Buesaco-Aranda Fault

Coordinates: 01°20′14.3″N 77°11′36.8″W / 1.337306°N 77.193556°W / 1.337306; -77.193556
Source: Wikipedia, the free encyclopedia.
Buesaco-Aranda Fault
Falla Buesaco-Aranda
Age
Quaternary
OrogenyAndean

The Buesaco-Aranda Fault (

strike in the Central Ranges of the Colombian Andes
. The 1995 Pasto earthquake is associated with the active fault showing high amounts of displacement. The earthquake caused seven fatalities.

Etymology

The fault is named after Buesaco and Aranda, a vereda of Pasto.[1] Other sources call the fault by the general name of Silvia-Pijao Fault.[2]

Description

The Buesaco-Aranda Fault, extends in a north-northeast to northeast direction from near the

glacial deposits.[1]

The Buesaco-Aranda Fault has a very well-defined fault trace, with strongly deformed landforms of Pleistocene-Holocene age, clear breaks in slope along eroded

alluvial deposits and in recent alluvial fans have fresh scarp morphology. The net cumulative horizontal slip calculated is 188 ± 14 metres (617 ± 46 ft), with 160 ± 10 metres (525 ± 33 ft) of displacement in offset landforms along the Aranda Fault.[1] The Morasurco volcano is enclosed by the Buesaco and Aranda Fault segments.[3]

Activity

The last strong seismic event occurred on the Buesaco Fault near Pasto at 18:23 on March 4, 1995; the magnitude of the biggest shock was M 5.0.[4] Seven people died as a result of the earthquake and the aftershocks.[5]

See also

References

  1. ^ a b c Paris et al., 2000a, p.26
  2. ^ Plancha 5-18, 2015
  3. ^ Tibaldi & Romero, 2000, p.360
  4. ^ (in Spanish) El sismo del 4 de marzo 1995, Pasto
  5. ^ (in Spanish) Siete muertos dejaron cuatro sismos en Pasto - El Tiempo

Bibliography

Maps