| Bucaramanga-Santa Marta Fault | |
| Other Name: | Bucaramanga-Santa Marta Fault System (Sistema de) Falla(s) de Bucaramanga-Santa Marta |
| Named For: | Bucaramanga, Santa Marta |
| Pushpin Map: | Colombia#Colombia Santander Department |
| Pushpin Map Caption: | Location of the fault in Colombia |
| Pushpin Relief: | 1 |
| Country: | Colombia |
| Region: | Caribbean, Andean |
| State: | Magdalena, Cesar, Norte de Santander, Santander |
| Cities: | Santa Marta, El Paso, Bucaramanga, Floridablanca, Piedecuesta |
| Coordinates: | 7.0903°N -73.0875°W |
| Elevation: | 1- |
| Range: | Sierra Nevada de Santa Marta Eastern Ranges Andes |
| Part Of: | Andean faults |
| Segments: | Santa Marta, Algarrobo, Bucaramanga Faults |
| Length: | 674km (419miles) |
| Strike: | 341 ± 23 (NNW-SSE) |
| Displacement: | 110km (70miles) |
| Plate: | South American Plate |
| Status: | Active |
| Earthquakes: | Pre-Columbian era (~1020 AD) |
| Type: | Strike-slip fault |
| Movement: | Sinistral |
| Rockunit: | Caribbean, La Guajira, Tahamí & Chibcha Terranes |
| Age: | Neogene-Holocene |
| Orogeny: | Andean |
The Bucaramanga-Santa Marta Fault (BSMF, BSF) or Bucaramanga-Santa Marta Fault System (Spanish; Castilian: (Sistema de) Falla(s) de Bucaramanga-Santa Marta) is a major oblique transpressional sinistral strike-slip fault (wrench 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 674km (419miles) 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. The Bucaramanga Fault segment separates the middle part of the Middle Magdalena Valley in the west from the Santander Massif in the east.
The fault system bounds and cuts the four largest terranes of the North Andes Plate; the La Guajira, Caribbean and Tahamí Terranes along the Santa Marta section and intraterrane movement in the Andean Chibcha Terrane. Studies of the fault segments have shown the fault was active in the pre-Columbian era, around the year 1020, when the area around Bucaramanga was inhabited by the Guane. Various seismic events analysed to have occurred during the Holocene of the Bucaramanga Fault segment lead to the conclusion the fault is active.
The Bucaramanga-Santa Marta Fault is a major fault system which extends for a total distance of 674km (419miles) from the Colombian Caribbean coast to the Eastern Ranges of the Colombian Andes to as far as about 6.5° N, south of the capital of Santander, Bucaramanga. The fault system, with an average strike of 341 ± 23 degrees, is a major wrench fault with a sinistral (left-lateral) displacement ranging from 45kmto110kmkm (28milesto70mileskm) and a fault slip rate of 0.01mm0.2mm per year.[1] The Santa Marta Fault forms the boundary between several distinct geological provinces: it is the western limit of the Santa Marta Massif with the Sinú-San Jacinto Basin, farther to the south the fault separates the Lower Magdalena Valley and northern Middle Magdalena Valley from the Cesar-Ranchería Basin. The Santander Massif is separated from the central part of the Middle Magdalena Valley along the southern Bucaramanga Fault segment of the fault system.[2]
The fault divides the northern part of the Eastern Ranges in two structurally distinct regions. The Andean uplifted eastern block mainly comprises crystalline igneous and metamorphic rocks of Paleozoic and pre-Cambrian age, with lesser amounts of Jurassic, Triassic and Tertiary sedimentary rocks. In the western downthrown block, predominately sedimentary rocks of Quaternary and Tertiary age are found, with lesser amounts of Cretaceous and Jurassic rocks. The northern half of the fault is partially covered by Quaternary deposits in the Cesar and Magdalena valleys.[2]
The fault is divided into three segments; the main Bucaramanga Fault segment in the south, the Algarrobo Fault in the central section,[3] and the main Santa Marta Fault segment in the northern part of the fault system.[4] [5] [6] Between the two main outcropping segments, the Algarrobo Fault is present in the subsurface, overlain by Quaternary sediments.[7] [8] [9] [10] [11] The urban centre of the major coal producing municipality El Paso, Cesar is located right above the fault.[9] The fault reappears at surface east of Tamalameque, Cesar, where it continues south-southeastward into the Eastern Ranges in the departments of Norte de Santander and Santander.[12] [13] [14] [15] [16] [17] The fault can be traced until San Andrés, Santander.[18] The Bucaramanga Fault possibly continues as the compressional Boyacá and Soapaga Faults on the Altiplano Cundiboyacense.[19]
| Municipality | Department | Altitude | Inhabitants | Notes |
|---|---|---|---|---|
| Santa Marta | ||||
| Magdalena | ||||
| Magdalena | ||||
| Magdalena | ||||
| Magdalena | ||||
| Magdalena | ||||
| Cesar | ||||
| Cesar | ||||
| Cesar | ||||
| Cesar | ||||
| Cesar | ||||
| Cesar | ||||
| Cesar | ||||
| Cesar | ||||
| Norte de Santander | ||||
| Cesar | ||||
| Norte de Santander | ||||
| Cesar | ||||
| Cesar | ||||
| Norte de Santander | ||||
| Norte de Santander | ||||
| Norte de Santander | ||||
| Santander | ||||
| Bucaramanga | Santander | |||
| Santander | ||||
| Santander | ||||
| Santander | ||||
| Santander | ||||
The Bucaramanga-Santa Marta Fault system is located in northwestern South America, on the North Andes Plate, where the 20mm2mm/yr east to southeastward moving Caribbean,[20] 60mm/yr eastward subducting Malpelo,[21] and South American Plates converge. Since Early Mesozoic times, the western portion of Colombia was subjected to different episodes of subduction, accretion and collision, at the boundaries of the South America continental and the oceanic Farallon, Nazca, and Caribbean Plates and various island arcs.[22] The interaction of the plate tectonic movements formed the Northern Andean Block, separated from the Maracaibo Block by the Bucaramanga-Santa Marta Fault.[23] The Northern Andean Block is subdivided into tectonic realms, with the Bucaramanga-Santa Marta Fault separating the Central Continental Sub-plate Realm in the west from the Maracaibo Sub-plate Realm in the east.[24] It has been suggested that these two realms are dominated by respectively Nazca and Caribbean Plate subduction.[25] The compressional stress regime caused the formation of the oblique sinistral Bucaramanga-Santa Marta Fault and dextral Oca and Boconó Faults.[26]
The interplay between the Santa Marta and Oca Faults produced offshore Caribbean platforms and valleys north of the Sierra Nevada de Santa Marta near Taganga.[27] Uplift along the western margin of the Santa Marta Fault probably commenced in the Pliocene.[28]
The Bucaramanga Fault intersects with the Boconó Fault at the Santander Massif.[29] In this area, the top of the subducting slab has been estimated at an initial depth of approximately 100km (100miles), then a horizontal part for about 50km (30miles), and a farther descending section to reach a depth of around 200km (100miles). The slab section, called Bucaramanga slab, here has a dip that continues to the oceanic crust of the Caribbean seafloor. Towards the north of the Bucaramanga Nest or Swarm, in a north–south area approximately 200km (100miles) in length, a well-defined Wadati-Benioff Zone extending to 175km (109miles) depth has been identified.[30]
A study published in 2009 about the Bucaramanga segment of the fault system revealed that the fault had eight episodes of activity during the late Holocene.[31] The most recent activity has been inferred to have been around the year 1020.[32] During this pre-Columbian era, the area around Bucaramanga was inhabited by the indigenous Guane. The authors consider the Bucaramanga Fault therefore as active.[31]
Other faults in the seismically active zone, named Bucaramanga Nest, produced 27 earthquakes of magnitudes 4.0 to 5.3 between May 2012 and January 2013.[33]