PhotosLocation


Oca-Ancón_Fault_System Latitude and Longitude:

11°00′N 71°45′W / 11.000°N 71.750°W / 11.000; -71.750
From Wikipedia, the free encyclopedia
Oca-Ancón Fault
Falla Oca-Ancón
Map showing the location of Oca-Ancón Fault
Map showing the location of Oca-Ancón Fault
Location of the fault in Venezuela
Topographic map of northern Colombia showing the Oca Fault segment
LocationNorthern South America
Coordinates 11°00′N 71°45′W / 11.000°N 71.750°W / 11.000; -71.750
Country  Colombia
  Venezuela
Region Caribbean
State La Guajira
Falcón, Zulia
Cities Maracaibo
Characteristics
Range Sierra Nevada de Santa Marta, Serranía del Perijá, Venezuelan Coastal Range
Part ofAndean faults
SegmentsOca, Ancón
Length830 km (520 mi)
Strike275 ± 7 (W-E)
Dip angleVertical to subvertical
Displacement0.2–2 mm (0.0079–0.0787 in)/yr
Tectonics
Plate South American
Status Active
Earthquakes 1834
Type Strike-slip fault
MovementDextral
Age Late Pleistocene- Holocene
Orogeny Andean

The Oca-Ancón Fault System ( Spanish: Falla Oca-Ancón) is a complex of geological faults located in northeastern Colombia and northwestern Venezuela near the Caribbean Sea. The fault system is of right-lateral strike-slip type and extends for an approximate length of 830 km (520 mi). [1] [2] [3] The Oca-Ancón Fault System is part of the diffuse boundary between the Caribbean Plate and the South American Plate. [4] The movement rate of the Oca-Ancón Fault System is estimated at 2 millimetres (0.079 in) each year, more than most Venezuelan faults. [2]

Oca Fault segment

The vertical to subvertical Oca Fault segment in the western part of the fault system has a length of 265 kilometres (165 mi), running west–east through La Guajira, Colombia. It forms the northern boundary of the Sierra Nevada de Santa Marta and cuts through the Serranía del Perijá continuing into Venezuela. The fault segment with a slip rate of 0.2 to 0.8 millimetres (0.0079 to 0.0315 in) per year has been active since the Late Pleistocene (~15,000 years ago) and its most recent activity has been registered in 1834. [1]

References

  1. ^ a b Paris et al., 2000, p.9
  2. ^ a b Audemard et al, 2006
  3. ^ Audemard et al., 1996a
  4. ^ Audemard et al., 1996b

Bibliography