During April 1819, the area around Copiapó in northern Chile was struck by a sequence of earthquakes over a period of several days. The largest of these earthquakes occurred on 11 April at about 15:00 local time, with an estimated magnitude of Mw 8.5. The other two events, on 3 April between 08:00 and 09:00 local time and on 4 April at 16:00 local time, are interpreted as foreshocks to the mainshock on 11 April. The mainshock triggered a tsunami that affected 800 km of coastline and was also recorded at Hawaii. The city of Copiapó was devastated.[1]
The magnitudes of the two foreshocks is not known. The magnitude of the mainshock has been estimated to be Mw 8.5.[3] The earthquake sequence is thought to have ruptured the same part of the plate boundary as that ruptured by the 1922 Vallenar earthquake.[4]
The tsunami triggered by the 11 April mainshock affected at least 800 km of the Chilean coastline, with a maximum run-up height of 4 m and a maximum inundation of 600 m. Places affected included Huasco, Caldera, and Concepción. Caldera suffered significant damage and at Concepción the schoonerLa Fortuna broke free from its moorings. The tsunami was also recorded in the Hawaiian IslandsatHonolulu, Hilo, Kahului and Molokai. It may also have been observed at MangarevainFrench Polynesia.[5]
The earthquake sequence caused major damage in both Copiapó and Vallenar.[4] The 3 April foreshock led to widespread damage in Copiapó. The 4 April foreshock caused the collapse of several buildings in the city including a church, killing "many people".[6] The effects of the mainshock on 11 April and its associated tsunami, combined with those of the foreshocks was the complete destruction of Copiapó and Caldera.
^National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information. (1972). "Significant Earthquake Information". NOAA National Centers for Environmental Information. doi:10.7289/V5TD9V7K.
^ abBeck, S.; Barrientos, S.; Kausel, E.; Reyes, M. (1998). "Source characteristics of historic earthquakes along the central Chile subduction zone". Journal of South American Earth Sciences. 11 (2): 115–129. doi:10.1016/S0895-9811(98)00005-4.
^National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information. (1972). "Tsunami Event Information". NOAA National Centers for Environmental Information. doi:10.7289/V5TD9V7K.
^National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information. (1972). "Significant Earthquake Information (4/4/1819)". NOAA National Centers for Environmental Information. doi:10.7289/V5TD9V7K.
