page_title: Bucaramanga-Santa Marta Fault
section_title: Panorama
hierarchical_section_title: Bucaramanga-Santa Marta Fault / Panorama
caption_attribution_description: English: Panorama of Floridablanca, Santander, Colombia and the Bucaramanga-Santa Marta Fault in the background.
context_page_description: The Bucaramanga-Santa Marta Fault or Bucaramanga-Santa Marta Fault System is a major oblique transpressional sinistral strike-slip fault in the departments of Magdalena, Cesar, Norte de Santander and Santander in northern Colombia. The fault system is composed of two main outcropping segments, named Santa Marta and Bucaramanga Faults, and an intermediate Algarrobo Fault segment in the subsurface. The system has a total length of 674 kilometres and runs along an average north-northwest to south-southeast strike of 341 ± 23 from the Caribbean coast west of Santa Marta to the northern area of the Eastern Ranges of the Colombian Andes.
  The fault system is a major bounding fault for various sedimentary basins and igneous and metamorphic complexes. The northern Santa Marta Fault segment separates the Sinú-San Jacinto Basin and Lower Magdalena Valley in the west from the Sierra Nevada de Santa Marta to the east. The buried Algarrobo Fault segment forms the boundary between the Lower Magdalena Valley and northern Middle Magdalena Valley to the west and the Cesar-Ranchería Basin in the east.
caption: View of the Bucaramanga section of the fault east of Floridablanca, Santander
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