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{{short description|8.2 Mw earthquake in Chile}} | |||
{{Use mdy dates|date= |
{{Use mdy dates|date=October 2024}} | ||
{{Infobox earthquake | {{Infobox earthquake | ||
| title = 1906 |
| title = 1906 Valparaíso earthquake | ||
| timestamp = 1906-08-17 00:40:04 | | timestamp = 1906-08-17 00:40:04 | ||
| anss-url = iscgemsup16957911 | | anss-url = iscgemsup16957911 | ||
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| image alt = Damage in ] after the earthquake | | image alt = Damage in ] after the earthquake | ||
| imagecaption = Damage in ] after the earthquake | | imagecaption = Damage in ] after the earthquake | ||
| image name = |
| image name = | ||
| map2 = {{Location map | Chile |relief=1 | | map2 = {{Location map | Chile |relief=1 | ||
| label= | | label= | ||
Line 20: | Line 21: | ||
| width= 150 | | width= 150 | ||
| float=center | | float=center | ||
| caption=}} |
| caption=}} | ||
| caption = ] location | | caption = ] location | ||
| magnitude = 8.2 {{M|w|link=y}}<ref name="USGSdeaths"/> | | magnitude = 8.2 {{M|w|link=y}}<ref name="USGSdeaths"/> | ||
| intensity = {{MMI|11}}<ref name=NGDC>{{citation|title=Significant Earthquake Database|url=https://www.ngdc.noaa.gov/hazel/view/hazards/earthquake/event-more-info/2779|author=National Geophysical Data Center / World Data Service (NGDC/WDS)|publisher=], ]|doi=10.7289/V5TD9V7K|year = 1972|type = Data Set}}</ref> | |||
| intensity = | |||
| depth = {{convert|25|km|mi|0|abbr=on}} | | depth = {{convert|25|km|mi|0|abbr=on}} | ||
| location = {{coord|32|24|S|71|24|W|type:event_region:CL|display=inline,title}}<ref name=ANSS/> | | location = {{coord|32|24|S|71|24|W|type:event_region:CL|display=inline,title}}<ref name=ANSS/> | ||
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| casualties = {{formatnum:3882}} dead<ref name="USGSdeaths"/> | | casualties = {{formatnum:3882}} dead<ref name="USGSdeaths"/> | ||
}} | }} | ||
The '''1906 Valparaíso earthquake''' hit ], Chile, on August 16 at 19:55 ]. Its ] was offshore from the ], and its |
The '''1906 Valparaíso earthquake''' hit ], ], on August 16 at 19:55 ]. Its ] was offshore from the ], and its magnitude was estimated at 8.2 {{M|w|link=y}}.<ref name=ANSS>{{Cite anss|Valparaiso, Chile|1906|iscgemsup16957911|M 8.2 – Valparaiso, Chile|access-date=August 16, 2018|mode=cs1}}</ref> This earthquake occurred thirty minutes after the ]. | ||
Much of Valparaíso was destroyed; there was severe damage in ] from ] to ]. The earthquake was felt from ] |
Much of Valparaíso was destroyed; there was severe damage in ] from ] to ]. The earthquake was felt from ] to ]. Reports said the earthquake lasted four minutes. A ] was also generated. The earthquake killed a reported 3,882 people. | ||
The record of previous seismic activity includes major earthquakes in 1647, 1730 and 1822.<ref>Korrat |
The record of previous seismic activity includes major earthquakes in 1647, 1730 and 1822.<ref>{{cite book|last1=Korrat |first1=I. |first2=R. |last2=Madariaga |chapter=Rupture of the Valparaiso (Chile) Gap from 1971–1985 |chapter-url=https://books.google.com/books?id=hh1dTskgyDEC&pg=PA251 |title=Earthquake Source Mechanics |year=1986 |page=251|publisher=American Geophysical Union |isbn=9780875904054 }}</ref> The 1906 disaster was predicted by Captain Arturo Middleton, Chief of the Chilean Army Meteorological Office, in a letter that was published in '']'', one week before it occurred. | ||
Admiral Luis Gómez Carreño ordered the shooting of at least 15 people, who were caught looting after the earthquake.<ref name="latercera"/> A Board for Reconstruction was formed some weeks after the earthquake. The Seismological Service of Chile was also created. | Admiral Luis Gómez Carreño ordered the shooting of at least 15 people, who were caught looting after the earthquake.<ref name="latercera"/> A Board for Reconstruction was formed some weeks after the earthquake. The Seismological Service of Chile was also created. | ||
==Background== | ==Background== | ||
Chile lies above a ], an area where the ] under the Pacific Ocean is ] or moved beneath the ]. In the region around Valparaiso, the rate of convergence is about 70 mm/yr.<ref name="USGS1">{{cite web| |
Chile lies above a ], an area where the ] under the Pacific Ocean is ] or moved beneath the ]. In the region around Valparaiso, the rate of convergence is about 70 mm/yr.<ref name="USGS1">{{cite web|archive-url=https://web.archive.org/web/20101101123940/http://earthquake.usgs.gov/earthquakes/eqinthenews/2010/us2010tfan/ |archive-date=November 1, 2010 |url-status=dead |url=https://earthquake.usgs.gov/earthquakes/eqinthenews/2010/us2010tfan/#summary |title=Magnitude 8.8 – OFFSHORE MAULE, CHILE |publisher=United States Geological Survey |date=October 8, 2010 |access-date=October 15, 2010 }}</ref> As these two plates converge, it drives the Nazca plate with massive movements called ]. The 1906 event was one of many large ] along this plate boundary. Earthquakes can originate at the plate interface itself or within either the subducting or overriding plates.{{Citation needed|date=August 2019}} | ||
Citing the conjunction of ] with the moon,<ref>{{cite web|url= http://diario.elmercurio.com/detalle/index.asp?id={87680ded-8f54-459b-84b5-0cbfa1dc7b4d}|title=Materialismo sísmico (y 2)|work=Revista Sábado|publisher=]|date=June 5, 2010|language=Spanish| |
Citing the conjunction of ] with the moon,<ref>{{cite web|url= http://diario.elmercurio.com/detalle/index.asp?id={87680ded-8f54-459b-84b5-0cbfa1dc7b4d}|title=Materialismo sísmico (y 2)|work=Revista Sábado|publisher=]|date=June 5, 2010|language=Spanish|access-date=October 11, 2010}} {{subscription required}}</ref> Captain Arturo Middleton, Chief of the ]'s Meteorological Office, predicted the earthquake in a letter published in the Valparaíso newspaper '']'' on August 6.<ref name="mer.cl">{{cite web|url= http://www.mer.cl/modulos/generacion/mobileASP/detailNew.asp?idNoticia=C38954220100529&strNamePage=SAPRO038201005291H.SWF&codCuerpo=745&codRev=889&iNumPag=038&strFecha=2010-05-29&iPage=1&tipoPantalla= |title=Materialismo sísmico|publisher=]|work=Revista Sábado|date=May 29, 2010|language=Spanish|access-date=October 11, 2010}} {{subscription required}}</ref> Captain Middleton was severely criticized in the following days, and was described as "ignorant and obscurantist."<ref name="mer.cl"/> | ||
== |
==Earthquake characteristics== | ||
On August 16, 1906, at 19:55 local time,<ref name="mem1">{{cite web |publisher=Memoria Chilena |url=http://www.memoriachilena.cl/archivos2/pdfs/MC0000522.pdf | |
On August 16, 1906, at 19:55 local time,<ref name="mem1">{{cite web |publisher=Memoria Chilena |url=http://www.memoriachilena.cl/archivos2/pdfs/MC0000522.pdf |archive-url=https://web.archive.org/web/20120316004918/http://www.memoriachilena.cl/archivos2/pdfs/MC0000522.pdf|archive-date=March 16, 2012 |url-status=live|title=La catástrofe del 16 de agosto de 1906 en Chile |language=Spanish |access-date=February 27, 2013}}</ref> while most Chileans were dining, a subterraneous sound was heard, and before it ended, the first tremor occurred, lasting about four minutes.<ref name="USGSdeaths"/> The second tremor occurred at 20:06 and, although it lasted only two minutes, was much more violent.<ref name="mem3"/> There were numerous aftershocks: at least 56 of them occurred during the first 24 hours after the beginning tremors.<ref name="mem1"/> | ||
The magnitude of the earthquake has been estimated to be 8.4 {{M|l|link=y}}, 8.2 {{M|w|link=y}}<ref name="such">{{cite web|publisher=Servicio Sismológico de la ]| |
The magnitude of the earthquake has been estimated to be 8.4 {{M|l|link=y}}, 8.2 {{M|w|link=y}}<ref name="such">{{cite web|publisher=Servicio Sismológico de la ]|archive-url=https://web.archive.org/web/20061231163803/http://www.sismologia.cl/home/terrem.html|archive-date=December 31, 2006 |url-status=dead|url=http://www.sismologia.cl/home/terrem.html|title=SISMOS IMPORTANTES Y/O DESTRUCTIVOS (1570 – Mayo 2005)|language=Spanish|access-date=October 11, 2010}}</ref> or {{M|s|link=y}} 8.2–8.3. The energy release has been re-evaluated with an estimated ] of 2.8 x 10<sup>28</sup>, equivalent to a magnitude of 8.26 {{M|w}}. The rupture length of the earthquake has been estimated at 200 km with a ] of about 40 km.<ref name="Okal"/> The ] has been assessed using contemporary seismograph records from five stations, which were published soon after the earthquake. The data suggest that the earthquake was probably along the subduction interface. Modelling of a tsunami using these source parameters shows that this earthquake was the origin of the transpacific tsunamis recorded that same day in Hawaii and Japan, rather than the almost contemporaneous ].<ref name="Okal"/> | ||
The 30-minute time gap between the Aleutian and Chilean earthquakes is thought to be coincidental, with no causal link between the two.<ref name="Okal">{{cite journal|last=Okal|first=E.A.|year=2005|title=A re-evaluation of the great Aleutian and Chilean earthquakes of 1906 August 17|journal=]|volume=161|issue=2|pages=268–282|doi=10.1111/j.1365-246X.2005.02582.x|bibcode=2005GeoJI.161..268O}}</ref> | The 30-minute time gap between the Aleutian and Chilean earthquakes is thought to be coincidental, with no causal link between the two.<ref name="Okal">{{cite journal|last=Okal|first=E.A.|year=2005|title=A re-evaluation of the great Aleutian and Chilean earthquakes of 1906 August 17|journal=]|volume=161|issue=2|pages=268–282|doi=10.1111/j.1365-246X.2005.02582.x|bibcode=2005GeoJI.161..268O|doi-access=free}}</ref> | ||
==Damage== | ==Damage== | ||
]'' newspaper on |
]'' newspaper on August 17, 1906, reporting the earthquake of the day before]] | ||
The earthquake caused damage throughout ], from ] to ].<ref name="USGSdeaths"/> There were several destructive fires in El Almendral (from Plaza de la Victoria to Cerro Barón), Mercado Cardonal, Teatro de la Victoria (Victory Theatre), the Intendencia, the Maritime Government in ] and the Fiscal Dock at the port.<ref name="ciudad">{{cite web|publisher=Ciudad de |
The earthquake caused damage throughout ], from ] to ].<ref name="USGSdeaths"/> There were several destructive fires in El Almendral (from Plaza de la Victoria to Cerro Barón), Mercado Cardonal, Teatro de la Victoria (Victory Theatre), the Intendencia, the Maritime Government in ] and the Fiscal Dock at the port.<ref name="ciudad">{{cite web|publisher=Ciudad de Valparaíso |url=http://www.ciudaddevalparaiso.cl/inicio/patrimonio_historia_sxxi.php?id_hito=14 |title=Valparaíso: las tragedias que marcaron su identidad |language=Spanish |access-date=October 11, 2010 |archive-url=https://web.archive.org/web/20110707010634/http://www.ciudaddevalparaiso.cl/inicio/patrimonio_historia_sxxi.php?id_hito=14 |archive-date=July 7, 2011 |url-status=dead }}</ref> | ||
The earthquake was also felt in ], the capital of Chile. The newspaper ''El Mercurio'' reported in its August 17 edition that "the earthquake was produced in a violent way since its beginning, and provoked an indescribable panic through all the four thousands of inhabitants of Santiago and an unprecedented terror in the last years. Two or three-story buildings, even the most solid ones such as the National Congress, were swinging like a vessel in the sea. The shakings were so strong that many people thought the earth was going to open itself in deep and long strips."<ref name="eldia">{{cite news|work=Diario el Día|title=El terremoto del Centenario.|date=October 11, 2010}}</ref> | The earthquake was also felt in ], the capital of Chile. The newspaper ''El Mercurio'' reported in its August 17 edition that "the earthquake was produced in a violent way since its beginning, and provoked an indescribable panic through all the four thousands of inhabitants of Santiago and an unprecedented terror in the last years. Two or three-story buildings, even the most solid ones such as the National Congress, were swinging like a vessel in the sea. The shakings were so strong that many people thought the earth was going to open itself in deep and long strips."<ref name="eldia">{{cite news|work=Diario el Día|title=El terremoto del Centenario.|date=October 11, 2010}}</ref> | ||
According to the ], there were {{formatnum:3882}} deaths.<ref name="USGSdeaths">{{cite web|url=https://earthquake.usgs.gov/earthquakes/world/world_deaths.php |title=Earthquakes with 1,000 or More Deaths since 1900 |publisher= |
According to the ], there were {{formatnum:3882}} deaths.<ref name="USGSdeaths">{{cite web|url=https://earthquake.usgs.gov/earthquakes/world/world_deaths.php |title=Earthquakes with 1,000 or More Deaths since 1900 |publisher=United States Geological Survey |access-date=October 11, 2010 |archive-url=https://web.archive.org/web/20130114225331/http://earthquake.usgs.gov/earthquakes/world/world_deaths.php |archive-date=January 14, 2013 |url-status=dead }}</ref> The earthquake left more than 20,000 injured.<ref name="ciudad"/> | ||
On August 19, Admiral Luis Gómez Carreño was appointed Plaza Port Chief. Gómez ordered the distribution of water and food, removal of corpses and demolition of buildings in risk of collapse, from a tent in Plaza de La Victoria.<ref name="latercera">{{cite web|publisher=] | |
On August 19, Admiral Luis Gómez Carreño was appointed Plaza Port Chief. Gómez ordered the distribution of water and food, removal of corpses and demolition of buildings in risk of collapse, from a tent in Plaza de La Victoria.<ref name="latercera">{{cite web|publisher=] |archive-url=https://web.archive.org/web/20110723233935/http://latercera.com/contenido/1453_230311_9.shtml |archive-date=July 23, 2011 |url-status=dead |url=http://latercera.com/contenido/1453_230311_9.shtml |title=Gómez Carreño, el "sheriff" que controló Valparaíso en el sismo de 1906. |language=Spanish |access-date=October 11, 2010 }}</ref> Adm. Gómez ordered the shooting of at least 15 people who had committed crimes during the aftermath.<ref name="latercera"/> Others received public lashings for warning about another disaster or attacking the police.<ref>{{Cite journal |last=Savala |first=Joshua |title="Let Us Bring it with Love": Violence, Solidarity, and the Making of a Social Disaster in the Wake of the 1906 Earthquake in Valparaíso, Chile |url=https://doi.org/10.1093/jsh/shx021 |journal=Journal of Social History |date=2018 |volume=51 |issue=4 |pages=934–935 |doi=10.1093/jsh/shx021 |via=Project Muse}}</ref> | ||
<gallery widths=220 heights=150> | <gallery widths="220" heights="150"> | ||
Teatro de la Victoria - Valparaíso, Chile.jpg|Teatro de la Victoria before the earthquake | Teatro de la Victoria - Valparaíso, Chile.jpg|Teatro de la Victoria before the earthquake | ||
Terremoto Valparaíso 1906-Teatro de la Victoria.JPG|Teatro de la Victoria after the earthquake | Terremoto Valparaíso 1906-Teatro de la Victoria.JPG|Teatro de la Victoria after the earthquake | ||
Saqueador fusilado-Terrremoto Chile 1906.JPG|Looters shot by the authorities. | Saqueador fusilado-Terrremoto Chile 1906.JPG|Looters shot by the authorities. | ||
</gallery> | </gallery> | ||
== |
==Relief efforts== | ||
Despite the state of the city, authorities quickly organized themselves into relief groups. Firefighters from other cities of Chile, including Santiago, ] and ], moved to Valparaíso to help the local Fire Bureau.<ref name="Lajornadadelhambre">{{cite web|url=http://www.bomberil.cl/varios/viaje.htm |title=La jornada del hambre | |
Despite the state of the city, authorities quickly organized themselves into relief groups. Firefighters from other cities of Chile, including Santiago, ] and ], moved to Valparaíso to help the local Fire Bureau.<ref name="Lajornadadelhambre">{{cite web|url=http://www.bomberil.cl/varios/viaje.htm |title=La jornada del hambre |access-date=October 11, 2010 |author=Ponce, Galvarino |archive-url=https://web.archive.org/web/20110707005848/http://www.bomberil.cl/varios/viaje.htm |archive-date=July 7, 2011 |url-status=dead |language=Spanish }}</ref> Physician José Grossi worked to counteract the plagues that followed the earthquake.<ref name="mem3">{{cite web |url= http://www.memoriachilena.cl/temas/dest.asp?id=terremotosvalparaiso|archive-url=https://web.archive.org/web/20120620091642/http://www.memoriachilena.cl/temas/dest.asp?id=terremotosvalparaiso|archive-date=June 20, 2012 |url-status=live|title=Terremoto Valparaíso |publisher=Memoria Chilena |language=Spanish |access-date=October 16, 2010}}</ref><ref name="desplomo">{{cite web|url= http://diario.elmercurio.cl/detalle/index.asp?id={02794789-2639-4bee-a4c4-bb18e7c20759} |title=La noche en que Valparaíso se desplomó |date=July 30, 2006 |language=Spanish |publisher=] |access-date=October 11, 2010}} {{subscription required}}</ref> | ||
On August 25, ] ] and President-Elect ] arrived at Valparaíso. They arrived there by train, on foot, or horseback to survey the magnitude of the disaster.<ref name="eldia"/> | On August 25, ] ] and President-Elect ] arrived at Valparaíso. They arrived there by train, on foot, or horseback to survey the magnitude of the disaster.<ref name="eldia"/> | ||
Working class organizations—mutual aid societies, labor unions, and Left organizations—held fundraisers to financially support those they thought were left behind or forgotten by state efforts. Some organizations in Santiago sent money to labor groups in Valparaíso; they also helped to temporarily house working class victims from Valparaíso in Santiago.<ref>{{Cite journal |last=Savala |first=Joshua |date=2018 |title="Let Us Bring it with Love": Violence, Solidarity, and the Making of a Social Disaster in the Wake of the 1906 Earthquake in Valparaíso, Chile |url=https://doi.org/10.1093/jsh/shx021 |journal=Journal of Social History |volume=51 |issue=4 |pages=938–944 |doi=10.1093/jsh/shx021 |via=Project Muse}}</ref> | |||
Some weeks after the earthquake, a Board for Reconstruction was formed, using money received from other countries.<ref name="latercera"/> | Some weeks after the earthquake, a Board for Reconstruction was formed, using money received from other countries.<ref name="latercera"/> | ||
== Aftermath == | == Aftermath == | ||
In 1906, the Seismological Service of Chile (Servicio Sismológico de Chile) was created. Its first chief executive was ].<ref name="fernand">{{cite web|url=http://www.dgf.uchile.cl/montessus/valparaiso.html | |
In 1906, the Seismological Service of Chile (Servicio Sismológico de Chile) was created. Its first chief executive was ].<ref name="fernand">{{cite web|url=http://www.dgf.uchile.cl/montessus/valparaiso.html |archive-url=https://web.archive.org/web/20130228011026/http://www.dgf.uchile.cl/montessus/valparaiso.html |archive-date=February 28, 2013 |url-status=dead |title=Fernand de Montessus de Ballore Primer Director del Servicio Sismológico, 1908–1923 |publisher=Seismological Service of Chile |language=Spanish |year=2006 |access-date=October 11, 2010 }}</ref> | ||
The effects of this historic seismic event in the |
The effects of this historic seismic event in the Valparaíso rupture zone would be studied and measurable in the context of further seismic activity in this vicinity.<ref>Korrat, (1986). {{Google books|JBh-MocjKuEC|pp. 247–258.|page=247}}</ref> | ||
==See also== | ==See also== | ||
Line 84: | Line 88: | ||
==Notes== | ==Notes== | ||
{{reflist |
{{reflist}} | ||
==References== | ==References== | ||
* Das, Shamita; John Boatwright and C. H. Scholz. (1986). ''Earthquake Source Mechanics.'' Washington, D.C.: American Geophysical Union. {{ISBN|9780875904054}}; | * ]; John Boatwright and C. H. Scholz. (1986). ''Earthquake Source Mechanics.'' Washington, D.C.: American Geophysical Union. {{ISBN|9780875904054}}; | ||
== Further reading == | == Further reading == | ||
*{{cite book | * {{cite book | ||
|last1=Rodríguez Rozas | |last1=Rodríguez Rozas | ||
|first1=Alfredo | |first1=Alfredo | ||
Line 103: | Line 107: | ||
==External links== | ==External links== | ||
{{Commons category |
{{Commons category}} | ||
* in Valparaíso Fire Bureau's website () {{ |
* in Valparaíso Fire Bureau's website () {{in lang|es}} | ||
* {{EQ-isc-link|16957911}} | * {{EQ-isc-link|16957911}} | ||
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] | ] | ||
] | ] | ||
] | ] | ||
] | ] | ||
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Revision as of 18:28, 28 December 2024
8.2 Mw earthquake in Chile
Epicentral location | |
UTC time | 1906-08-17 00:40:04 |
---|---|
ISC event | 16957911 |
USGS-ANSS | ComCat |
Local date | August 16, 1906 (1906-08-16TUTC-4) |
Local time | 19:55 |
Magnitude | 8.2 Mw |
Depth | 25 km (16 mi) |
Epicenter | 32°24′S 71°24′W / 32.400°S 71.400°W / -32.400; -71.400 |
Areas affected | Chile |
Max. intensity | MMI XI (Extreme) |
Tsunami | Yes |
Casualties | 3,882 dead |
The 1906 Valparaíso earthquake hit Valparaíso, Chile, on August 16 at 19:55 local time. Its epicenter was offshore from the Valparaíso Region, and its magnitude was estimated at 8.2 Mw. This earthquake occurred thirty minutes after the 1906 Aleutian Islands earthquake.
Much of Valparaíso was destroyed; there was severe damage in central Chile from Illapel to Talca. The earthquake was felt from Tacna to Puerto Montt. Reports said the earthquake lasted four minutes. A tsunami was also generated. The earthquake killed a reported 3,882 people.
The record of previous seismic activity includes major earthquakes in 1647, 1730 and 1822. The 1906 disaster was predicted by Captain Arturo Middleton, Chief of the Chilean Army Meteorological Office, in a letter that was published in El Mercurio, one week before it occurred.
Admiral Luis Gómez Carreño ordered the shooting of at least 15 people, who were caught looting after the earthquake. A Board for Reconstruction was formed some weeks after the earthquake. The Seismological Service of Chile was also created.
Background
Chile lies above a convergent plate boundary, an area where the Nazca plate under the Pacific Ocean is subducted or moved beneath the South American plate. In the region around Valparaiso, the rate of convergence is about 70 mm/yr. As these two plates converge, it drives the Nazca plate with massive movements called megathrust earthquakes. The 1906 event was one of many large earthquakes in Chile along this plate boundary. Earthquakes can originate at the plate interface itself or within either the subducting or overriding plates.
Citing the conjunction of Neptune with the moon, Captain Arturo Middleton, Chief of the Chilean Army's Meteorological Office, predicted the earthquake in a letter published in the Valparaíso newspaper El Mercurio on August 6. Captain Middleton was severely criticized in the following days, and was described as "ignorant and obscurantist."
Earthquake characteristics
On August 16, 1906, at 19:55 local time, while most Chileans were dining, a subterraneous sound was heard, and before it ended, the first tremor occurred, lasting about four minutes. The second tremor occurred at 20:06 and, although it lasted only two minutes, was much more violent. There were numerous aftershocks: at least 56 of them occurred during the first 24 hours after the beginning tremors.
The magnitude of the earthquake has been estimated to be 8.4 ML, 8.2 Mw or Ms 8.2–8.3. The energy release has been re-evaluated with an estimated seismic moment of 2.8 x 10, equivalent to a magnitude of 8.26 Mw . The rupture length of the earthquake has been estimated at 200 km with a focal depth of about 40 km. The focal mechanism has been assessed using contemporary seismograph records from five stations, which were published soon after the earthquake. The data suggest that the earthquake was probably along the subduction interface. Modelling of a tsunami using these source parameters shows that this earthquake was the origin of the transpacific tsunamis recorded that same day in Hawaii and Japan, rather than the almost contemporaneous 1906 Aleutian Islands earthquake.
The 30-minute time gap between the Aleutian and Chilean earthquakes is thought to be coincidental, with no causal link between the two.
Damage
The earthquake caused damage throughout Central Chile, from Illapel to Talca. There were several destructive fires in El Almendral (from Plaza de la Victoria to Cerro Barón), Mercado Cardonal, Teatro de la Victoria (Victory Theatre), the Intendencia, the Maritime Government in Sotomayor Square and the Fiscal Dock at the port.
The earthquake was also felt in Santiago, the capital of Chile. The newspaper El Mercurio reported in its August 17 edition that "the earthquake was produced in a violent way since its beginning, and provoked an indescribable panic through all the four thousands of inhabitants of Santiago and an unprecedented terror in the last years. Two or three-story buildings, even the most solid ones such as the National Congress, were swinging like a vessel in the sea. The shakings were so strong that many people thought the earth was going to open itself in deep and long strips."
According to the University of Chile, there were 3,882 deaths. The earthquake left more than 20,000 injured.
On August 19, Admiral Luis Gómez Carreño was appointed Plaza Port Chief. Gómez ordered the distribution of water and food, removal of corpses and demolition of buildings in risk of collapse, from a tent in Plaza de La Victoria. Adm. Gómez ordered the shooting of at least 15 people who had committed crimes during the aftermath. Others received public lashings for warning about another disaster or attacking the police.
- Teatro de la Victoria before the earthquake
- Teatro de la Victoria after the earthquake
- Looters shot by the authorities.
Relief efforts
Despite the state of the city, authorities quickly organized themselves into relief groups. Firefighters from other cities of Chile, including Santiago, Concepción and Talcahuano, moved to Valparaíso to help the local Fire Bureau. Physician José Grossi worked to counteract the plagues that followed the earthquake.
On August 25, President Germán Riesco and President-Elect Pedro Montt arrived at Valparaíso. They arrived there by train, on foot, or horseback to survey the magnitude of the disaster.
Working class organizations—mutual aid societies, labor unions, and Left organizations—held fundraisers to financially support those they thought were left behind or forgotten by state efforts. Some organizations in Santiago sent money to labor groups in Valparaíso; they also helped to temporarily house working class victims from Valparaíso in Santiago.
Some weeks after the earthquake, a Board for Reconstruction was formed, using money received from other countries.
Aftermath
In 1906, the Seismological Service of Chile (Servicio Sismológico de Chile) was created. Its first chief executive was Fernand de Montessus de Ballore.
The effects of this historic seismic event in the Valparaíso rupture zone would be studied and measurable in the context of further seismic activity in this vicinity.
See also
Notes
- ^ "Earthquakes with 1,000 or More Deaths since 1900". United States Geological Survey. Archived from the original on January 14, 2013. Retrieved October 11, 2010.
- ^ ANSS. "Valparaiso, Chile 1906: M 8.2 – Valparaiso, Chile". Comprehensive Catalog. U.S. Geological Survey. Retrieved August 16, 2018.
- National Geophysical Data Center / World Data Service (NGDC/WDS) (1972), Significant Earthquake Database (Data Set), National Geophysical Data Center, NOAA, doi:10.7289/V5TD9V7K
- Korrat, I.; Madariaga, R. (1986). "Rupture of the Valparaiso (Chile) Gap from 1971–1985". Earthquake Source Mechanics. American Geophysical Union. p. 251. ISBN 9780875904054.
- ^ "Gómez Carreño, el "sheriff" que controló Valparaíso en el sismo de 1906" (in Spanish). La Tercera. Archived from the original on July 23, 2011. Retrieved October 11, 2010.
- "Magnitude 8.8 – OFFSHORE MAULE, CHILE". United States Geological Survey. October 8, 2010. Archived from the original on November 1, 2010. Retrieved October 15, 2010.
- "Materialismo sísmico (y 2)". Revista Sábado (in Spanish). El Mercurio. June 5, 2010. Retrieved October 11, 2010. (subscription required)
- ^ "Materialismo sísmico". Revista Sábado (in Spanish). El Mercurio. May 29, 2010. Retrieved October 11, 2010. (subscription required)
- ^ "La catástrofe del 16 de agosto de 1906 en Chile" (PDF) (in Spanish). Memoria Chilena. Archived (PDF) from the original on March 16, 2012. Retrieved February 27, 2013.
- ^ "Terremoto Valparaíso" (in Spanish). Memoria Chilena. Archived from the original on June 20, 2012. Retrieved October 16, 2010.
- "SISMOS IMPORTANTES Y/O DESTRUCTIVOS (1570 – Mayo 2005)" (in Spanish). Servicio Sismológico de la Universidad de Chile. Archived from the original on December 31, 2006. Retrieved October 11, 2010.
- ^ Okal, E.A. (2005). "A re-evaluation of the great Aleutian and Chilean earthquakes of 1906 August 17". Geophysical Journal International. 161 (2): 268–282. Bibcode:2005GeoJI.161..268O. doi:10.1111/j.1365-246X.2005.02582.x.
- ^ "Valparaíso: las tragedias que marcaron su identidad" (in Spanish). Ciudad de Valparaíso. Archived from the original on July 7, 2011. Retrieved October 11, 2010.
- ^ "El terremoto del Centenario". Diario el Día. October 11, 2010.
- Savala, Joshua (2018). ""Let Us Bring it with Love": Violence, Solidarity, and the Making of a Social Disaster in the Wake of the 1906 Earthquake in Valparaíso, Chile". Journal of Social History. 51 (4): 934–935. doi:10.1093/jsh/shx021 – via Project Muse.
- Ponce, Galvarino. "La jornada del hambre" (in Spanish). Archived from the original on July 7, 2011. Retrieved October 11, 2010.
- "La noche en que Valparaíso se desplomó" (in Spanish). El Mercurio. July 30, 2006. Retrieved October 11, 2010. (subscription required)
- Savala, Joshua (2018). ""Let Us Bring it with Love": Violence, Solidarity, and the Making of a Social Disaster in the Wake of the 1906 Earthquake in Valparaíso, Chile". Journal of Social History. 51 (4): 938–944. doi:10.1093/jsh/shx021 – via Project Muse.
- "Fernand de Montessus de Ballore Primer Director del Servicio Sismológico, 1908–1923" (in Spanish). Seismological Service of Chile. 2006. Archived from the original on February 28, 2013. Retrieved October 11, 2010.
- Korrat, (1986). pp. 247–258., p. 247, at Google Books
References
- Das, Shamita; John Boatwright and C. H. Scholz. (1986). Earthquake Source Mechanics. Washington, D.C.: American Geophysical Union. ISBN 9780875904054; OCLC 13526041
Further reading
- Rodríguez Rozas, Alfredo; Gajardo Cruzat, Carlos (1906). La catástrofe del 16 de agosto de 1906 en la República de Chile (in Spanish). Santiago, Chile: Imprenta y Litografía Barcelona.
External links
- Terremoto de 1906 in Valparaíso Fire Bureau's website (archive) (in Spanish)
- The International Seismological Centre has a bibliography and/or authoritative data for this event.
Earthquakes in 1900–1909 | |
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1901 | |
1902 | |
1904 |
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1905 |
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1906 |
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1908 |
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† indicates earthquake resulting in at least 30 deaths ‡ indicates the deadliest earthquake of the year |
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Historical | |
20th century | |
21st century |