1976 Guatemala earthquake

1976 Guatemala earthquake

Date February 4, 1976 (1976-02-03), 09:01:43 UTC-6
Magnitude 7.5 Mw
Depth 5 kilometres (3 mi)
Epicenter
Motagua Fault
Countries or regions  Guatemala
Max. intensity MM IX[1]
Casualties 23,000 fatalities, 76,000 injured

The 1976 Guatemala earthquake struck on February 4, 1976 at 03:01:43 local time (09:01:43 UTC-6). It was a 7.5 Mw earthquake, centered in the Motagua Fault, about 160 km northeast of Guatemala City, Guatemala. The quake's hypocenter was located at a depth of 5 km near the town of Los Amates in the department of Izabal.[1]

Cities throughout the country suffered damage, and most adobe type houses in the outlying areas of Guatemala City were completely destroyed. The earthquake struck during the early morning (at 3:01 am, local time) when most people were asleep. This contributed to the high death toll of 23,000. Approximately 76,000 were injured, and many thousands left homeless. Some of areas went without electricity and communications for days.

The main shock was followed by thousands of aftershocks, some of the larger ones causing additional damage and loss of life.[2]

Contents

Seismic data

The quake's epicentre was located near the town of Los Amates, in the eastern part of the Motagua Fault, a left-lateral strike-slip fault that forms the tectonic boundary between the North American plate and the Caribbean plate.[1] Ground shaking was felt during approximately 39 seconds, and caused visible rupturing over 230 km along the Motagua fault, while the inferred length of faulting—based on aftershock registration—was estimated at 300 km. Average horizontal displacement along the Motagua fault was 100 cm, with a maximum displacement of 326 cm.[1]

Maximum seismic intensity (MM IX) was located in the Mixco area, some sections of Guatemala City and in Gualán. A seismic intensity of MM VI covered an area of 33,000 km².[1] Liquefaction and sand boils were observed in several locations with high seismic intensity.

The main quake activated secondary fault zones, including the Mixco fault, located in a densely populated area just north-west of Guatemala City.

Several heavy aftershocks, ranging from 5.2 to 5.8 Mw caused additional casualties and hampered relief efforts.

Date Origin Time Coordinates Location Depth Magnitude
Feb. 04 1976 09.30.28.3 7 km NNE of Mixco 5 km 5.8 Mw
Feb. 06 1976 04.11.03.3 6 km SSE of San Lucas Tolimán 5 km 4.8 Mw
Feb. 06 1976 18.11.59.2 11 km ENE of Cuilapa 5 km 5.2 Mw
Feb. 06 1976 18.19.17.7 5 km ENE of San Pedro Sacatepéquez 5 km 5.8 Mw
Feb. 08 1976 08.13.51.9 13 km SE of Puerto Barrios 5 km 5.7 Mw
Feb. 09 1976 11.44.46.7 30 km WSW of Morales 5 km 5.1 Mw
Feb. 10 1976 06.17.43.0 18 km WNW of Zacapa 5 km 4.7 Mw
Mar. 07 1976 02.54.05.4 14.5 km SW of Joyabaj 5 km 4.8 Mw
Mar. 07 1976 03.15.40.3 Chinautla (9 km North of Guatemala City) 5 km 4.9 Mw
Source: Wayerly Person, William Spence, and James W. Dewey. Main event and principal aftershocks from teleseismic data. In: Guatemalan Earthquake of February 4, 1976, A Preliminary Report.

Victims and damage

The most heavily affected area covered some 30,000 km², with a population of 2.5 million. Some 23,000 people were reported dead and 77,000 wounded. Approximately 258,000 houses were destroyed, leaving about 1.2 million people homeless. 40% of the national hospital infrastructure was destroyed, while other health facilities also suffered substantial damage.[3]

International reaction

Very soon after the earthquake, the then president Kjell Eugenio Laugerud García invited most of the foreign ambassadors to tour the affected regions by helicopter, which prompted them to quickly ask for help in their home countries. For example, the United States of America rebuilt most of the roads, and the Canadians and Belgians each rebuilt a village.

See also

Notes

  1. ^ a b c d e NOAA database
  2. ^ Historic Earthquakes
  3. ^ Olcese (e.a.), 1977

References

Bates, F.L.; Killian, C.D., Daniel G.R., & Klein, R.E. (1979). "Emergency Food Programmes following the 1976 Guatemalan Earthquake: An Evaluation: Final Report". Washington: USAID. http://pdf.usaid.gov/pdf_docs/PNAAQ014.pdf. 
Bucknam, R.C.; George Plafker and R.V. Sharp (March 1978). "Fault movement (afterslip) following the Guatemala earthquake of February 4, 1976". Geology 6 (3): 170–173. doi:10.1130/0091-7613(1978)6<170:FMAFTG>2.0.CO;2. http://geology.gsapubs.org/content/6/3/170.abstract. 
Langer, C.V.; G.A. Bollinger. "Secondary faulting near the terminus of a seismogenic strike-slip fault: aftershocks of the 1976 Guatemala earthquake". Bulletin of the Seismological Society of America 69 (2): 427–444. 
Matumoto, Tosimatu; Latham, Gary V.. "Aftershocks of the Guatemalan earthquake of February 4, 1976". Geophysical Research Letters 3 (10): 599–602. Bibcode 1976GeoRL...3..599M. doi:10.1029/GL003i010p00599. 
Olcese, Orlando; Ramón Moreno and Francisco Ibarra (July 1977). "The Guatemala Earthquake Disaster of 1976: A Review of its Effects and of the contribution of the United Nations family" (pdf). UNDP, Guatemala. http://desastres.unanleon.edu.ni/pdf2/2005/septiembre-octubre/parte1/pdf/eng/doc4146/doc4146-1.pdf. 
Olson, Robert A.; Richard Stuart Olson (1977). "The Guatemala earthquake of 4 February 1976: Social science observations and research suggestions". Mass Emergencies (2): 69–81. http://www.massemergencies.org/v2n2/Olson_v2n2.pdf. 
Plafker, G. (1976). "Tectonic aspects of the Guatemala earthquake of 4 February 1976". Science 193 (4259): 1201–1208. doi:10.1126/science.193.4259.1201. PMID 17837005. 
Plafker, G.; M.G. Bonilla, and S.B. Bonis (1976). Geologic effects in the Guatemala Earthquake of February 4, 1976, a preliminary Report. Professional Paper 1002. Washington: USGS. pp. 38–51. 
USGS (May–June 1976). "Guatemalan Quake Culprit Fault Identified". Earthquake Information Bulletin (USGS) 8 (3). 
Young, Christopher J.; Thorne Lay and Christopher S. Lynnes (June 1989). "Rupture of the 4 February 1976 Guatemalan earthquake". Bulletin of the Seismological Society of America 79 (3): 670–689. 

External links