El Tambor Fault

El Tambor Fault
Falla El Tambor
Map showing the location of El Tambor Fault
Etymology Cerro El Tambor
Country  Colombia
Region Pacific/Chocó
State Cauca, Valle del Cauca
Characteristics
Range Western Ranges, Andes
Part of Andean oblique faults
Length 117.5 km (73.0 mi)
Strike 026.1 ± 09
Dip East
Dip angle High
Displacement <0.2 mm (0.0079 in)/yr
Tectonics
Plate North Andean
Status Inactive
Type Oblique thrust fault
Movement Dextral reverse
Age Quaternary
Orogeny Andean

The El Tambor Fault (Spanish: Falla El Tambor) is an inactive dextral oblique thrust fault in the departments of Cauca and Valle del Cauca in Colombia. The fault has a total length of 117.5 kilometres (73.0 mi) and runs along an average northeast to southwest strike of 026.1 ± 09 to the west of the Western Ranges of the Colombian Andes.

Etymology

The fault is named after Cerro El Tambor, Timbiquí, Cauca.[1][2]

Description

The El Tambor Fault borders the western slope of the Western Ranges of the Colombian Andes, west of the Farallones de Cali.[3] Through most of its trace, the fault places Cretaceous volcanic and sedimentary rocks on the east, against Neogene rocks on the west, which commonly crops out across most of the plains of the Pacific Coast. The fault displays strong linear topographic features, tectonic control of drainage, and deflected stream channels and was active in the Late Pleistocene or Early Holocene.[4]

See also

References

  1. ↑ Mapa Geológico de Cauca, 1979
  2. ↑ Paris et al., 2000a, p.53
  3. ↑ Paris et al., 2000b
  4. ↑ Paris et al., 2000a, p.54

Bibliography

Maps

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