Oca-Ancón Fault System

Coordinates: 11°00′N 71°45′W / 11.000°N 71.750°W / 11.000; -71.750
Source: Wikipedia, the free encyclopedia.
Oca-Ancón Fault
Falla Oca-Ancón
Age
Late Pleistocene-Holocene
OrogenyAndean

The Oca-Ancón Fault System (

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