Usme Fault

Usme Fault
Falla de Usme
Map showing the location of Usme Fault
Etymology Usme
Country  Colombia
Region Andean
State Cundinamarca
Cities Bogotá
Characteristics
Range Eastern Ranges, Andes
Part of Andean oblique faults
Length 64.9 km (40.3 mi)
Strike 022.7 ± 6
Dip East
Dip angle High
Displacement 1–5 mm (0.039–0.197 in)/yr
Tectonics
Plate North Andean
Status Active
Earthquakes Possibly historic
Type Oblique normal fault
Movement Dextral
Age Quaternary
Orogeny Andean

The Usme Fault (Spanish: Falla de Usme) is a dextral oblique normal fault in the department of Cundinamarca in central Colombia. The fault has a total length of 64.9 kilometres (40.3 mi) and runs along an average north-northeast to south-southwest strike of 022.7 ± 6 in the Eastern Ranges of the Colombian Andes.

Etymology

The fault is named after Usme, southern locality of the Colombian capital Bogotá.[1]

Description

The Usme Fault is located in the Eastern Ranges of the Colombian Andes, south of Bogotá and extends along the western margin of the Tunjuelo River valley.[1] The fault underlies the Sumapaz Páramo.[2] The fault displaces Cretaceous and Tertiary rocks as well as Quaternary alluvial and glacial (moraine) deposits.[1]

The fault valley shows features suggesting a half-graben with a steep slope wall on the west and low-angle slope on the east. The fault forms a steep, prominent circa 40 metres (130 ft) high east-facing scarp on Cretaceous rocks that show initial development of triangular facets. The hanging valleys have Quaternary alluvial deposits on the western uplifted block. The scarp forms the western wall of a narrow and long valley. To the south of Bogotá, it appears that Pleistocene moraines are offset as recorded by east-facing well-preserved scarps about 3 metres (9.8 ft) high.[3]

See also

References

  1. 1 2 3 Paris et al., 2000a, p.48
  2. Paris et al., 2000b
  3. Paris et al., 2000a, p.49

Bibliography

Maps

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