Bogotá Fault
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The Bogotá Fault is a major inactive slightly dextral oblique thrust fault in the department of Cundinamarca in central Colombia. The fault has a total length of 79.3 kilometres, while other authors d
The Bogotá Fault borders the Colombian capital to the east; bottom right to top left here
Monserrate Hill was formed by the Bogotá Fault
Fault scarps at Cerro Aguanoso
Intense fracturing in the Guadalupe Group
Tunjuelo Formation
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The Tunjuelo Formation, Río Tunjuelo or Río Tunjuelito Formation is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consist
Bogotá Fault
…and Neogene Guaduas, Cacho and Bogotá Formations. Pulsations of the fault movement in the early Quaternary have produced the alluvial fans of the Tunjuelo Formation. In part, the fault is covered by Late Pleistocene deposits of the Sabana Formation showing a pre-Holocene activity with no known historical seismicity…
Paleogeography of the Pleistocene by Ron Blakey