August 2018 Venezuela Earthquake

earthquakesnatural-disastersvenezuelageology
4 min read

Diosdado Cabello was mid-sentence. The president of Venezuela's Constituent National Assembly was delivering a cadena nacional -- a compulsory broadcast that preempts all other programming -- on the evening of August 21, 2018, when the ground began to move. Television cameras captured his reaction: he stopped talking, looked side to side, visibly confused. Six hundred and twenty-two kilometers to the east, just off the coast near Cariaco in Sucre state, the seafloor had ruptured at a depth of 123 kilometers. The magnitude 7.3 earthquake was the largest to strike Venezuela since the 1900 San Narciso earthquake.

Where Two Plates Grind

Venezuela's northern coast sits atop the El Pilar fault system, where the Caribbean and South American tectonic plates meet. Usually, these plates experience what geologists call horizontal differential motion -- the Caribbean plate moves eastward, the South American plate moves westward, and they catch against each other in a grinding lateral dance. But the August 2018 quake was unusual. Its depth of 123 kilometers -- the epicenter lay just east of Carupano -- indicated something different from typical strike-slip or transform faulting. A seismologist from the University of Southampton suggested the quake may have been caused by the edge of the South American plate subducting under the Lesser Antilles arc, a mechanism that experts described as exceptional. Juan Cigala of Mexico's Iquique Emergency Center called it an event that "hasn't happened before" and concluded that "the Earth is behaving in a different way."

Shockwaves Across Borders

The earthquake's reach was extraordinary. Caracas shook despite being over 600 kilometers from the epicenter, because the city sits on the San Sebastian fault -- part of the same fault system. Bogota, the Colombian capital nearly 2,000 kilometers away, felt tremors. Shaking was reported across eight Caribbean nations: Colombia, Guyana, Brazil, Grenada, Dominica, Barbados, St. Vincent and the Grenadines, St. Lucia, and Trinidad and Tobago. In Trinidad, only about 100 miles from the epicenter, the damage was tangible: power outages hit Arima and Valsayn, 218 homes were damaged, 95 schools reported impacts, and one person died of a heart attack in Arima. In Grenada, rockfalls split the ground. A seismograph at Virginia Tech, thousands of kilometers north in the United States, registered the event.

The Tower That Leaned

In Caracas, the Tower of David -- Venezuela's second-tallest building and the eleventh tallest in South America -- sustained structural damage and began leaning. The unfinished skyscraper, originally intended as a bank headquarters before it was abandoned and occupied by squatters, had already become a symbol of the country's economic unraveling. The Caracas fire service inspected it and reported no imminent risk of collapse, but a BBC Caribbean correspondent photographed the tilting structure and called it an "economic metaphor" for Venezuela. Telephone and internet services were disrupted across the capital. In Puerto Ordaz, in Bolivar state, homes and buildings cracked. Then, the next morning at 9:27 a.m., a second earthquake struck -- magnitude 5.8, centered 9 kilometers west of Yaguaraparo -- forcing the evacuation of the National Assembly in Caracas during a session discussing the detention of a political representative.

Dark Humor from the Rubble

Venezuela in August 2018 was already in freefall. Hyperinflation had obliterated the currency -- the government launched a new bolivar on the very day the earthquake struck. Social media responded with the gallows humor of people who had run out of other options. One tweet joked: "Inflation is so bad that the 7.3 magnitude earthquake has turned into 78,093.3. The strongest in history." Another noted that videos of Venezuelan supermarkets shaking were less dramatic than footage from Trinidad -- because in Venezuela, there were no products on the shelves to fall. The BBC's Venezuela correspondent observed something startling: for many people, the earthquake was actually welcome. It "had distracted them from the tough realities of everyday life." The Venezuelan government, criticized for having ambulances grounded and emergency systems unprepared, found that geology had done what politics could not -- briefly unite the country in a shared experience that, for once, was not man-made.

From the Air

The August 2018 earthquake epicenter was at approximately 10.74N, 62.91W, just off the northern coast of Venezuela near Cariaco and east of Carupano in Sucre state. The fault zone follows the coastline along the El Pilar fault system. Cumana (SVCU) is the nearest significant airport. Caracas (SVMI/Maiquetia) is 622 km to the west. The earthquake zone extends across the entire northern Venezuelan coast and was felt as far as Trinidad (TTPP) to the east.