| La Plata Fault | |
|---|---|
| Chusma Fault, Falla de La Plata, Falla de Chusma | |
  | |
| Etymology | La Plata |
| Coordinates | 02°15′42.6″N 76°00′03.2″W / 2.261833°N 76.000889°W |
| Country |  Colombia |
| Region | Andean |
| State | Huila |
| Cities | La Plata, Teruel |
| Characteristics | |
| Range | Central Ranges, Andes |
| Part of | Andean oblique faults |
| Length | 113.2 km (70.3 mi) |
| Strike | 039 ± 12 |
| Dip | West |
| Dip angle | 40-60 |
| Displacement | 0.2–1 mm (0.0079–0.0394 in)/yr |
| Tectonics | |
| Plate | North Andean |
| Status | Active |
| Earthquakes | 1967, 1996 |
| Type | Oblique thrust fault |
| Movement | Dextral reverse |
| Rock units | Honda Group |
| Age | Quaternary |
| Orogeny | Andean |
The La Plata or Chusma Fault (Spanish: Falla de La Plata, Falla de Chusma) is a dextral oblique thrust fault in the department of Huila in southwestern Colombia. The fault has a total length of 113.2 kilometres (70.3 mi) and runs along an average northeast to southwest strike of 039 ± 12 in the Central Ranges of the Colombian Andes.
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Transcription
Etymology
The fault is named after La Plata, Huila.[1]
Description
The La Plata or Chusma Fault extends across the eastern slope of the Central Ranges of the Colombian Andes, southeast of the city of Neiva in southwestern Colombia. The fault displaces Triassic, Jurassic and Cretaceous sedimentary rocks, as well as Tertiary volcanic rocks. Coalescent Quaternary alluvial fan deposits are offset by the La Plata Fault. The trace is characterised by old retreated and declined scarps, en-echelon semiparallel associated faults that cut alluvial deposits of the Páez River and local lahar deposits, a well developed topographic fault-line expression, and a probable pull-apart basin filled with Quaternary alluvial fans and alluvium near the town of La Plata. The slip rate has been estimated at 0.2 to 1 millimetre (0.0079 to 0.0394 in) per year based on geomorphologic expression.[1] Activity of the fault in 1967 and 1996 has been registered.[2]
See also
- List of earthquakes in Colombia
- Eastern Frontal Fault System
- Irlanda Fault
- La Dina Fault
- Romeral Fault System
References
- ^ a b Paris et al., 2000a, p.57
- ^ (in Spanish) La Chusma puso en alerta a Teruel - El Tiempo
Bibliography
- 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.
Maps
- 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.
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| Terranes |
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| Orogenies |
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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. | ||||||||||
This page was last edited on 9 December 2020, at 16:50