The 1918 San Fermín earthquake,[5][6] also known as the Puerto Rico earthquake of 1918, struck the island of Puerto Rico at 10:14:42 local time on October 11. The earthquake measured 7.1 on the moment magnitude scale and IX (Violent) on the Mercalli intensity scale. The mainshock epicenter occurred off the northwestern coast of the island, somewhere along the Puerto Rico Trench.
The earthquake triggered a tsunami that swept the west coast of the island. The combined effects of the earthquake and tsunami made it one of the worst natural disasters that have struck the island. The losses resulting from the disaster were approximately 76–118 casualties[4] and $4–29 million in property damage.
Earthquake
The epicenter of the 1918 San Fermín earthquake was located in the Mona Passage off the northwestern coast of the island. The strongest ground shaking has been estimated at intensity IX on the Mercalli intensity scale. The resulting tsunami affected primarily the west coast towns of the island (primarily Mayaguez).
Damage
Numerous structures in the west coast suffered irreparable damage. Factories and production facilities were virtually destroyed, while bridges and roads were severely damaged. The earthquake caused several mudslides in areas where the intensity exceeded Level VII, but none caused numerous deaths. Also, the river currents were affected, which, in many cases affected the foundations of many bridges, resulting in their collapse. Telegraph cables under the ocean were damaged, cutting off the island from outside communication for a time.[7]
The reported casualties of the earthquake have been estimated somewhere between 76 and 116 deaths. Approximately 40 of these deaths were caused by the tsunami which swept shore communities. Damage to property was estimated to be between $4 and 29 million.
In Aguadilla, the closest town to the earthquake epicenter, the parish church and most of the stone and concrete buildings were either destroyed or partially damaged.[8] The nearby Spanish-built Punta Higuero lighthouse of Rincón also was severely damaged.[9][10]
In Mayagüez, the largest city to be directly affected, 700 masonry buildings were damaged and 1,000 wooden houses, so many people were homeless. Major buildings like the church, post office, municipal theater and city hall were severely damaged. With fear because of the aftershocks, many people camped out in the hills for weeks.[7] Some of the buildings of the recently founded University of Puerto Rico campus were also damaged or destroyed. The Edificio José de Diego suffered structural damages and the Degetau Hall was destroyed with its main entrance portico being the only standing structure left intact.[11] These ruins were later preserved, and its portico would later on become a local landmark and the official emblem of the institution today.[12][13]
As a result of the earthquake, a tsunami lashed the west coast of the island, probably 4–7 minutes after the main shock. The highest waves were estimated at 6.0 m (19.7 ft) in Point Agujereada, 4.5 m (15 ft) at Punta Borinquen (where it destroyed the lighthouse),[23] and 5.2 m (17 ft) at Point Jiguero.[24] Several coastal villages were destroyed, and it has been estimated that 40 people drowned (32 in Aguadilla alone) as a direct result of the tsunami.[25] The earthquake and consequent tsunami destroyed most historic vernacular residences in downtown Aguadilla with only a few, such as the Amparo Roldán residence,[26] surviving. Many of the historic tombs and mausolea of the historic cemetery were also badly damaged by the waves.[27]
Aftershocks
Several aftershocks were reported immediately after the main earthquake. On October 24 and November 12, two strong aftershocks were reported on the island. However, no damage was reported as a result.
United States response
The response from the United States was to exempt the municipalities most affected from paying taxes for a short period immediately following the quake: those municipalities were Mayagüez, Aguada, Aguadilla, Añasco and Isabela. The U.S. appropriated funds for the repair of municipal buildings of the most affected municipalities.[28]
Gallery
Cathedral of Mayagüez after the first earthquake; further damage toppled the left tower
^Subcomite de la Historia de Mayagüez (1960), Historia de Mayagüez 1760–1960 (in Spanish), Talleres Graficos Interamericanos, retrieved September 7, 2010
^Álvarez Cervela, José María (1988). El Pórtico Federico Degetau en la Universidad de Puerto Rico en Mayagüez: Su Historia estética, constructiva y simbólica así como sus influencias arquitectónicas en Mayagüez. Editorial UPRM. p. 91.
^National Archives, Records of the Public Buildings Service, Record Group #121; Box #855; "Ponce, P.R., Custom House"
^Armando Morales-Pares, State Architect, and Abelardo Gonzalez-Architect, State Historic Preservation Office, 23 May 1984. In National Register of Historic Places Inventory-Nomination Form – Parque de Bombas de Ponce – (Ponce Firehouse). United States Department of the Interior. National Park Service. (Washington, D.C.) p. 3. Listing Reference Number 84003150. 12 July 1984.
^Mariano G. Coronas Castro, Certifying Official; Felix J. del Campo, State Historian; and Jorge Ortiz Colom, State Architect, Puerto Rico Historic Preservation Office. (San Juan, Puerto Rico) April 7, 1987. In National Register of Historic Places Inventory – Nomination Form. United States Department of the Interior. National Park Service. (Washington, D.C.) p. 3. Listing Reference Number 87000769. May 14, 1986.
Brink, U.; Chaytor, J.; Flores, C.; Wei, Y.; Detmer, S.; Lucas, L.; Andrews, B.; Georgiopoulou, A. (2023). "Seafloor Observations Eliminate a Landslide as the Source of the 1918 Puerto Rico Tsunami". Bulletin of the Seismological Society of America. doi:10.1785/0120220146. ISSN0037-1106.