1980 Azores Islands earthquake
Striking the Autonomous Region of Azores on 1 January, the 1980 Azores Island earthquake killed 61 people and injured over 400, causing severe damage on the islands of Terceira and São Jorge. Measuring 6.9 on the moment magnitude scale, it also shook the islands of Pico and Faial, and resulted from a strike slip fracture, typical of other historical Azorean earthquakes.
Terceira Graciosa São Jorge | |
| UTC time | 1980-01-01 16:42:42 |
|---|---|
| ISC event | 652123 |
| USGS-ANSS | ComCat |
| Local date | January 1, 1980 |
| Local time | 15:42:42 |
| Magnitude | 6.9 Mw(ISC-GEM) |
| Depth | 10 kilometres (6 mi) |
| Epicenter | 50 km West of Angra do Heroísmo 38°49′N 27°47′W / 38.81°N 27.78°W |
| Type | Strike-slip |
| Areas affected | Portugal Azores |
| Max. intensity | VIII (Severe)–IX (Violent)[1] |
| Tsunami | A small tsunami was registered in Angra do Heroismo |
| Casualties | 61 confirmed dead, 400 injured |
In response to the earthquake, Portuguese president António Ramalho Eanes announced three days of national mourning, while relief efforts, initiated by agents of the local Air Force, were soon accompanied by government-supported agencies.
Geology Edit
Background Edit
In 1950, another strong earthquake had rocked the Azores Islands region, and this was the largest earthquake since.[2]
Description Edit
Volcanic in origin, the Azores lie in a tectonically complex area on either side of the Mid-Atlantic Ridge, between the European, American and African plate boundaries, forming their own microplate.[3] The 1980 earthquake was the result of movement along the northwest to southeast trending strike-slip fault.[3]
After aftershocks from the quake had concluded, examination took place, producing a focal solution to the small events. Movement of these shocks was similar to that of previous earthquakes around the Azores. For these earthquakes, scientists had determined that the conjugate nodal plane was responsible, seeing shearing on the right-lateral (dextral) side.[4] All faulting in this area is strike-slip-oriented, and on a rather large scale.[5] Because of this research, information now points towards Azores volcanism being controlled by earthquake movement.[4]
Damage and casualties Edit
The earthquake that struck the Azorean islands was 6.9 Mw. It caused considerable damage on three separate islands (Terceira, São Jorge Island, and Graciosa),[6] destroying several buildings.[7] According to local reports, roughly 70% of the houses on Terceira were completely demolished, including the historic quarter of the island capital, Angra do Heroísmo.[2] In general, public buildings such as churches remained intact, while several buildings caved in on themselves.[2] Public utilities such as electricity and water, were reported cut in several areas.[2]
Initially, the number of fatalities was set at 52,[7] but it was later revised to 61.[3] Additionally, the injuries were set at 300,[8] but this was also revised to more than 400.[6] At least 20,000 people were left homeless.[9] Minor damage was recorded at Pico and Faial islands.[2]
No fatalities were recorded at the Lajes Field air base, nor any major damage.[2]
Relief efforts and response Edit
United States Navy and Air Force personnel stationed at Lajes functioned as disaster relief workers,[2] sheltering as many as 150 families.[10] Portuguese Air Force members brought supplies to earthquake victims, while a Portuguese Navy João Coutinho-class corvette transported medical officials to the island. The Portuguese president, António Ramalho Eanes, flew in on a plane accompanied by medical personnel and supplies (such as bedding).[2] Local officials including policemen and volunteer firemen cleared roads for relief supplies and transports. Responding to the situation, these officials were also involved in looking for survivors in the rubble.[2] Soon after, tents were erected to replace the destroyed or unsafe homes for approximately 200 families of the islands. Portable homes were constructed by the People to People International project fund, resulting in 100 shelters.[10]
Three days of national mourning were declared by Eanes.[2] Following the relief efforts, 19 seismographic stations were installed to monitor seismic activities. Eleven of these were used to monitor earthquake activity, while the other eight also record information on the island's geothermal areas.[11]
The earthquake forced hundreds of people to leave the country for the United States. It occurred during a period of several major natural disasters in which many residents of the island left; in 1975, 8,000 residents left. In 1981, however, just 2,500 people left the island.[9]
Analysis and current situation Edit
Later studies of the events leading up to the tragedy found several factors contributing to the extent of the damage. A. Malheiro (2006) linked five major causes to damage from these earthquakes. The buildings most damaged by the earthquake were near fault lines on top of loosely packed soil. They tended to be of poor construction and did not conform to proper building code, nor had they been adequately examined.[12]
The area around the Azores remains active. Threats from earthquakes and landslides remain.[12]
See also Edit
References Edit
- Notes
- ^ "Significant Earthquake: AZORES: TERCEIRA, ANGRA DO HEROISMO". National Geophysical Data Center. January 1, 1980. Retrieved June 23, 2021.
- ^ a b c d e f g h i j Western Newspapers (2 January 1980)
- ^ a b c Borges et al. (2007), p.37–54
- ^ a b Hirn, A.; Haessler, H.; Trong, P. Hoang; Wittlinger, G.; Vcitor, L. A. Mendes (July 1980). "Aftershock sequence of the January 1, 1980, earthquake and present-day tectonics in the Azores". Geophysical Research Letters. 7 (7): 501–504. Bibcode:1980GeoRL...7..501H. doi:10.1029/GL007i007p00501.
- ^ Udías, Agustín; Buforn, Elisa (1990). "Regional stresses along the Eurasia-Africa plate boundary derived from focal mechanisms of large earthquakes". Pure and Applied Geophysics. 136 (4): 433–448. Bibcode:1991PApGe.136..433U. doi:10.1007/BF00878580. S2CID 129343125.
- ^ a b . United States Geological Survey. February 18, 2009. Archived from the original on June 1, 2008. Retrieved September 1, 2009.
- ^ a b . Los Angeles Times. January 2, 1980. Archived from the original on October 22, 2012. Retrieved September 1, 2009.
- ^ "Earthquake Kills 52 in the Azores". The New York Times. January 2, 1980. Retrieved September 1, 2009.
- ^ a b "Azores' Exiles Forsake U.S. And Go Home". The New York Times. October 3, 1982.
- ^ a b . Lajes Air Field. Archived from the original on May 7, 2008. Retrieved September 19, 2009.
- ^ Lee & Hung 2003, p. 1415.
- ^ a b Malheiro, A. (August 2006). "Geological hazards in the Azores archipelago: Volcanic terrain instability and human vulnerability". Journal of Volcanology and Geothermal Research. 156 (1–2): 158. Bibcode:2006JVGR..156..158M. doi:10.1016/j.jvolgeores.2006.03.012.
- Sources
- Lee, Kan; Hung, William (2003). International handbook of earthquake and engineering seismology, Part 2. International Association of Seismology and Physics of the Earth's Interior's.
- Silva, M (2005). Caracterização da sismicidade histórica dos Açores com base na reinterpretação de dados de macrossísmica: contribuição para avaliação do risco sísmico nas ilhas do Grupo Central (in Portuguese). Ponta Delgada: University of the Azores, Departamento de Geociências. p. 146.
- Madeira, J.; A. Ribeiro (1992). "O regime tectónico nos Açores". In C.S. Oliveira; A.R. Lucas; J.H. Guedes (eds.). Monografia 10 anos após o sismo dos Açores de 1 de Janeiro de 1980 (in Portuguese). Vol. 1. Secretaria Regional da Habitação e Obras Públicas (Terceira); Laboratório Nacional de Engenharia Civil (Lisbon). pp. 163–174.
- CVARG (2010). . Centro de Vulcanologia e Availação de Riscos Geológicos. Archived from the original on 2012-03-05. Retrieved 2010-04-09.
- Borges, J.F.; Bezzeghoud, M.; Buforn, E.; Pro, C.; Fitas, A. (2007), "The 1980, 1997 and 1998 Azores earthquakes and some seismo-tectonic implications", Tectonophysics, 435 (1–4): 37–54, Bibcode:2007Tectp.435...37B, doi:10.1016/j.tecto.2007.01.008, hdl:10174/6383
- Udías, Agustín; Buforn, Elisa (1990). "Regional stresses along the Eurasia-Africa plate boundary derived from focal mechanisms of large earthquakes". Pure and Applied Geophysics. Birkhäuser Basel. 136 (4): 433–448. Bibcode:1991PApGe.136..433U. doi:10.1007/BF00878580. S2CID 129343125.
- "Earthquakes devastates Azores Island". Western Newspapers Inc. 2 January 1980. Retrieved 1 September 2009.
External links Edit
- The International Seismological Centre has a bibliography and/or authoritative data for this event.