Costa Rica Earthquake

First Posting | Summary
Posting Date: September 5, 2012, 2:00:00 PM

According to the United States Geological Survey (USGS), at 8:42 AM local time this morning (14:42 UTC), a magnitude 7.6 earthquake struck a sparsely populated region of western Costa Rica approximately 150 km west of San José , the nation’s capital and largest city (approximate population 365,800 as of 2006). The earthquake, initially estimated at a magnitude of 7.9, struck at a depth of 40 kilometers. Though the size of the quake prompted the Pacific Tsunami Warning Center to issue a tsunami warning for the Pacific coastlines of Costa Rica, Nicaragua and Panama, as well as for locations as far away as Mexico and Chile, the Center later canceled the tsunami warning, reporting that sea level readings had not indicated a tsunami was generated. Prior to the cancellation of the warning, local police indicated that about 5,000 people (80 percent of the population) had been evacuated from coastal towns in the district west of the quake's center. Today’s earthquake was felt as far away as Managua, the capital of Nicaragua, though the USGS estimates that only about 42,000 people (those who live within approximately 75 km of the epicenter) experienced strong shaking (Modified Mercalli Index of VI or higher). A preliminary review of the event by Costa Rica's National Commission of Risk Prevention and Emergency Attention revealed some structural damage near the epicenter and minor nonstructural damage beyond, though it is early in the aftermath of the event and the damage picture is still taking shape. Two deaths and at least twenty injuries have been reported. Reported Impact In the location closest to the epicenter, the tourist beach town of Samara, reports indicate that the quake was felt “very strongly.” The owner of Samara’s Belvedere Hotel felt the hotel shake and saw countless items fell from shelves, but reported no significant damage. Local schools and businesses in Samara have closed today. Nearby, in the town of Hojancha, a city official reported that the quake knocked down several houses. Eight kilometers north of the epicenter, in the coastal town of Nosara, trees shook violently, roads cracked, and power lines toppled. In the coastal city of Puntarenas, Monsignor Sanabria Hospital suffered structural damage and was evacuated. To the north, in the province of Guanacaste, one resident reported that roof tiles were shaken off his home. Power and water were also disrupted in many locations of the province, including in the northern pacific beach town of Playas del Coco. There were also reports of damage at the province’s Hotel RIU and at Hotel Barceló Tambor Beach in Playa Tambor. Farther inland, in a town in the province of Heredia, a bridge completely collapsed during the quake. A Heredia hospital was also reported damaged. Closer to the capital, at the University of Costa Rica, a large crack was reported in the university’s electrical engineering building. All buildings at the college were temporarily closed while experts assessed the damage. In San José, where residents reported the swaying of buildings during the quake, phone lines and electricity remain disrupted. Due in part to a landslide on a main highway that connects to the capital, officials had trouble reaching San José this morning; thus, to better assess any damage to highways and structures there, they flew over San José, collecting aerial images. Reports from the Costa Rican President following meetings with the National Emergency Council and the International Committee of the Red Cross do indicate several buildings in the capital have been damaged, though the full damage picture in San José is still being revealed. Meanwhile, government buildings in the capital, including the National Assembly complex, have been evacuated. As a precaution against aftershocks—which are expected to last for several days and could exceed M 6.0—thousands of school children were sent home today. Regional Seismicity Costa Rica has considerable seismic risk. In the last 30 years, six damaging earthquakes with magnitudes greater than 6.0 have struck different regions of the country from its east to west coasts. Today’s earthquake occurred in the Middle American Trench subduction zone where the Cocos plate subducts underneath the Caribbean plate at a rate of 8.5 centimeters per year. Preliminary earthquake faulting mechanisms indicate that today’s temblor occurred along the interface of these two plates—and that it is a subduction zone thrust event. Although the plate convergence rate across the Middle American Trench is one of the fastest in the world, few earthquakes exceeding M8.0 have occurred here in known history. However, moderately large earthquakes, such as today’s event, do occur offshore of Costa Rica. Two earthquakes of approximately M7.5 occurred in Costa Rica’s southern offshore region in 1941 and 1983. More recently, in 1990, an earthquake of magnitude 7.0 occurred just south of Costa Rica’s Nicoya Peninsula, causing some damage in the province of Puntarenas. In the country’s northern offshore region, an earthquake between M7.7 and M7.9 occurred in 1950, causing damage in Costa Rica’s Central Valley and again in Puntarenas. Today’s event occurred between the epicenters of the 1950 and 1990 earthquakes, within 60 km of both, indicating that this area is quite seismically active. Exposure at Risk So far, damage reports from today’s quake have included mostly nonstructural damage, with some instances of structural damage. Costa Rica’s history of damaging earthquakes in recent years has resulted in improvements to the building code. The first edition of the modern seismic code was published in 1974 as a result of the 1972 earthquake in Managua, Nicaragua, which caused tremendous structural damage. Using new seismic information and taking into account improved building technologies, Costa Rica updated the code again in 1986. The regulations were then updated in 2002 and again in 2004, making the Costa Rican code one of the most comprehensive in the region. Today, the building code is generally well enforced in cities. However, many buildings in rural locations (like that of today’s quake) are older; they typically do not adhere to the country’s building code and are characterized by poorer seismic performance than modern buildings. Furthermore, in some cases, buildings in these areas are built of adobe block and mud wall construction, which is very vulnerable to seismic shaking. The predominant construction type for insured residential buildings in Costa Rica is masonry; many masonry homes are either reinforced or confined masonry, both of which are expected to sustain the moderate shaking generated by today’s event with little damage. (Confined masonry, in particular, performs better than plain masonry under lateral loads due to the additional stability provided by confining elements.) Masonry is also the main construction type for low-rise commercial and industrial buildings, while high-rise commercial and industrial buildings, including those in the Costa Rican capital, are generally comprised of steel and reinforced concrete. Given the remote location and the depth of today’s quake, significant structural damage, including collapse, is not expected over a widespread area. Today’s earthquake was the biggest temblor in Costa Rica since a M7.6 quake in 1991 left 47 people dead. (More recently, 40 people died in a M6.1 quake that occurred in January 2009.) Again, despite the magnitude of today’s quake, damage may not be significant given the depth of the event (over 40 kilometers), as well as the remote location in which it occurred and the sparse population it impacted. Properties within a 20 to 30 kilometer radius of the epicenter may experience damage if they are constructed of unreinforced masonry, which is typical of uninsured properties in this region. The full damage picture from this event is still taking shape. AIR continues to monitor the situation and will provide updates if warranted by events.

First Posting | Downloads
Posting Date: September 5, 2012, 2:00:00 PM