Murindó Fault

06°45′55″N 76°39′12″W / 6.76528°N 76.65333°W / 6.76528; -76.65333Country ColombiaRegionPacific/ChocóStateAntioquia, ChocóCitiesDabeibaCharacteristicsRangeChocó Basin, Western Ranges, AndesPart ofAndean strike-slip faultsLength60.6 km (37.7 mi)Strike347.4 ± 6DipEastDip angleHighDisplacement0.2–1 mm (0.0079–0.0394 in)/yrTectonicsPlateNorth AndeanStatusActiveEarthquakes18 October 1992 (MW 7.3)TypeStrike-slip faultMovementSinistralAgeQuaternaryOrogenyAndean

The Murindó Fault (Spanish: Falla Murindó) is a strike-slip fault in the department of Antioquia and Chocó in northwestern Colombia. The fault has a total length of 60.6 kilometres (37.7 mi) and runs along an average north-northwest to south-southeast strike of 347.4 ± 6 in the Chocó Basin along the western edge of the Western Ranges of the Colombian Andes.

Etymology

The fault is named after Murindó.[1]

Description

The fault in the Chocó Basin extends along the western slope of the Western Ranges of the Colombian Andes, from the Arquia River in the south to the Río Sucio and the basin of the Atrato River in the north. The Murindó Fault places Cretaceous volcanic (basic) rocks against Tertiary turbidites, and crosscuts Tertiary quartz-diorite and granodiorite.[1] The Murindó River flows along the Murindó Fault near Murindó.[2] The fault underlies the municipalities of Dabeiba and Frontino.[3] To the south, the fault runs parallel to the Mutatá and Encarnación Faults.[4][5]

In the southernmost part, the fault shows evidence of tectonic control of streams. It also forms aligned saddles that face toward the mountain front. The fault is active with an approximate slip rate of 0.2 to 1 millimetre (0.0079 to 0.0394 in) per year, and caused the 1992 Murindó earthquake (MW 7.3) on October 18. A foreshock of 6.7 was registered the day before. Many earthquakes that occurred since 1883 in the region are associated with the Murindó Fault.[6]

See also

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References

  1. ^ a b Paris et al., 2000, p.14
  2. ^ Plancha 113, 2007
  3. ^ Plancha 128, 2002
  4. ^ Plancha 129, 2002
  5. ^ Plancha 145, 2002
  6. ^ Paris et al., 2000, p.15

Bibliography

  • Paris, Gabriel; Michael N. Machette; Richard L. Dart, and Kathleen M. Haller. 2000. Map and Database of Quaternary Faults and Folds in Colombia and its Offshore Regions, 1–66. USGS. Accessed 2017-09-18.

Maps

  • Paris, Gabriel; Michael N. Machette; Richard L. Dart, and Kathleen M. Haller. 2000. Map of Quaternary Faults and Folds of Colombia and Its Offshore Regions, 1. USGS. Accessed 2017-09-18.
  • Cossio, Ubaldo, and Gilberto Zapata. 2007. Plancha 113 - Murindó - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
  • Cossio, Ubaldo, and Gilberto Zapata. 2002. Plancha 128 - Murrí - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
  • Londoño, Ana Cristina, and Humberto González. 2002. Plancha 129 - Cañasgordas - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
  • González, Humberto. 2002. Plancha 145 - Urrao - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.

Further reading

  • Page, W.D. 1986. Seismic geology and seismicity of Northwestern Colombia, 1–200. San Francisco, California, Woodward-Clyde Consultants Report for ISA and Integral Ltda., Medellín.
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Sources
     Paris, Gabriel; Machette, Michael N.; Dart, Richard L.; Haller, Kathleen M. (2000). Map and Database of Quaternary Faults and Folds in Colombia and its Offshore Regions (PDF). USGS. pp. 1–66. Retrieved 2017-06-20.

      Gómez Tapias, Jorge; Montes Ramírez, Nohora E.; Almanza Meléndez, María F.; Alcárcel Gutiérrez, Fernando A.; Madrid Montoya, César A.; Diederix, Hans (2015). Geological Map of Colombia. Servicio Geológico Colombiano. pp. 1–212. Retrieved 2019-10-29.

      Various authors (2014). Enciclopedia de desastres naturales históricos de Colombia (PDF). Universidad del Quindío. pp. 1–21. Retrieved 2017-06-20.
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