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Remolino-El Charco Fault

From Wikipedia, the free encyclopedia

Remolino-El Charco Fault
Falla de Remolino-El Charco
EtymologyRemolino Grande & El Charco
LocationTumaco Basin
Coordinates02°11′41.9″N 78°25′57.0″W / 2.194972°N 78.432500°W / 2.194972; -78.432500
Country Colombia
RegionPacific/Chocó
StateNariño
CitiesTumaco
Characteristics
Part ofPacific strike-slip faults
Length148.7 km (92.4 mi)
Strike046.4 ± 6
DipVertical
Displacement<0.2 mm (0.0079 in)/yr
Tectonics
PlateNorth Andean
StatusInactive
TypeStrike-slip fault
MovementDextral
AgeQuaternary
OrogenyAndean

The Remolino-El Charco Fault (Spanish: Falla de Remolino-El Charco) is a dextral strike-slip fault in the department of Nariño in Colombia. The fault has a total length of 148.7 kilometres (92.4 mi) and runs along an average northeast to southwest strike of 046.4 ± 6 in the Tumaco Basin along the Pacific Coast of Colombia.

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Transcription

Etymology

The fault is named after Remolino Grande and El Charco, Nariño.[1]

Description

The Remolino-El Charco Fault extends through the Pacific coastal lowlands and plains of Colombia to the east of the city of Tumaco. The fault begins in the southwesternmost point of Colombia and runs towards Guapi.[2] It is close to and parallels the coast. It displaces alluvial fan sediments of the Patía, Mira, and Telembí Rivers and some Pleistocene marine terraces. The fault appears to be a southern continuation of the Naya-Micay Fault. The fault has a very well defined fault line on aerial photographs and satellite images. Pattern of deflection of streams suggests west side of fault is up.[1]

See also

References

  1. ^ a b Paris et al., 2000a, p.55
  2. ^ Paris et al., 2000b

Bibliography

Maps

This page was last edited on 9 December 2020, at 16:51
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