Suárez Fault

Coordinates: 06°35′48″N 73°18′16″W / 6.59667°N 73.30444°W / 6.59667; -73.30444
Source: Wikipedia, the free encyclopedia.
Suárez Fault
Falla del Suárez
Age
Quaternary
OrogenyAndean

The Suárez Fault (

strike of 021.1 ± 8 in the Eastern Ranges of the Colombian Andes from Barbosa in the south to Bucaramanga in the north, where it connects with the regional Bucaramanga-Santa Marta Fault
.

Etymology

The fault is named after the Suárez River.[1]

Description

The Suárez Fault runs from

mud flows that form the "Bucaramanga Terrace".[6] The trace of the fault is well defined, controls linear drainages such as the Suárez River for several kilometers, has sag ponds, and locally dams alluvium. The fault vertically offsets debris flows in the area of Girón and La Fuente and displaces a Tertiary erosion surface. The slip rate is estimated at 0.1 millimetres (0.0039 in) per year on the basis of displaced Quaternary deposits.[1]

See also

References

  1. ^ a b Paris et al., 2000, p.34
  2. ^ Mapa Geológico Santander, 1999
  3. ^ Plancha 170, 2009
  4. ^ Plancha 135, 2009
  5. ^ Plancha 151, 2009
  6. ^ Plancha 120, 2010

Bibliography

  • Paris, Gabriel; Michael N. Machette; Richard L. Dart, and Kathleen M. Haller. 2000a. Map and Database of Quaternary Faults and Folds in Colombia and its Offshore Regions, 1–66. USGS. Accessed 2017-09-18.

Maps

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.