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United States

Zona Sísmica: High North America
Total de Terremotos
2 709
Mayor Magnitud
4,9
Zona Sísmica
High

United States se encuentra en North America y tiene una clasificación de riesgo sísmico High. Se han registrado un total de 2709 terremotos en la historia sísmica del país. El mayor terremoto registrado en el país alcanzó una magnitud de 4,9. Con una población de 340 110 988 y un área terrestre de 9 525 067 km², los eventos sísmicos pueden tener implicaciones significativas para la infraestructura y la seguridad pública.

Visión General Sísmica

The United States sits astride some of the most geologically complex and hazardous terrain on Earth, exposing virtually every populated coastal and inland region to some degree of seismic risk. Three major tectonic systems dominate the picture. Along the Pacific Coast, the boundary between the North American Plate and the Pacific Plate creates the right-lateral [[fault]] system anchored by the 1,300-kilometre San Andreas Fault in California. To the north, the Cascadia [[subduction-zone]] carries the Juan de Fuca Plate beneath Oregon, Washington, and British Columbia in a slow-motion collision that builds stress toward rare but catastrophic megathrust ruptures. In the continental interior, ancient rift structures buried beneath thick sediments — most notably the New Madrid Seismic Zone in the central Mississippi Valley — remind geologists and emergency managers that seismic hazard is not confined to plate edges. Alaska occupies a separate seismic world, sitting squarely on the Pacific Ring of Fire where the Pacific Plate dives beneath North America and the Aleutian Arc curves westward for more than 3,000 kilometres. Hawaii faces a different hazard entirely, generated by hotspot volcanism rather than plate boundary friction.

The historical record of major earthquakes on United States soil is both long and sobering. The New Madrid sequence of 1811 and 1812 produced three events likely exceeding [[magnitude]] 7.5, temporarily reversing flow in the Mississippi River and ringing church bells as far away as Boston. The 1906 San Francisco earthquake (magnitude 7.9) killed between 3,000 and 6,000 people and destroyed much of the city through both shaking and subsequent fire; the [[epicenter]] lay near the offshore segment of the San Andreas Fault, which ruptured nearly 480 kilometres. Alaska delivered the second-largest earthquake ever recorded on instruments when the Good Friday earthquake struck Prince William Sound on 28 March 1964 at magnitude 9.2, generating a [[tsunami]] that killed people as far south as California and Oregon and levelling the coastal town of Valdez. The 1971 San Fernando earthquake (magnitude 6.6) prompted sweeping reforms to California's building codes after hospital collapses killed patients. The 1989 Loma Prieta earthquake (magnitude 6.9) killed 63 people during evening rush hour on the San Francisco Bay Area's infrastructure. The 1994 Northridge earthquake (magnitude 6.7) caused 57 deaths and over 20 billion dollars in damage, exposing critical weaknesses in steel-frame construction. More recently, the 2011 Virginia earthquake (magnitude 5.8) was felt by more people simultaneously than any other quake in U.S. history owing to the efficiency with which seismic waves travel through old, cold Eastern crust. Washington State faces a once-every-200-to-500-year Cascadia megathrust threat capable of producing magnitude 8.5 to 9.2 ruptures and catastrophic [[tsunami]]s along the entire Pacific Northwest coast.

The tectonic architecture of the contiguous United States reflects the assembly and subsequent deformation of the North American continent over hundreds of millions of years. The ancient Precambrian craton of the continental interior — stable basement rock more than one billion years old — forms the relatively aseismic heartland of the country. Around this stable nucleus, younger orogenic belts record successive phases of mountain building along former plate margins. The Rocky Mountains reflect Laramide-era compression; the Basin and Range province records ongoing extension as the continent is being pulled apart between the Colorado Plateau and the Sierra Nevada, producing a landscape of alternating mountain ranges and valleys riddled with normal [[fault]]s. The Pacific Plate boundary is one of the most intensively monitored [[fault]] systems in the world, tracked by the Southern California Seismic Network, the Pacific Northwest Seismic Network, and the USGS Advanced National Seismic System. The [[early-warning]] system ShakeAlert now delivers alerts ahead of damaging [[seismic-wave]]s to millions of residents in California, Oregon, and Washington, providing seconds to tens of seconds of warning before strong shaking arrives.

Terremotos Recientes

Mag Ubicación Hora
2,0 12 km WSW of Stanton, Texas 42 minutos atrás
1,7 16 km SSW of Jal, New Mexico 1 hora, 31 minutos atrás
1,5 9 km S of Westbrook, Texas 1 hora, 53 minutos atrás
1,5 13 km SSW of Jal, New Mexico 2 horas, 13 minutos atrás
1,8 13 km SSW of Jal, New Mexico 5 horas, 6 minutos atrás
1,6 13 km SSW of Jal, New Mexico 7 horas, 37 minutos atrás
1,2 20 km NW of Stanton, Texas 16 horas, 48 minutos atrás
1,1 19 km NW of Stanton, Texas 16 horas, 48 minutos atrás
1,9 14 km SSW of Jal, New Mexico 18 horas, 13 minutos atrás
2,0 13 km SSW of Jal, New Mexico 18 horas, 37 minutos atrás

Earthquakes Near Major Cities in United States

Preguntas Frecuentes

United States is located in a high seismic risk zone, meaning earthquakes are frequent and can be destructive. A total of 2,709 earthquakes have been recorded in United States's seismic history.

The largest recorded earthquake in United States had a magnitude of 4.9. Earthquakes of this size can cause significant damage depending on depth, location, and local building standards.

United States has had 2,709 recorded earthquakes. This count includes events of all magnitudes detected by seismic monitoring networks. The actual number of earthquakes may be higher, as smaller events can go undetected.

United States is classified in the "High" seismic zone, located in North America. Seismic zones indicate the relative level of earthquake hazard based on historical activity, geological conditions, and proximity to tectonic plate boundaries.

Durante un terremoto, Agáchese, Cúbrase y Sujétese. Métase debajo de un escritorio o mesa resistente, proteja su cabeza y cuello, y sujétese hasta que el temblor se detenga. Aléjese de ventanas y objetos pesados. Después del terremoto, revise si hay heridos y prepárese para réplicas.

El riesgo sísmico de un país se evalúa utilizando varios factores: proximidad a los límites de placas tectónicas, sismicidad histórica (frecuencia y magnitud de eventos pasados), condiciones geológicas, densidad de población en zonas sísmicas y aplicación de códigos de construcción. QuakeFYI asigna zonas sísmicas de 0 (sin riesgo) a 4 (muy alto) basándose en estos factores.

Una zona sísmica es un área geográfica clasificada por el nivel de peligro sísmico. La Zona 0 tiene riesgo insignificante, la Zona 1 tiene riesgo bajo, la Zona 2 tiene riesgo moderado, la Zona 3 tiene riesgo alto y la Zona 4 tiene riesgo muy alto. Estas zonas se determinan por datos históricos de terremotos, contexto tectónico y condiciones geológicas.

Los países a lo largo del Cinturón de Fuego del Pacífico experimentan la mayor cantidad de terremotos. Japón, Indonesia, Chile, Filipinas e Irán registran consistentemente la mayor actividad sísmica. Estados Unidos (especialmente Alaska y California), Turquía y México también se encuentran entre las naciones más sísmicamente activas.

La densidad de población amplifica el riesgo sísmico porque más personas e infraestructura están expuestas a posibles daños. Un terremoto de magnitud 7,0 en una ciudad densamente poblada puede causar miles de víctimas, mientras que el mismo evento en un área deshabitada puede no causar ninguna. Los códigos de construcción y la preparación para emergencias reducen enormemente el riesgo en áreas pobladas.

La densidad sísmica mide la concentración de actividad sísmica en relación con el área terrestre de un país, expresada como terremotos por cada 1.000 kilómetros cuadrados. Una alta densidad sísmica indica actividad sísmica frecuente por unidad de área, lo que ayuda a comparar el riesgo sísmico entre países de diferentes tamaños.

Métricas Sísmicas

Densidad Sísmica
0,28
terremotos por 1.000 km²
Exposición Sísmica
7,97
terremotos por millón de personas

Actividad Sísmica Cercana

Resumen Anual

Seguridad ante terremotos

United States se encuentra en una zona de alto riesgo sísmico. Se recomienda encarecidamente estar preparado para terremotos.

  • Agáchese, cúbrase y sujétese durante el temblor
  • Mantenga un kit de emergencia con agua, comida y primeros auxilios
  • Identifique lugares seguros en cada habitación, lejos de ventanas y objetos pesados
  • Conozca las rutas de evacuación por tsunami si se encuentra en una zona costera