1995 Guerrero earthquake

Last updated
1995 Guerrero earthquake
Mexico relief location map.jpg
Bullseye1.png
UTC  time1995-09-14 14:04:31
ISC  event 84239
USGS-ANSS ComCat
Local dateSeptember 14, 1995
Local time08:04
Magnitude7.4 Mw
Depth23 km
Epicenter 16°46′44″N98°35′49″W / 16.779°N 98.597°W / 16.779; -98.597
Areas affectedMexico
Max. intensity VII (Very strong)
Casualties3 killed

The 1995 Guerrero earthquake occurred on September 14, 1995, at 14:04 UTC (08:04 local time). This earthquake had a magnitude of Mw 7.4, with the epicenter being located in the state of Guerrero, Mexico. Three people were reported dead. In the rural part of southeast Guerrero, many houses with adobe of poor quality suffered heavier damage. [1] The intensity in Copala reached MM VII. [2] The earthquake could be felt strongly along the coast from Michoacán to Chiapas. [3]

Contents

The earthquake occurred in the region of the Middle America Trench. It was an interplate earthquake. It had a reverse faulting focal mechanism. [4] [5]

See also

Related Research Articles

Body-waves consist of P-waves that are the first to arrive, or S-waves, or reflections of either. Body-waves travel through rock directly.

The 1995 Neftegorsk earthquake occurred on 28 May at 1:04 local time on northern Sakhalin Island in the Russian Far East. It was the most destructive earthquake known within the current territory of Russia, with a magnitude of Ms7.1 and maximum Mercalli intensity of IX (Violent) that devastated the oil town of Neftegorsk, where 1,989 of its 3,977 citizens were killed, and another 750 injured.

The 1995 Colima–Jalisco earthquake occurred on October 9 at 15:35 UTC with a moment magnitude of 8.0 and a maximum Mercalli intensity of VIII (Severe). The shock occurred off the coast of Jalisco, Mexico, where a tsunami was triggered that affected a 200 km (120 mi) stretch of the coast. The earthquake could be felt in Mexico City and in high-rise buildings in Dallas and Houston. In Mexico, the Cihuatlan-Manzanillo was the most severely affected area. At least 49 people died and 100 were injured.

The 1965 Oaxaca earthquake occurred in Mexico on August 23 at 13:46 with a moment magnitude of 7.5. Five people were reported dead in Mexico City and one in Oaxaca. There was an anomalous change in seismic activities before the earthquake. There was a quiescent stage from late 1963 to mid-1964, and it was followed by a renewal of seismic activities before the main shock. This earthquake was a shallow thrust earthquake in the interplate subduction zone, in which the Cocos Plate is subducting beneath the North American Plate.

The 1973 Veracruz earthquake, also known as El Terremoto de Orizaba, occurred at 3:50 a.m. local time on August 28, with the epicenter located in the vicinity of Serdán in the Mexican state of Puebla. It registered 7.1 on the moment magnitude scale and had a maximum perceived intensity of VIII (Severe) on the Mercalli intensity scale. The effects were felt in the Mexican states of Veracruz and Puebla in southeast Mexico.

The 1872 North Cascades earthquake occurred at 9:40 p.m. local time on December 14 in central Washington Territory. A maximum Mercalli intensity of VIII (Severe) was assessed for several locations, though less intense shaking was observed at many other locations in Washington, Oregon, and British Columbia. Some of these intermediate outlying areas reported V (Moderate) to VII shaking, but intensities as high as IV (Light) were reported as far distant as Idaho and Montana. Due to the remote location of the mainshock and a series of strong aftershocks, damage to structures was limited to a few cabins close to the areas of the highest intensity.

The 1968 Hyūga-nada earthquake occurred on April 1 at 09:42 local time. The earthquake had a magnitude of Mw 7.5, and the epicenter was located in Hyūga-nada Sea, off the islands of Kyushu and Shikoku, Japan. The magnitude of this earthquake was also given as MJMA 7.5. A tsunami was observed. One person was killed, and 22 people were reported injured. The intensity reached shindo 5 in Miyazaki and Kōchi.

<span class="mw-page-title-main">1994 offshore Sanriku earthquake</span> Earthquake in Japan

The 1994 offshore Sanriku earthquake occurred on December 28, 1994, at 12:19 UTC. This was a magnitude Mw 7.7 earthquake with epicenter located in the Pacific Ocean at about 180 km east of Hachinohe, Aomori. The intensity reached shindo 6 in Hachinohe, Aomori, about 187.6 km from epicenter. It could be felt in Tokyo, about 632.9 km from epicenter, with shindo 2. The Japanese Meteorological Agency put the magnitude at MJMA 7.5. Slip associated with this earthquake continued for more than a year and it has been termed an 'ultra-slow earthquake'.

The 1941 Colima earthquake occurred on April 15 at 19:09 UTC. The epicenter was located in the State of Michoacán, Mexico.

The 1911 Guerrero earthquake occurred on December 16 at 12:14 local time near the coast of Guerrero, Mexico along the Mexican subduction zone. The earthquake's energy was calculated using several different magnitude scales with an estimated moment magnitude of 7.6 and a surface wave magnitude of 7.8. Following the event, telegraphy reports came in from a broad area of Mexico. Cities from Guadalajara, Mérida, and Tapachula all reported the tremors. The earthquake lasted over two minutes and resulted in the deaths of 28 people.

The 1932 Jalisco earthquakes began on June 3 at 10:36 UTC with a megathrust event that registered 8.1 on the moment magnitude scale. With a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale, at least 400 deaths were caused in Mexico and neighboring Guatemala. It was the first of a series of seismic events that affected parts of western Mexico during the month of June 1932, all reaching magnitude 7 or greater.

The 1964 Guerrero earthquake occurred on July 6 at 01:22 local time in Guerrero, Mexico. The magnitude of this earthquake was given as Ms 7.4, or ML 7.2.

The 1968 Tokachi earthquake occurred on May 16 at 0:49 UTC in the area offshore of Aomori and Hokkaido. The magnitude of this earthquake was put at Mw 8.3. The intensity of the earthquake reached shindo 5 in Aomori, Aomori and Hakodate, Hokkaido.

The 1981 Playa Azul earthquake occurred on October 24, 1981, at 21:22 local time. It was located near Playa Azul, Michoacán, Mexico. The magnitude of the earthquake was Mw 7.2, or Ms 7.3. Three deaths were reported, two from Michoacán and one from Mexico City. Some buildings were damaged in both Michoacán and Mexico City. A small tsunami was registered in Acapulco with a maximum height of 9 cm.

The 1787 New Spain earthquake, also known as the San Sixto earthquake, occurred on 28 March at 11:30 local time. It caused a large tsunami that affected the coast of the Puebla Intendancy and the Oaxaca Intendancy in Southwestern New Spain. With an estimated magnitude of 8.6 on the moment magnitude scale, it was more powerful than any instrumentally recorded Mexican earthquake.

On January 30, at 15:01 (UTC–6), a magnitude 7.6 earthquake struck 43 km beneath the Sierra Madre del Sur range in the Mexican states of Colima, Jalisco and Michoacán. On the Mercalli intensity scale, the earthquake reached a maximum intensity of X (Extreme), causing serious damage in the region. At least 56 people were killed and about 390 were injured. The event is commonly referred to as the Colima earthquake.

The 1920 Xalapa earthquake was the deadliest earthquake in Mexico's history prior to 1985. It occurred on January 3 at 22:25 local time, killing between 648 and 4,000 people. Deadly mudflows and landslides were triggered, destroying buildings in rural towns across Veracruz and Puebla. More than 400 perished as a result of the mudflows and landslides. The earthquake was attributed to a shallow fault in the Trans-Mexican Volcanic Belt. It measured magnitude 6.3–6.4 and had a hypocenter depth of <15 km (9.3 mi). The Mexican government took immediate action in the aftermath—providing assistance and establishing communication services. The aftershocks were studied by scientists and is widely regarded as the first scientific study of aftershocks following a major earthquake.

The 1979 Petatlán earthquake, also known as the IBERO earthquake occurred on March 14 at 05:07 local time in the Mexican state of Guerrero. The earthquake had a surface wave magnitude of Ms  7.6 or moment magnitude of Mw  7.4 and maximum Modified Mercalli intensity of VIII (Severe). The epicenter, onshore, was located 12 km south southeast of Vallecitos de Zaragoza.

References

  1. "INICIO" (PDF). Archived from the original (PDF) on 2012-03-28. Retrieved 2011-07-29.
  2. Gama-García, A.; Gómez-Berna, A. Relationships between instrumental ground motion parameters, and modified Mercalli intensity in Guerrero, Mexico (PDF). The 14th World Conference on Earthquake Engineering, October 12-17, 2008. Beijing, China.
  3. "Significant Earthquakes of the World". Archived from the original on 2011-06-08. Retrieved 2010-03-13.
  4. Furumura, T.; Singh, S. K. (August 2002). "Regional Wave Propagation from Mexican Subduction Zone Earthquakes: The Attenuation Functions for Interplate and Inslab Events" (PDF). Bulletin of the Seismological Society of America. 92 (6): 2110–2125.
  5. Courboulex, F.; Santoyo, M. A.; Pacheco, J. F.; Singh, S. K. (1997), "The 14 September 1995 (M = 7.3) Copala, Mexico, earthquake: A source study using teleseismic, regional, and local data", Bulletin of the Seismological Society of America, 87 (4): 999–1010, Bibcode:1997BuSSA..87..999C, doi:10.1785/BSSA0870040999, S2CID   131652894