| 1604 Arica earthquake | |
| Pre-1900: | Yes |
| Timestamp: | 1604-11-24 18:30:00 |
| Local-Time: | 13:30 |
| Depth: | 300NaN0 |
| Location: | -18.5°N -70.4°W |
| Fault: | Peru-Chile Trench |
| Type: | Megathrust |
| Affected: | Arica, (then part of Chile), Arequipa, Peru |
| Tsunami: | Yes |
| Casualties: | 100+ |
The 1604 Arica earthquake is an earthquake that occurred at 1:30 pm on November 24, 1604, offshore Arica, Chile (formerly part of the Spanish Empire). The estimated magnitude range is and up to and . It had a destructive tsunami that destroyed moust of Southern Peru, including Arica and Arequipa. of coastline was affected by the tsunami. The recorded effects of this earthquake are very similar to those for the 1868 Arica event, suggesting a similar magnitude and rupture area of the megathrust between the subducting Nazca Plate and the overriding South American Plate. Tsunami deposits have been identified on the Chatham Islands that are likely to have been caused by a trans-Pacific tsunami caused by the 1604 earthquake.
Off the coasts of Peru and Chile, the Nazca plate subducts underneath the South American plate along the Peru-Chile Trench. At the location of the earthquake, the convergence rate between the two plates is 60NaN0/year. Large events at the plate boundary are relatively common, with similar large earthquakes occurring in 1687, 1784, 1868, and 2001. In the area of the earthquake, the Nazca Ridge functions as a semi-persistent rupture barrier. This inhibits the ability for most earthquakes to continue rupturing through this area. As a result, this earthquake cycle is considered to be bimodal, which means that the recurring earthquake is either a large (up to) or a truly giant earthquake. Only the 1604 and 1868 events are considered to have been the latter truly colossal events.
Little is known about the earthquake, but it is interpreted to be similar in size and faulting to the 1868 Arica earthquake. The cities of Arequipa, Tacna, and Moquegua experienced shaking of Modified Mercalli Intensity VIII, while Cuzco and Ica experienced VI shaking. Shaking was strongly felt in Lima. The rupture length is thought to be between NaN0NaN0 long. It is believed that the 1604 event was unable to rupture north of the Nazca Ridge, which means that only the absolute largest earthquakes (such as 1868) can pass through this semi-persistent rupture barrier.
The tsunami was widespread and impacted many countries. The tsunami, along with the 1868 event, is considered one of "the greatest historical tsunami events along the Perú-Chile Trench" and "among the greatest tsunamis ever observed in the Pacific ocean". Tsunami run-ups height were estimated to be around 16m (52feet) high. It was recorded along at least 12000NaN0 and potentially up to 28000NaN0 of coastline in South America between Lima and Concepción. Weak waves arrived in Northern Peru. At Arica, the tsunami indundated up to inland. In Oceania, the Chatham Islands have recorded what is very likely evidence of tsunami from this event as well.
Arica was destroyed and rebuilt after the earthquake, while Arequipa was so severely damaged that only the San Francisco monastery remained standing. Camaná, Moquegua, and Tacna suffered major devastation. In Pausa, a majority of houses were destroyed. In Pisco, only certain parts of the town experienced major damage. The city of Ica was slightly damaged despite being far from the rupture area. Landslides reportedly occurred between the latitudes of 15.5 and 18.5S. Other ground deformations such as cracks and liquefactions occurred as well. Damage was reported across the Pacific ocean. Overall, damages from the earthquake were comparable to the 1868 earthquake.