Irlanda Fault

Irlanda Fault
Irlanda Fault
Falla Irlanda
Etymology	Vereda Irlanda, Popayán
Coordinates	02°55′01″N 76°03′25″W / 2.91694°N 76.05694°W
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[edit]

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

Description[edit]

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[edit]

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]

References[edit]

^ ^a ^b Paris et al., 2000a, p.57
^ Paris, 2000b
^ Paris et al., 2000a, p.58
^ Olson et al., 1995, p.61
^ Olson et al., 1995, p.12

Bibliography[edit]

Paris, Gabriel; Michael N. Machette; Richard L. Dart, and Kathleen M. Haller. 2000a. Map and Database of Quaternary Faults and Folds in Colombia and its Offshore Regions, 1–66. USGS. Accessed 2017-09-18.
Olson, Richard Stuart; Juan Pablo Sarmiento Prieto; Omar Dário Cardona A.; María Teresa Findji; Víctor Daniel Bonilla; Gustavo Wilches Chaux, and Fernando Ramírez Gómez. 1995. El Desastre y la Reconstrucción del Páez. Desastres y Sociedad 4. 1–130. Accessed 2017-09-19.

Maps[edit]

Paris, Gabriel; Michael N. Machette; Richard L. Dart, and Kathleen M. Haller. 2000b. Map of Quaternary Faults and Folds of Colombia and Its Offshore Regions, 1. USGS. Accessed 2017-09-18.