Abriaquí Fault
Falla de Abriaquí
Etymology	Abriaquí
Coordinates	06°40′09″N 76°06′38″W / 6.66917°N 76.11056°W / 6.66917; -76.11056
Country	Colombia
Region	Andean
State	Antioquia
Characteristics
Range	Western Ranges, Andes
Part of	Andean oblique faults
Length	33.8 km (21.0 mi)
Strike	311 ± 2
Dip	Northeast
Dip angle	High
Displacement	0.2–1 mm (0.0079–0.0394 in)/yr
Tectonics
Plate	North Andean
Status	Inactive
Type	Oblique thrust fault
Movement	Reverse sinistral
Age	Quaternary
Orogeny	Andean

The Abriaquí Fault (Spanish: Falla de Abriaquí) is an oblique thrust fault in the department of Antioquia in northwestern Colombia. The fault has a total length of 33.8 kilometres (21.0 mi) and runs along an average northwest to southeast strike of 311 ± 2 in the Western Ranges of the Colombian Andes.

Etymology

The fault is named after Abriaquí.^[1]

Description

The Abriaquí Fault parallels the Cañasgordas Fault to the south, cutting Cretaceous oceanic volcanic rocks as well as Tertiary and Cretaceous sedimentary rocks. The fault has a well defined fault trace with scarps, saddles, and deflected streams. The slip rate is estimated at 0.2 to 1 millimetre (0.0079 to 0.0394 in) per year deduced from displaced geomorphologic features.^[1]

See also

• List of earthquakes in Colombia
• Romeral Fault System

References

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.