Irlanda Fault

Irlanda Fault
Falla Irlanda
Map showing the location of Irlanda Fault
Etymology Vereda Irlanda, Popayán
Country  Colombia
Region Andean
State Cauca, Huila
Cities Popayán
Characteristics
Range Central Ranges, Andes
Part of Andean strike-slip faults
Length 54.6 km (33.9 mi)
Strike 023.9 ± 4
Dip Vertical
Dip angle 90
Displacement <0.2 mm (0.0079 in)/yr
Tectonics
Plate North Andean
Status Active
Earthquakes 1994 Páez River (Mw 6.8)
Type Strike-slip fault
Movement Dextral
Age Quaternary
Orogeny Andean

The Irlanda Fault (Spanish: Falla Irlanda) is a dextral strike-slip fault in the department of Cauca in south-central Colombia. A small portion of the fault runs through Huila. The fault has a total length of 54.6 kilometres (33.9 mi) and runs along an average northeast to southwest strike of 023 ± 4 in the Central Ranges of the Colombian Andes. The fault is active and associated with the deadly 1994 Páez River earthquake.

Etymology

The fault is named after vereda Irlanda of Popayán, Cauca.[1]

Description

The Irlanda Fault extends through the axis of the Central Ranges, east of the city of Popayán. It cuts igneous and metamorphic rocks that are capped with Quaternary volcanic ash and lapilli. The Irlanda Fault consists of two en-echelon strands. The fault trace has medium geomorphic expression and, although somewhat obscure, there are offset spurs, degraded fault scarps, broad fault valleys, saddles, aligned drainage, and deflected streams.[1] The fault runs east of the Puracé volcano and south of the Nevado del Huila.[2]

Activity

The fault has been estimated as being responsible for the 1994 Páez River earthquake, occurring on June 6, 1994.[3] The earthquake happened at a depth of 12 kilometres (39,000 ft) and had a moment magnitude of 6.8 and an intensity of VII. The earthquake destroyed the town of Páez and produced approximately 1100 fatalities.[4] The Colombian Red Cross presented a figure of 28,000 people affected by the earthquake and the resulting landslides, mudflows, avalanches and isolation due to lacking communication.[5]

See also

References

  1. 1 2 Paris et al., 2000a, p.57
  2. ↑ Paris, 2000b
  3. ↑ Paris et al., 2000a, p.58
  4. ↑ Olson et al., 1995, p.61
  5. ↑ Olson et al., 1995, p.12

Bibliography

Maps

Further reading

  • Vergara, H.; G. Paris; A. Taboada; J. Romero, and E. Castro. 1996. Actividad Neotectónica en las Fuentes Sismogénicas de la Región Central de Colombia, 1–13. Congreso Colombiano de Geología.
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