Massive earthquake M7.3 registered off the coast of Nicaragua

Massive earthquake M7.3 registered off the coast of Nicaragua

A massive earthquake measuring M7.3 on the Richter scale was registered off the coast of Nicaragua on October 14, 2014 at 03:51 UTC (21:51 local time on October 13). USGS is reporting depth of 40 km (24.9 miles). EMSC is reporting M7.3 at depth of 80 km.

INETER (Nicaragua) is reporting M7.3 at shallow depth of 24.2 km and numerous aftershocks.

Epicenter was located 67 km (42 miles) WSW of Jiquilillo, Nicaragua, 86 km (53 miles) SSW of La Union, El Salvador and 95 km (59 miles) W of Corinto, Nicaragua.

There are 960 912 people living within 100 km radius.

Local authorities have called a tsunami alert in Nicaragua and El Salvador. However, a widespread destructive tsunami threat does not exist based on historical earthquake and tsunami data.

Evacuations were ordered for at least two coastal communities in Nicaragua.

USGS issued yellow alert for shaking-related fatalities and economic losses. Some casualties and damage are possible and the impact should be relatively localized. Past yellow alerts have required a local or regional level response.

Estimated economic losses are less than 1% of GDP of Nicaragua.

Overall, the population in this region resides in structures that are vulnerable to earthquake shaking, though some resistant structures exist. The predominant vulnerable building types are unreinforced brick masonry and heavy wood frame construction.

Recent earthquakes in this area have caused secondary hazards such as tsunamis, landslides, and fires that might have contributed to losses.

The mayor of San Miguel (El Salvador), Luis Salgado, is reporting at least 1 death due to a falling lamp post.

There are reports of minor to moderate damage in some cities of El Salvador: 12 homes were damaged in La Peña de Alegria. Some walls as high as 4 meters fell in San Miguel. The National Hospital San Juan de Dios was damaged. Landslides happened in various locations. (ER)

TCS, a television network in El Salvador, said in a live broadcast Monday night that landslides had been reported. Moderate to heavy rain was falling across the country at the time of the earthquake. (TWC)

Population exposure

Population per ˜1 sq. km. from LandScan

Selected cities exposed

from GeoNames Database of Cities with 1,000 or more residents

MMI City Population
VII Jiquilillo 4k
VI Chirilagua 6k
VI Intipuca 4k
VI Puerto Morazan      8k
VI Monjaras 7k
VI El Realejo 6k
IV San Salvador 526k
IV Managua 973k
IV Tegucigalpa 851k
III San Pedro Sula 489k
III Guatemala City 995k

(k = x1,000)

Tectonic summary

The October 14, 2014 M 7.3 earthquake off the coast of El Salvador occurred as the result of normal faulting in the Central America subduction zone. The location and depth of the earthquake are consistent with its occurrence either within the subducting oceanic Cocos plate, or in the accretionary wedge of the overriding Caribbean plate, rather than on the main subduction zone thrust. At the latitude of this event, the Cocos plate is converging with the Caribbean plate at a rate of roughly 73 mm/yr in an east-northeast direction. The approximate depth of the subducted Cocos plate at the location of the earthquake is 50 km.


The portion of the Middle America subduction zone bordering El Salvador and Nicaragua, locus of the October 14 earthquake, is very seismically active, with events of M 7.3 (2012), M 7.7 (2001), M 7.7 (1992) and M 7.3 (1982) all having occurred within 200 km of the October 14 earthquake in the past 35 years. The 2001 M7.7 earthquake involved normal faulting with similar orientation to the October 14 event, and likely occurred within the subducting Cocos plate. It caused substantial damage in El Salvador and Guatemala, with the majority of fatalities caused by a triggered landslide. The 2001 earthquake also triggered aftershocks in the overriding Carribean plate, including a M 6.6 event in the vicinity of San Salvador.

Seismotectonics of the Caribbean Region and Vicinity

Extensive diversity and complexity of tectonic regimes characterizes the perimeter of the Caribbean plate, involving no fewer than four major plates (North America, South America, Nazca, and Cocos). Inclined zones of deep earthquakes (Wadati-Benioff zones), ocean trenches, and arcs of volcanoes clearly indicate subduction of oceanic lithosphere along the Central American and Atlantic Ocean margins of the Caribbean plate, while crustal seismicity in Guatemala, northern Venezuela, and the Cayman Ridge and Cayman Trench indicate transform fault and pull-apart basin tectonics.

Along the northern margin of the Caribbean plate, the North America plate moves westwards with respect to the Caribbean plate at a velocity of approximately 20 mm/yr. Motion is accommodated along several major transform faults that extend eastward from Isla de Roatan to Haiti, including the Swan Island Fault and the Oriente Fault. These faults represent the southern and northern boundaries of the Cayman Trench. Further east, from the Dominican Republic to the Island of Barbuda, relative motion between the North America plate and the Caribbean plate becomes increasingly complex and is partially accommodated by nearly arc-parallel subduction of the North America plate beneath the Caribbean plate. This results in the formation of the deep Puerto Rico Trench and a zone of intermediate focus earthquakes (70-300 km depth) within the subducted slab. Although the Puerto Rico subduction zone is thought to be capable of generating a megathrust earthquake, there have been no such events in the past century. The last probable interplate (thrust fault) event here occurred on May 2, 1787 and was widely felt throughout the island with documented destruction across the entire northern coast, including Arecibo and San Juan. Since 1900, the two largest earthquakes to occur in this region were the August 4, 1946 M8.0 Samana earthquake in northeastern Hispaniola and the July 29, 1943 M7.6 Mona Passage earthquake, both of which were shallow thrust fault earthquakes. A significant portion of the motion between the North America plate and the Caribbean plate in this region is accommodated by a series of left-lateral strike-slip faults that bisect the island of Hispaniola, notably the Septentrional Fault in the north and the Enriquillo-Plantain Garden Fault in the south. Activity adjacent to the Enriquillo-Plantain Garden Fault system is best documented by the devastating January 12, 2010 M7.0 Haiti strike-slip earthquake, its associated aftershocks and a comparable earthquake in 1770.

Moving east and south, the plate boundary curves around Puerto Rico and the northern Lesser Antilles where the plate motion vector of the Caribbean plate relative to the North and South America plates is less oblique, resulting in active island-arc tectonics. Here, the North and South America plates subduct towards the west beneath the Caribbean plate along the Lesser Antilles Trench at rates of approximately 20 mm/yr. As a result of this subduction, there exists both intermediate focus earthquakes within the subducted plates and a chain of active volcanoes along the island arc. Although the Lesser Antilles is considered one of the most seismically active regions in the Caribbean, few of these events have been greater than M7.0 over the past century. The island of Guadeloupe was the site of one of the largest megathrust earthquakes to occur in this region on February 8, 1843, with a suggested magnitude greater than 8.0. The largest recent intermediate-depth earthquake to occur along the Lesser Antilles arc was the November 29, 2007 M7.4 Martinique earthquake northwest of Fort-De-France.

The southern Caribbean plate boundary with the South America plate strikes east-west across Trinidad and western Venezuela at a relative rate of approximately 20 mm/yr. This boundary is characterized by major transform faults, including the Central Range Fault and the Boconó-San Sebastian-El Pilar Faults, and shallow seismicity. Since 1900, the largest earthquakes to occur in this region were the October 29, 1900 M7.7 Caracas earthquake, and the July 29, 1967 M6.5 earthquake near this same region. Further to the west, a broad zone of compressive deformation trends southwestward across western Venezuela and central Columbia. The plate boundary is not well defined across northwestern South America, but deformation transitions from being dominated by Caribbean/South America convergence in the east to Nazca/South America convergence in the west. The transition zone between subduction on the eastern and western margins of the Caribbean plate is characterized by diffuse seismicity involving low- to intermediate-magnitude (M<6.0) earthquakes of shallow to intermediate depth.

The plate boundary offshore of Colombia is also characterized by convergence, where the Nazca plate subducts beneath South America towards the east at a rate of approximately 65 mm/yr. The January 31, 1906 M8.5 earthquake occurred on the shallowly dipping megathrust interface of this plate boundary segment. Along the western coast of Central America, the Cocos plate subducts towards the east beneath the Caribbean plate at the Middle America Trench. Convergence rates vary between 72-81 mm/yr, decreasing towards the north. This subduction results in relatively high rates of seismicity and a chain of numerous active volcanoes; intermediate-focus earthquakes occur within the subducted Cocos plate to depths of nearly 300 km. Since 1900, there have been many moderately sized intermediate-depth earthquakes in this region, including the September 7, 1915 M7.4 El Salvador and the October 5, 1950 M7.8 Costa Rica events.

The boundary between the Cocos and Nazca plates is characterized by a series of north-south trending transform faults and east-west trending spreading centers. The largest and most seismically active of these transform boundaries is the Panama Fracture Zone. The Panama Fracture Zone terminates in the south at the Galapagos rift zone and in the north at the Middle America trench, where it forms part of the Cocos-Nazca-Caribbean triple junction. Earthquakes along the Panama Fracture Zone are generally shallow, low- to intermediate in magnitude (M<7.2) and are characteristically right-lateral strike-slip faulting earthquakes. Since 1900, the largest earthquake to occur along the Panama Fracture Zone was the July 26, 1962 M7.2 earthquake. (USGS) More information on regional seismicity and tectonics

References for the Panama Fracture Zone: 
Molnar, P., and Sykes, L. R., 1969, Tectonics of the Caribbean and Middle America Regions from Focal Mechanisms and Seismicity: Geological Society of America Bulletin, v. 80, p. 1639-1684.

Featured image: USGS

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