Bahía Solano Fault
Bahía Solano Fault | ||
---|---|---|
Falla Bahía Solano, Utría Fault, Utría-Bahía Solano Fault | ||
Age Quaternary | | |
Orogeny | Andean |
The Bahía Solano Fault (
Etymology
The fault is named after Bahía Solano, Chocó.[1]
Description
The Bahía Solano Fault extends along the Pacific Coast of Colombia, bordering the Panama, Coiba, Malpelo and North Andes Plates.[2] It bounds a structural valley between the Solano Bay and Utría Bay, and displaces the Eocene turbidites of the Uva Formation in the south,[3][4][5] and Cretaceous oceanic Baudó Basalts in the north,[6][7][8][9] The fault forms a well developed and continuous fault line (scarp),[1] and the brecciated zone of the fault reaches 5 kilometres (3.1 mi) in width.[10] The peninsulas of Cabo Corrientes and Bahía Solano are composed of oceanic crust displaced by the Bahía Solano Fault.[11]
Segments of the fault have been called Utría Fault,[4][5][7][9][11] and Utría-Bahía Solano Fault.[8]
Activity
The slip rate of the fault is estimated at between 0.2 and 1 millimetre (0.0079 and 0.0394 in) per year.
See also
References
- ^ a b c Paris et al., 2000, p.16
- ^ Zhang et al., 2017
- ^ Galvis Vergara, 1980, p.10
- ^ a b Plancha 183, 2002
- ^ a b Plancha 202, 2002
- ^ Galvis Vergara, 1980, p.23
- ^ a b Plancha 127, 2002
- ^ a b Plancha 143, 2002
- ^ a b Plancha 163, 2002
- ^ Galvis Vergara, 1980, p.31
- ^ a b Galvis Vergara, 1980, p.34
- ^ Ramírez, 1975, p.207
- ^ USGS. "M 6.5 - near the west coast of Colombia". United States Geological Survey. Retrieved 2017-09-18.
- ^ Ramírez, 1975, p.208
Bibliography
- Galvis Vergara, Jaime. 1980. Un arco de islas terciario en el occidente colombiano. Geología Colombiana 11. 7–43. Accessed 2017-09-20.
- 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.
- Ramírez, Jesús Emilio. 1975. Historia de los terremotos en Colombia, 1–250. Instituto Geográfico Agustín Codazzi.
- Zhang, Tuo; Richard G. Gordon; Jay K. Mishra, and Chengzu Wang. 2017. The Malpelo Plate Hypothesis and implications for nonclosure of the Cocos-Nazca-Pacific plate motion circuit. Geophysical Research Letters 44. 1–6. Accessed 2017-09-01.
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.
- González, Margarita, and Ubaldo Ossio. 2002. Plancha 127 - Cupica - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
- González, Margarita. 2002. Plancha 143 - Bahía Solano - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
- Zapata, Gilberto. 2002. Plancha 163 - Nuquí - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
- Zapata, Gilberto. 2002. Plancha 183 - Coquí - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
- Salazar, Gabriel. 2002. Plancha 202 - Pilizá - 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.