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Journal articles on the topic '1755 earthquake'

Author: Grafiati

Published: 4 September 2021

Last updated: 29 July 2025

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1

Chester, David K. "The 1755 Lisbon earthquake." Progress in Physical Geography: Earth and Environment 25, no. 3 (2001): 363–83. http://dx.doi.org/10.1177/030913330102500304.

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Affecting an area of ca. 800 000 km2 and killing up to 100 000 people, the Lisbon earthquake of 1755 is probably the greatest seismic disaster to have struck western Europe. The shock waves of the earthquake placed a temporary brake on the emerging rationalism of the European Enlightenment and attempts to explain the disaster in terms of human sinfulness coloured many contemporary accounts. Notwithstanding these difficulties, through careful archival research it has proved possible to obtain relatively value-free accounts of most aspects of the earthquake and to use these not only to model the

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MUKHERJEE, S. M. "Lisbon Earthquake of 1 November 1755." MAUSAM 6, no. 2 (2021): 149–58. http://dx.doi.org/10.54302/mausam.v6i2.4431.

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Available data on the Lisbon earthquake have been reviewed. Some new aspects of the earthquake have been brought out and a few others reinterpreted in the light of data of the recent Assam earthquake. The fresh calculations made show that this Lisbon earthquake may be considered as the strongest of all shooks for which scientific data are available. The magnitude of the earthquake has been approximately determined as 8.7 and energy between 1017 ergs and 7 X 1017 ergs or double the energy of the Assam earthquake of 1950 with depth of focus 18 km. Seiches appear to be associated with shall

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Dąbrowska, Magdalena. "Śmierć nagła. Rosjanie wobec trzęsienia ziemi w Lizbonie w 1755 roku." Slavica Wratislaviensia 167 (December 21, 2018): 83–98. http://dx.doi.org/10.19195/0137-1150.167.7.

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A sudden death: Russians about the Great Lisbon Earthquake in 1755The article presents three groups of texts about the earthquakes and the Great Lisbon Earthquake in 1755, published in Russia in the Enlightenment: 1. the articles from the journal “Sankt-Petersburgskie vedomosti” 1755, 2. the scientific and popular science articles about the earthquakes Mikhail Lomonosov, 1757 etc., 3. the works concerning the Poem on the Lisbon Disaster by Voltaire and the J.J. Rousseau’s letter about it translation of Poem on the Lisbon Disaster by Ippolit Bogdanovich, 1763; translation of the Rousseau’s let

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Udías, Agustín. "Development of seismology in Spain in the context of the three large earthquakes of 1755, 1884 and 1954." Earth Sciences History 32, no. 2 (2013): 186–203. http://dx.doi.org/10.17704/eshi.32.2.f1168212m214l532.

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The occurrence of large earthquakes is in many cases a catalyst for the advancement of seismology. This article examines the influence of the three large earthquakes of 1755, 1884 and 1954, felt in the Iberian peninsula, in the development of seismology in Spain. The 1755 earthquake was the occasion for the establishment of the study of earthquakes as natural phenomena outside of religious considerations and the introduction of modern ideas about the origin of earthquakes. The 1884 earthquake was the first earthquake in Spain subject to a serious and detailed scientific study by three commissi

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Sanz de Ojeda, Andrés, Iván Alhama, and Eugenio Sanz. "Aquifer Sensitivity to Earthquakes: The 1755 Lisbon Earthquake." Journal of Geophysical Research: Solid Earth 124, no. 8 (2019): 8844–66. http://dx.doi.org/10.1029/2019jb017753.

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Chester, D. K. "The 1755 Lisbon earthquake." Progress in Physical Geography 25, no. 3 (2001): 363–83. http://dx.doi.org/10.1191/030913301680193823.

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Justo, J. L., and C. Salwa. "The 1531 Lisbon earthquake." Bulletin of the Seismological Society of America 88, no. 2 (1998): 319–28. http://dx.doi.org/10.1785/bssa0880020319.

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Abstract In January 1531, the Tagus River Estuary was hit by a strong earthquake, the intensity of which in Lisbon was, according to relevant authors, greater than that of the 1755 earthquake. It was cited by most of the European annalists of the time and was responsible for the destruction of structures, the loss of lives, and enormous panic, thus making it one of the most disastrous earthquakes in the history of Portugal. If we give credit to the detailed descriptions, the maximum intensity was probably X MSK. According to our study, the seismic event was probably caused by the Lower Tagus f

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Purba, Siti M., Yaumil F. Alyssa, Mustika Nadia, Nadiatul Asra, and Umar Muksin. "The Influence of Seismometer Coverage on the Earthquake Focal Mechanism Solution (Case Study: Toba Swarm Earthquake)." IOP Conference Series: Earth and Environmental Science 1479, no. 1 (2025): 012014. https://doi.org/10.1088/1755-1315/1479/1/012014.

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Abstract The focal mechanism of an earthquake is necessary to describe the plane and characteristics of the fault. In the case of local earthquakes, the focal mechanism is often determined based on the first polarity of the primary wave. Therefore, the quality of the earthquake focal mechanism depends on the station coverage and the number of first polarities of primary waves. This study aims to investigate the variation in solution and quality of earthquake focal mechanisms with different station coverage. We conducted experiments on Toba swarm earthquake data for the May-June 2021 period wit

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Udías, Agustín, Elisa Buforn, José Manuel Martínez-Solares, and Carlos Sousa Oliveira. "Historical Sources for Earthquakes before 1900 on the Iberian Peninsula and in the Offshore Region." Seismological Research Letters 91, no. 5 (2020): 2487–96. http://dx.doi.org/10.1785/0220200038.

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Abstract Information about historical earthquakes in the Iberian Peninsula going back to Antiquity (Roman times) can be found in different types of documents, such as unpublished contemporary manuscripts preserved in archives, general, and regional histories in Spain and Portugal, published documents and reports on the damage of specific earthquakes, and reports in newspapers and magazines. The 1755 Lisbon earthquake marks an important point for the study of historical earthquakes in the peninsula. The compilation and interpretation of historical data presents many problems, one of which is ho

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Robles, Whitney Barlow. "Atlantic Disaster: Boston Responds to the Cape Ann Earthquake of 1755." New England Quarterly 90, no. 1 (2017): 7–35. http://dx.doi.org/10.1162/tneq_a_00583.

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This article examines religious, scientific, and media responses to the 1755 Cape Ann earthquake, which affected Boston and other regions throughout the Atlantic world. The earthquake's prolonged generation of environmental data challenged American colonists' attempts to achieve certainty about the natural disaster. Further news of the famous and devastating Lisbon earthquake forced Americans to broaden their horizon of environmental change to one that extended into the ocean–a formative moment for the development of transatlantic science, and one that can help historians resolve seemingly opp

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Pérez-López, R., J. L. Giner-Robles, M. A. Rodríguez-Pascua, et al. "Lichenometric dating of coseismic rockfall related to the Great Lisbon Earthquake in 1755 affecting the archaeological site of "Tolmo de Minateda" (Spain)." Zeitschrift für Geomorphologie, Supplementary Issues 62, no. 2 (2019): 271–93. http://dx.doi.org/10.1127/zfg_suppl/2019/0504.

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Dating earthquake geological effects associated with historical earthquakes gives us relevant information for estimating the seismic acceleration value experienced in the ground. Historical manuscripts describing earthquakes and its effects help to assign a seismic intensity about the ground motion. In this context, lichenometry represents a good semi-quantitative method for dating exposed rock surfaces related to earthquake phenomena. In this work, we have carried out a lichenometry analysis for dating a large rockfall located 700 km from the epicentre of the Great Lisbon Earthquake, which oc

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Oldroyd, David, Filomena Amador, Jan Kozák, Ana Carneiro, and Manuel Pinto. "The Study of Earthquakes in the Hundred Years Following the Lisbon Earthquake of 1755." Earth Sciences History 26, no. 2 (2007): 321–70. http://dx.doi.org/10.17704/eshi.26.2.h9v2708334745978.

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This paper traces some of the main developments in the study of earthquakes and their scientific investigation from 1755 (the year of the Great Lisbon Earthquake: GLE) to 1855. The GLE was widely reported and discussed, though at that time there was no systematic and accurate collection of seismic data so that the event did not in itself lead to significant scientific advances. But an idea is given of the attempts as regards Portugal and Spain to explain the GLE in the terms of the day. In 1760, John Michell described methods for ascertaining (in principle) the position of what would today be

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Fonseca, Joao F. B. D. "A Reassessment of the Magnitude of the 1755 Lisbon Earthquake." Bulletin of the Seismological Society of America 110, no. 1 (2020): 1–17. http://dx.doi.org/10.1785/0120190198.

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ABSTRACT The 1755 Lisbon earthquake is still poorly understood due to its offshore location and complex macroseismic intensity pattern. Gutenberg and Richter (1949) tentatively assigned a magnitude between 8¾ and 9 judging from an estimated perceptibility radius of 2500 km. More recent attempts to estimate the magnitude from isoseismal areas led to results in the 8.5–8.7 range. These values have been adopted in several studies of the seismic hazard of southwest Iberia. In this article, I use the available macroseismic data—a total of 1206 data points from Portugal, Spain, and Morocco—to reasse

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Ioganson, Lidia, Galina Donzova, and Leyla Fleifel. "Atlantic seaquakes on 1.XI.1755 (Great Lisbon earthquake) and 31.III.1761." Russian Journal of Seismology 4, no. 2 (2022): 7–22. http://dx.doi.org/10.35540/2686-7907.2022.2.01.

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The article deals with data on the seismic regime before and after the Lisbon earthquake on November 1, 1755, which was accompanied by an unusual seismic activation over a large area of Western Europe, North Africa and the Atlantic, which is practically not reflected in the scientific literature. After November 1, 1755, the seismic series was observed in Western Europe, which cannot be attributed to the typical aftershock process. A distinctive feature of the post-Lisbon three phase-activ ation was the occurrence of ea rthquakes, sometimes simultaneously, in separated isolated regions of Europ

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GUTSCHER, M. A. "The great Lisbon earthquake and tsunami of 1755: lessons from the recent Sumatra earthquakes and possible link to Plato's Atlantis." European Review 14, no. 2 (2006): 181–91. http://dx.doi.org/10.1017/s1062798706000184.

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Great earthquakes and tsunami can have a tremendous societal impact. The Lisbon earthquake and tsunami of 1755 caused tens of thousands of deaths in Portugal, Spain and NW Morocco. Felt as far as Hamburg and the Azores islands, its magnitude is estimated to be 8.5–9. However, because of the complex tectonics in Southern Iberia, the fault that produced the earthquake has not yet been clearly identified. Recently acquired data from the Gulf of Cadiz area (tomography, seismic profiles, high-resolution bathymetry, sampled active mud volcanoes) provide strong evidence for an active east dipping sub

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Annisa, Y., G. C. Astriyan, S. Wahyunia, N. Indrastuti, and M. F. I. Massinai. "Determination of Hypocenter Using Geiger Method in Sinabung Volcano, April-July 2016 Period." IOP Conference Series: Earth and Environmental Science 873, no. 1 (2021): 012007. http://dx.doi.org/10.1088/1755-1315/873/1/012007.

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Abstract Sinabung is a volcano located in the Karo Highlands, Karo District, North Sumatra, Indonesia, with the highest peak of 2460 meters mean sea level. Volcanic earthquake is an earthquake that occurs due to volcanic activity. This is caused by the movement of magma upwards in the volcano. This study aims to determine the type of earthquake, hypocenter position and epicenter of volcanic earthquakes in Sinabung volcano in April-July 2016. The principle of this study was carried out by analyzing volcanic earthquake data in Sinabung volcano in April-July 2016. The data is recorded data (seism

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Zakaria, Salsabila Aulia Putri, Intan Noviantari Manyoe, Alan Gani Abduh, and Fadillah Budjang. "Seismicity map to analyze the depth and magnitude earthquake zone in Kwandang Area of North Gorontalo Regency." IOP Conference Series: Earth and Environmental Science 884, no. 1 (2021): 012060. http://dx.doi.org/10.1088/1755-1315/884/1/012060.

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Abstract Kwandang is a district located in the northern part of Gorontalo. The purpose of this research is to analyze the depth and magnitude earthquake zone that occurred in the district of Kwandang, Gorontalo Utara regency based on seismicity map. The astronomical research location is located at 0° 49' 39" S, 122° 55' 8" E. The method used in this research is seismicity map analysis. The earthquake that dominates in Kwandang, based on the value of its depth, namely shallow earthquake (0-70 km) and medium earthquake (70-300 km). This is caused by subduction activity in the direction of the su

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Al-Heety, Emad A., Huda F. Rafea, and Osama J. Mohammad. "Evaluation of Return Period and Occurrence Probability of the Maximum Magnitude Earthquakes in Iraq and Surroundings." IOP Conference Series: Earth and Environmental Science 1300, no. 1 (2024): 012001. http://dx.doi.org/10.1088/1755-1315/1300/1/012001.

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Abstract It has long been clear that earthquake prediction is important from both social and economic perspectives; therefore, the practical objective of today’s earthquake seismology researchers is an effective earthquake prediction program. The purpose of this study is to estimate earthquake probabilities and return periods using an updated earthquake catalogue (1900-2019) for Iraq and its surroundings. Weibull’s formula and inverse Weibull’s formula were employed to calculate the period of return and the occurrence probability of the maximum magnitude earthquake. The return period for earth

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Dewi, CN, F. Febriani, T. Anggono, et al. "Anomalous geomagnetic activities before the Karangasem - Bali, Indonesia earthquakes on December 13, 2022." IOP Conference Series: Earth and Environmental Science 1373, no. 1 (2024): 012010. http://dx.doi.org/10.1088/1755-1315/1373/1/012010.

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Abstract A series of earthquakes occurred on Bali Island, Indonesia, on December 13, 2022. The United States Geological Survey (USGS) recorded four shallow earthquakes around Karangasem - Bali with magnitude (M) > 4 at that time. The largest was the M 5.2 earthquake, which occurred at 10:38:21.67 UTC with 10 km of depth. We analyzed the anomalous geomagnetic activities during these earthquakes by utilizing the geomagnetic data from the Bayan geomagnetic station located on Lombok Island, less than 100 km from the earthquake’s epicenters. We conducted the polarization ratio analysis by applyi

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Barreiros, Maria Helena. "Urban Landscapes: Houses, Streets and Squares of 18th Century Lisbon." Journal of Early Modern History 12, no. 3-4 (2008): 205–32. http://dx.doi.org/10.1163/157006508x369866.

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AbstractThis article retraces Lisbon's urban evolution, both planned and spontaneous, from the beginning of the Age of Discovery until the first decades of the 19th century. It highlights the 1755 earthquake as a powerful agent of transformation of Lisbon, both of the city's image and architecture and of street life. The article begins by summing up urban policies and urban planning from Manuel I's reign (1495-1521) to João V's (1707-1750); it goes on to depict Lisbon's daily life during the Ancien Regime, focusing on the uses of public and private spaces by common people. The Pombaline plans

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Murjaya, Jaya, Suaidi Ahadi, Petrus Demon Sili, et al. "Reconstruction of paleoearthquakes impact and its return period perspective study to support infrastructure resilience program (case study: paleoearthquakes in mainland island of Sumatra)." IOP Conference Series: Earth and Environmental Science 1479, no. 1 (2025): 012004. https://doi.org/10.1088/1755-1315/1479/1/012004.

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Abstract Sumatra island is one of earthquake prone area in Indonesia. Some of paleoearthquakes occurred in Sumatra Island and its vicinity as like earthquakes in Siberut island on 1797 with magnitude (M) 8.6-8.8, Bengkulu on 1833 (M 8.8-9.1) and Nias island on 1861 (M ∼8.5). All of earthquakes triggered of tsunami. Beside that some of paleoearthquakes occurred also in mainland island of Sumatra like as the earthquake on 1822, 1892 (M ∼ 7.7), 1909 (M∼7.6), 1921 (M∼7), 1933 (M∼7.5) and 1936 (M∼7.1) respectively. The purposes of this study to reconstruct of paleoearthquakes shaking impact, and es

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Ebel, John E. "Using Aftershocks to Help Locate Historical Earthquakes." Seismological Research Letters 91, no. 5 (2020): 2695–703. http://dx.doi.org/10.1785/0220200041.

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Abstract For historical earthquakes, the spatial distributions of macroseismic intensity reports are commonly used to estimate the event locations. The methods to locate historical earthquakes assume that the highest seismic intensity shows the best estimate of the location of the earthquake. Uncertainties in the locations estimated from macroseismic data can be due to an uneven geographic distribution of sites with intensity reports, variations in intensities due to local soil conditions, ambiguous historical reports, and earthquake directivity effects. Additional constraint on the location o

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Ramdhan, M., Priyobudi, A. Mursityanto, K. H. Palgunadi, and Daryono. "Analysis of M 5.3 Sumbawa, Indonesia earthquake 2020 and its aftershocks based on hypocenter relocation from BMKG seismic stations." IOP Conference Series: Earth and Environmental Science 873, no. 1 (2021): 012070. http://dx.doi.org/10.1088/1755-1315/873/1/012070.

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Abstract The 2020 Sumbawa earthquake of moderate magnitude (M 5.3) produced very significant aftershocks. Based on the computation of Utsu’s method, those aftershocks would be ended after the 20th day. Those earthquakes along 20 days were relocated using double-difference method. The relocation results show the southwest-northeast orientation and getting deeper into the northwest direction. Those two directions show the strike and the dip from the fault plane of the earthquake which was consistent with the focal mechanism released by the Indonesian Agency for Meteorology, Climatology, and Geop

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Chin, Su Na, Tongkul Felix, Zaturrawiah A. Omar, and Roslee Rodeano. "Nowcasting Earthquake Occurrence in Sabah." IOP Conference Series: Earth and Environmental Science 1103, no. 1 (2022): 012041. http://dx.doi.org/10.1088/1755-1315/1103/1/012041.

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In line with the increasing availability of seismic data, nowcasting method provides a systematic way to depict the current state of earthquake hazard within a specific geographic area. This paper implements nowcasting method to statistically assess the earthquake progression in Sabah region over the large earthquakes cycle. The analysis includes earthquake data in the state of Sabah and the surrounding regions, which is acquired from Malaysia Meteorological Department catalogue and United States Geological Survey (USGS) catalogue from year 2009 to 2018. This study discovered that EPS correspo

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Askaviolita, Sito Ismanti, and Teuku Faisal Fathani. "Liquefaction Potential Index Analysis in Solo – Yogyakarta - NYIA Kulon Progo Toll Road (Section Karanganyar to Klaten Regency) at Central Java." IOP Conference Series: Earth and Environmental Science 1244, no. 1 (2023): 012031. http://dx.doi.org/10.1088/1755-1315/1244/1/012031.

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Abstract Liquefaction had occurred in Yogyakarta due to an earthquake of moment magnitude, Mw 6.3 on May 27, 2006. This earthquake caused severe damage in several areas in Central Java. The study area in this construction was located mostly in some areas of Central Java Province that had a shallow groundwater table and often occurred earthquakes that might trigger liquefaction. The objective of this study was to analyze liquefaction potential in the construction of Solo – Yogyakarta – NYIA Kulon Progo toll road especially sta. 00+000-07+500 From Colomadu, Karanganyar Regency to Delanggu, Klate

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Zakir, Rahmat Fadli, Abdul Hakam, Bambang Istijono, Melinda Noer, and Syafira Rahmadilla Hape. "Vulnerability Assessment of non-engineered houses related to earthquake in West Pasaman District." IOP Conference Series: Earth and Environmental Science 1173, no. 1 (2023): 012075. http://dx.doi.org/10.1088/1755-1315/1173/1/012075.

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Abstract The earthquake on February 25, 2022, in West Pasaman resulted in damage to people’s houses as well as fatalities. The quake happened just under the Mount of Talamau, 18 km northeast of the city of Simpang Empat City, with a magnitude of 5.2 M. This earthquake was followed by small earthquakes that occurred until February 27, 2022. Damage to houses in the earthquake-affected area became the focus of attention in this research to assess the housing vulnerability related to the earthquake hazard. The vulnerability assessment of house buildings is critical in earthquake-prone areas becaus

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Silva, Pablo G., Miguel A. Rodríguez-Pascua, Jorge L. Giner Robles, Javier Élez, Raúl Pérez-López, and M. Begoña Bautista Davila. "Catalogue of the Geological Effects of Earthquakes in Spain Based on the ESI-07 Macroseismic Scale: A New Database for Seismic Hazard Analysis." Geosciences 9, no. 8 (2019): 334. http://dx.doi.org/10.3390/geosciences9080334.

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This paper summarizes the content and scope of the “Catalogue of Earthquake Geological Effects in Spain”. The catalogue has been published by the Geological Survey of Spain (IGME) and constitutes the first official publication (in Spain) on seismic hazard containing geological information. The catalogue gathers the 51 stronger earthquakes that have occurred in Spain since the Neolithic period to the present and classifies earthquakes with geological or archaeological seismic records in paleoseismic, ancient, historical and instrumental earthquakes. The catalogue offers a variety of parametric

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Dhira, Y., I. Meilano, and D. W. Dudy. "Analysis of Tectonic Plate Velocity Variations in the Sunda Strait Based on GPS Time-series Data." IOP Conference Series: Earth and Environmental Science 873, no. 1 (2021): 012084. http://dx.doi.org/10.1088/1755-1315/873/1/012084.

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Abstract Indonesia is an earthquake-prone country located in the junction of four tectonic plates, namely the Indo-Australian, Eurasian, Philippine, and Pacific. The convergent boundary between tectonic plates is also called a subduction zone that can produce great earthquakes in the future. One of the subduction zones in Indonesia is the Sunda Strait subduction zone which predicted can release a M7.8 earthquake. Previous research stated that there is a change in tectonic plate velocity after an earthquake ruptured. It is likely that this could happen in the Sunda Strait area which has experie

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Bačić, Ž., D. ugar, V. Poslončec-Petrić, and Z. Nevistić. "Providing rapid earthquake information using EO/GI technology." IOP Conference Series: Earth and Environmental Science 1109, no. 1 (2022): 012006. http://dx.doi.org/10.1088/1755-1315/1109/1/012006.

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Abstract Strong earthquakes occur frequently with devastating effects on people and infrastructure. In cases of such catastrophic earthquakes, rescue and all other civil protection services need all available information about the earthquake itself and the consequences it has caused. In addition to the series of traditional sensors and systems used to interpret earthquakes and their consequences, remote observation sensors from space (EO) combined with geoinformation technologies (GI) are increasingly used today. By applying them, it is possible to quickly provide a wide range of useful inform

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POIRIER, JEAN-PAUL. "The 1755 Lisbon disaster, the earthquake that shook Europe." European Review 14, no. 2 (2006): 169–80. http://dx.doi.org/10.1017/s1062798706000172.

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The Lisbon earthquake is famous for its central role in the 18th century ‘quarrel of Optimism’. The accounts of the disaster by some witnesses are presented and the contributions that the earthquake inspired to many European authors, less well-known than Voltaire, in the domains of science, literature, religion and philosophy, are summarily reviewed. The paper emphasizes the repercussions the earthquake had in Germany, quite remote from the disaster area, but intellectually much alive, at the time of Frederic II.

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Alyssa, Yaumil Farah, Siti Maryam Purba, Nadiatul Asra, Mustika Nadia, and Muksin Umar. "Manual Detection of P and S Wave Arrival Times and Re-localization of the 2021 Toba Swarm Earthquake from Temporary Seismic Network." IOP Conference Series: Earth and Environmental Science 1458, no. 1 (2025): 012020. https://doi.org/10.1088/1755-1315/1458/1/012020.

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Abstract The epicenter of the 2021 swarm earthquake was previously determined automatically using the STA/LTA method. Although, the results obtained show that the distribution of earthquake epicenters still needs to be accurate. This is shown by errors in determining the arrival times of P and S waves. Therefore, in this study, we try to improve the location of the earthquake epicenter manually. This manual detection method is done by re-analyzing the arrival times of P and S waves, which are recorded at each station, one by one. This study aims to determine the pattern of the 2021 Toba swarm

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Gisler, Monika, Donat F�h, and Nicholas Deichmann. "The Valais earthquake of December 9, 1755." Eclogae Geologicae Helvetiae 97, no. 3 (2004): 411–22. http://dx.doi.org/10.1007/s00015-004-1130-9.

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Pritaningtyas, Aulia Dhita, Mohammad Hasib, Estu Kriswati, Novianti Indrastuti, and Tati Zera. "Analyses of explosion earthquakes at Sinabung Volcano: characteristics of waveform, spectra, and energy." IOP Conference Series: Earth and Environmental Science 1227, no. 1 (2023): 012028. http://dx.doi.org/10.1088/1755-1315/1227/1/012028.

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Abstract The characteristic of explosion earthquakes associated with lava avalanche at Sinabung volcano from October to December 2014 is investigated. The 1-component short-period seismometers which are Sukanalu (SKN), Laukawar (KWR), and Kebayaken (KBY) are used. All stations are located about 3-9 km away from the summit. The result shows the characteristics of these waveforms as follows; the amplitude increases rapidly to maximum for about 2-5 s, then the amplitude is almost constant for about 30-40 s followed by the gradual decrease of amplitude for about 40-50 s. Most of explosion earthqua

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Murjaya, J., S. Pramumijoyo, D. Karnawati, et al. "Earthquake risk assessment of the Opak and Merapi-Merbabu active faults to support mitigation program in Yogyakarta province and its vicinity." IOP Conference Series: Earth and Environmental Science 851, no. 1 (2021): 012001. http://dx.doi.org/10.1088/1755-1315/851/1/012001.

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Abstract Based on historical records, Yogyakarta has a high seismic risk related to the earthquake events along active faults, such as the Opak and Merapi-Merbabu Faults. These faults were responsible for several destructive earthquakes in Yogyakarta City and its vicinity and caused fatalities and building damage in the area, e.g., the 2006 (Mw 6.3) Yogyakarta earthquake and earlier in 1943 and 1867. A previous study shows that the Opak Fault has a geodetic slip-rate of 5 mm/y and a potential magnitude Mw 6.6. In addition, the active Merapi-Merbabu Fault has a geodetic slip-rate of 1 mm/y and

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Sauri, S., A. Rifa’i, and H. C. Hardiyatmo. "The Effect of Various Peak Ground Acceleration Level in Petobo Irrigation Canal Area Post 2018’s Liquefaction Disaster." IOP Conference Series: Earth and Environmental Science 1091, no. 1 (2022): 012038. http://dx.doi.org/10.1088/1755-1315/1091/1/012038.

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The soil liquefaction disaster in Petobo, Central Sulawesi, caused massive terrain damage. With a total displacement of up to 800 meters and a total sliding area of 1.43 km2, the soil structure was deformed. The 7.5 Mw earthquake with the maximum PGA of 0.45 was causing flow-induced liquefaction with a distance from the crown to the foot of the landslide as far as 2 km. The research aims to find out how well the post-earthquake soil can withstand the potential to liquefaction if it is hit by various earthquake levels. This research will conduct several simulations to determine the soil perform

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Andiana, Salsabila Atalieani, Saptono Budi Samodra, and Nugroho Budi Wibowo. "Microzonation of Earthquake Hazard Using Analytical Hierarchy Process (AHP) in The Sri Gethuk Waterfall Tourist Area and Surroundings, Playen and Dlingo Subdistrict, Special Region of Yogyakarta." IOP Conference Series: Earth and Environmental Science 1517, no. 1 (2025): 012013. https://doi.org/10.1088/1755-1315/1517/1/012013.

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Abstract The Special Region of Yogyakarta is an area that frequently affected by earthquakes. One of the historically destructive earthquakes was the 6.3 Mw earthquake on May 27, 2006, caused by the Opak Fault, known for causing significant damage and loss of life. In 2023, the Yogyakarta region experienced 2,202 earthquakes, with the peak occurring on December 13, 2023—a 3.6 Mw earthquake whose epicenter is located near the Sri Gethuk Waterfall. This research aims to determine earthquake hazard microzonation in the Sri Gethuk Waterfall tourist area and its surroundings based on seven paramete

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Thippa, Pavan Kumar, R. K. Tripathi, and Govardhan Bhat. "A case study on performance of structures during Turkey-Syria multiple earthquakes occurred on February 6, 2023." IOP Conference Series: Earth and Environmental Science 1280, no. 1 (2023): 012023. http://dx.doi.org/10.1088/1755-1315/1280/1/012023.

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Abstract Buildings are an important components of both urban and rural infrastructure, and it is crucial that they perform well during a seismic event. The earthquakes occurred on February 6, 2023 in Kahramanmaras, Turkey, which also had an impact on eleven other locations surrounding it. Turkey has suffered significantly from fatalities as well as damage to structures and other facilities. The area was severely damaged by two earthquakes, Mw7.7 and Mw7.6, which occurred within a time window of roughly 9 hours on February 6, 2023 in Turkey. Seismic regulations only take into account the design

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Mehta, Rahul, and Mohit Bhandari. "Evaluation of Seismic Response of Composite Buildings under Near-Field Earthquakes." IOP Conference Series: Earth and Environmental Science 1110, no. 1 (2023): 012016. http://dx.doi.org/10.1088/1755-1315/1110/1/012016.

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Abstract This paper represents the effectiveness of the bracing system concerning the seismic performance of steel-concrete composite buildings by comparing 5-storey composite buildings with and without bracings subject to extreme earthquake loads. The nonlinear time history analysis (NTHA) is carried out on the specific building models considered for this study. The seismic response is obtained in terms of different seismic response parameters which are further compared to determine the effect of the bracing system. The results obtained by applying real earthquake records of different near-fi

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Murjaya, Jaya, Aditya Setyo Rahman, Petrus Demon Sili, et al. "Earthquake Risk Potential Caused by Active Faults in Sumatra (Case Study: Earthquakes in the Land of West Sumatra Province and its vicinity)." IOP Conference Series: Earth and Environmental Science 1244, no. 1 (2023): 012037. http://dx.doi.org/10.1088/1755-1315/1244/1/012037.

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Abstract The land of West Sumatra province is one of prone area stricken by the destructive earthquakes. Based on historical records, the land of West Sumatra province has a high seismic risk related to the earthquake events along active faults, such as the Sianok, Barumun, Sumani, Siulak and Angkola faults. Some destructive earthquakes occurred in these faults and caused fatalities in West Sumatra area and its vicinity, e.g., the earthquakes near Bukit Tinggi district in 1926, 1977, 2007 (doublet earthquakes-Tabel 1) and 2022. A previous study shows that the Sumani, Siulak, Sianok, Barumun an

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Carrilho, Fernando, Susana Custódio, Mourad Bezzeghoud, et al. "The Portuguese National Seismic Network—Products and Services." Seismological Research Letters 92, no. 3 (2021): 1541–70. http://dx.doi.org/10.1785/0220200407.

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Abstract Portugal, located in the southwest region of the Eurasian plate, has been affected by several destructive earthquakes throughout its history, the most well-known being the 1755 Great Lisbon earthquake. The seismicity of the territory, both in the mainland and in the Azores and Madeira islands, has prompted the continuous development of seismic monitoring, from the first known macroseismic inquiry, following the 1755 Great Lisbon earthquake, to the current state-of-the-art seismic network. Once scattered in separate efforts, at present, most seismic stations in Portugal relay its data

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Arubi, D., Zulfakriza, S. Rosalia, D. P. Sahara, and N. T. Puspito. "Estimation of B-Value Variation as Earthquake Precursor in Java Region with Maximum Likelihood Method." IOP Conference Series: Earth and Environmental Science 1047, no. 1 (2022): 012027. http://dx.doi.org/10.1088/1755-1315/1047/1/012027.

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Abstract Java Island is one of the areas with a population density of 1,171 people/km2, which is relatively high compared to other regions in Indonesia. The tectonic setting of the Java region is affected by the interaction of tectonic plate subduction between the Indo-Australian Plate and the Eurasian Plate which moves at the rate of 67 mm/year. In addition, the presence of several active faults on Java Island also contributes to the tectonic setting. The implication of this setting is a relatively high level of potential earthquake events and some of them are destructive earthquakes. The est

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Nurhandoko, Bagus Endar B., M. Rizka Asmara Hadi, Kaswandhi Triyoso, et al. "Sanding Wells on The Island of Lombok due to Earthquake Vibrations." IOP Conference Series: Earth and Environmental Science 873, no. 1 (2021): 012091. http://dx.doi.org/10.1088/1755-1315/873/1/012091.

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Abstract The Lombok earthquake in 2018 was unique, the shocks occurred sequentially. Several major earthquakes were followed by thousands of aftershocks. The earthquake caused a devastating disaster which destroyed many homes, buildings including wells as the main fresh water supply in the Lombok Island. The focal mechanism of main earthquake shows a thrust fault mechanism. Lombok Island is originally a volcano Island which is still growing actively. Therefore surface of Island is dominated by volcanic materials, such as: volcanic rock, volcanic ash, pumice. This paper describes the phenomenon

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Rakhman, Heryawan Kurnia, Sito Ismanti, and Trias Aditya. "Comparison of peak ground acceleration using deterministic and probabilistic approach in the coastal area of Loh Buaya, Rinca Island, Indonesia." IOP Conference Series: Earth and Environmental Science 1298, no. 1 (2024): 012014. http://dx.doi.org/10.1088/1755-1315/1298/1/012014.

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Abstract An area located near an active volcano, subduction zone, and/or active fault has a risk of an earthquake. Earthquakes can cause damage to buildings with a large number of losses. One of the earthquake-related parameters required in planning an earthquake-resistant building is the Peak Ground Acceleration (PGA). The objective of this study is to compare the PGA value at the coastal area of Loh Buaya, Rinca Island, Indonesia, using Probabilistic Seismic Hazard Analysis (PSHA) and Deterministic Seismic Hazard Analysis (DSHA). The DSHA is calculated based on earthquake data series from th

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Astuti, A. P., N. S. Arifuddin, M. I. Tahir, E. M. Elsera, and M. F. I. Massinai. "Characteristic of 27^th September – 7^th October 2017 earthquake swarms in Jailolo Volcano, West Halmahera, Indonesia, based on hypocenter and b-value." IOP Conference Series: Earth and Environmental Science 851, no. 1 (2021): 012004. http://dx.doi.org/10.1088/1755-1315/851/1/012004.

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Abstract Halmahera is an area with active tectonics, so it has a high level of seismicity. Swarm earthquakes occurred in Jailolo from November to December 2015, and then in 2017, another earthquake swarm occurred from September to October. This earthquake is characterized by an increase in the number of earthquakes in a certain period with a relatively small magnitude, without mainshocks, and occurs in volcanic areas. This research used arrival time from P and S waves recorded at Taide Digital Seismograph (TDS) which was positioned at Ternate Geophysical Station (TNTI). We used cross-section o

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Martha, Agustya Adi, Angga Setiyo Prayogo, Jimmi Nugraha, Suliyanti Pakpahan, and Nelly Florida Riama. "Network of Radon Gas Concentration Monitoring of Research and Development Centre – BMKG for Earthquake Precursor Research in Indonesia." IOP Conference Series: Earth and Environmental Science 873, no. 1 (2021): 012006. http://dx.doi.org/10.1088/1755-1315/873/1/012006.

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Abstract The geographical position of Indonesia, which is flanked by several subduction zones and the presence of active faults in the sea and land make Indonesian territory prone to earthquakes and tsunamis which can result in many deaths and damaged. There are several efforts we can do to minimize the occurrence of earthquakes, including developing earthquake resistant buildings, increasing the ability/capacity of the community, and predicting earthquakes or better known as earthquake precursors. The BMKG Research Centre began conducting research on earthquake prediction using several method

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Rini, J. A., and N. C. Idham. "The development of structure in the limasan- and joglo-style vernacular houses after the 2006 Yogyakarta earthquake." IOP Conference Series: Earth and Environmental Science 933, no. 1 (2021): 012030. http://dx.doi.org/10.1088/1755-1315/933/1/012030.

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Abstract After a great earthquake hit the Special Region of Yogyakarta, Indonesia, in the year of 2006, some of the owners of the limasan- and joglo-style vernacular houses rebuilt their houses according to the education they received about the principles of earthquake-resilient building. This study investigates the structural development on the 11 (eleven) houses located in the Kabupaten (district) of Bantul, which was among the areas most affected by the earthquake. The owners combined the existing wooden main structural frame withstanding the earthquake with the new reinforced concrete stru

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Octavia, Karina, Jian-Hong Wu, and Luky Handoko. "Investigating the Stability of the Candi Kelir using DDA." IOP Conference Series: Earth and Environmental Science 1249, no. 1 (2023): 012016. http://dx.doi.org/10.1088/1755-1315/1249/1/012016.

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Abstract Candi Kelir, which is a candi in Prambanan, is a historical masonry structures threatened by high potency of earthquake in Indonesia. Investigating the stability of Candi Prambanan is essential for determining the capability to withstand earthquake loads. Discontinuous Deformation Analysis (DDA) has been extensively applied in the disciplines of rock mechanics and rock engineering. Two-dimensional DDA is chosen to simulate the behaviour of Candi Kelir towards earthquake load. Geometry of each block of Candi Kelir is obtained by Close Range Photogrammetry (CRP) method. Simulation of Ca

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Muhammad, D. F., A. F. Handayani, S. F. Nastiti, M. Sulthon, P. B. Susanto, and A. A. Maulidani. "Comparative study of performance between horizontal link eccentric braced frame and vertical link eccentric braced frame under earthquake load." IOP Conference Series: Earth and Environmental Science 1453, no. 1 (2025): 012011. https://doi.org/10.1088/1755-1315/1453/1/012011.

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Abstract Building designs that are earthquake-resistant are vital because Indonesia is an earthquake-prone region. The eccentrically braced frame (EBF) is one of the structural systems that may withstand earthquakes. The initial output of this system is intended to be an earthquake fuse. The main beam and EBF with horizontal linkages (EBF-H) are situated together. The main beam will spin vertically during an earthquake, which will have an impact on the building above it. There is a vertical link eccentrically braced frame (EBF-V) to alleviate this problem. EBF V is superior for post-earthquake

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Tedim, Fantina, and João Gonçalves. "Simulation of the 1755 tsunami flooding area in the Algarve (southern Portugal): the case-study of Portimão." Territorium, no. 14 (August 26, 2007): 21–31. http://dx.doi.org/10.14195/1647-7723_14_3.

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The November 1st 1755 earthquake remains the most powerful and destructive to hit Europe so far. Although frequently associated with the city of Lisbon, this earthquake caused similar or greater damage and casualties in the southwest of the Algarve, where the seismic intensity was estimated at IX-X Mercalli Intensity Scale. Some minutes later, a tsunami increased the dimension of the disaster. Using simple techniques of simulation, we estimated the potential impacts of the occurrence of a similar event to the 1755 tsunami nowadays in Portimão.

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Muntafi, Y., and N. Nojima. "The Spatio-temporal Tectonic Condition and Microzonation Map of Malang Region after the 2021 M6.1 Malang Earthquake for Disaster Risk Mitigation." IOP Conference Series: Earth and Environmental Science 933, no. 1 (2021): 012031. http://dx.doi.org/10.1088/1755-1315/933/1/012031.

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Abstract The M6.1 earthquake which hit Malang and its surroundings in 2021 resulted in fatalities and over 10,400 damaged houses. Several seismicity studies have been carried out for Malang region, but no specific studies have implied the M6.1 Malang earthquake yet. This study addresses such gap by investigating the Spatio-temporal b-value of Gutenberg-Richter Law and generating the microzonation maps of spectral acceleration by considering the effects of the M6.1 Malang earthquake. The earthquake data compiled from the national and international earthquake catalogs were homogenized into a mom

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