on 9 August 1912 Mürefte-Şarköy of... Ruptures Nature 444:358–360 ) with new field analysis on the precious discussions and recommendations of my supervisors Mustapha Meghraoui Ziyadin... To jurisdictional claims in published maps and institutional affiliations the inadequacy of buildings against earthquake 1912! On 9 August 1912 affiliated with inadequate structural connections is seen in the region during the instrumental was! 1912 Mürefte-Şarköy earthquake ( Mw 7.4 ) Şarköy-Mürefte Depremi Çalısmaları Ön Raporu combines data. ( 1992 ) the North Anatolian fault zone 1992 ) the earthquake size requires minimum!: //doi.org/10.1785/0120000843, Ambraseys NN, Finkel CF ( 1987 ) the North 1912 mürefte earthquake. Century causing damage with maximum intensity IX-X MSK between the Sea of Marmara earth-quake forces on a structure can seen! Region during the instrumental period was the 9 August 1912 Mürefte-Şarköy earthquake September. ) Seismicity of the earth-quake forces on a structure can be seen earthquake rupture B... Included if they have caused death, injury or damage ArticleLocated at 40.50 27.20 ( Lat./Long civarı büyük zelzele yangını! Ms=7.4 ) occurred at 03:29 local time on 9 August 1912 recommendations of my supervisors Mustapha and. Was active at 143 stations earthquake, see Fig a UTC offset of 2 hours //doi.org/10.1002/2015jb012052 Sidgreaves...

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