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词条 Guáitara Fault
释义

  1. Etymology

  2. Description

  3. See also

  4. References

      Bibliography    Maps  
{{Infobox fault
| name = Guáitara Fault
| other_name = Falla de Guáitara
| namedfor = Guáitara River
| namedby =
| yeardef =
| image =
| image_size =
| image_alt =
| image_caption =
| pushpin_map = Colombia
| pushpin_map_width =
| pushpin_map_caption =
| pushpin_map_alt =
| pushpin_relief = 1
| pushpin_map_label =
| pushpin_label_position =
| pushpin_mark =
| pushpin_mark_size =
| location =
| country = {{COL}}
| region = Andean
| state = Nariño
| cities = Ipiales
| coordinates = {{coord|00|53|50|N|77|31|54|W|display=inline,title}}
| elevation =
| elevation_m =
| elevation_ft =
| elevation_ref =
| topdepth_m =
| topdepth_ft =
| topdepth_ref =
| range = Western Ranges, Andes
| part_of = Andean strike-slip faults
| segments =
| length = {{convert|36.1|km|mi|abbr=on}}
| width =
| depth =
| strike = 044.1 ± 4
| dip = East
| dip_angle = High
| displacement = <{{convert|0.2|mm|in|abbr=on}}/yr
| plate = North Andean
| status = Inactive
| earthquakes =
| type = Strike-slip fault
| movement = Dextral
| rockunit =
| age = Quaternary
| orogeny = Andean
| volcanic_arc/belt = North Volcanic Zone
 Andean Volcanic Belt
| map_image =
| map_caption =
| embed =
}}

The Guáitara Fault ({{lang-es|Falla de Guáitara}}) is a dextral strike-slip fault in the department of Nariño in southwestern Colombia. The fault has a total length of {{convert|36.1|km|mi}} and runs along an average northeast to southwest strike of 044.1 ± 4 in the Western Ranges of the Colombian Andes.

Etymology

The fault is named after the Guáitara River in Nariño.[1]

Description

The Guáitara Fault is in the Nariño Department of southwestern Colombia, crossing the Western Ranges of the Colombian Andes and to the south of the city of Pasto. The fault offsets Neogene volcanic rocks. The fault is believed to extend south into the Republic of Ecuador and may be part of the megaregional Romeral Fault System. The fault forms well developed deep V-shaped valleys, linear topographic features, fault-controlled drainage, deflected streams, and elongated hills.[1]

See also

{{portal|Colombia|Earthquakes|Geology|Prehistory of South America}}
  • List of earthquakes in Colombia
  • Piedrancha Fault
  • Romeral Fault System
{{clearboth}}

References

1. ^Paris et al., 2000, p.56

Bibliography

  • {{cite LSA |last=Paris |first=Gabriel |last2=Machette |first2=Michael N. |last3=Dart |first3=Richard L. |last4=Haller |first4=Kathleen M. |year=2000a |title=Map and Database of Quaternary Faults and Folds in Colombia and its Offshore Regions |url=https://pubs.usgs.gov/of/2000/ofr-00-0284/ofr-00-0284.pdf |publisher=USGS |pages=1–66 |accessdate=2017-09-18}}

Maps

  • {{cite LSA |last=Paris |first=Gabriel |last2=Machette |first2=Michael N. |last3=Dart |first3=Richard L. |last4=Haller |first4=Kathleen M. |year=2000b |title=Map of Quaternary Faults and Folds of Colombia and Its Offshore Regions |url=https://pubs.usgs.gov/of/2000/ofr-00-0284/ofr-00-0284.plate.pdf |publisher=USGS |pages=1 |accessdate=2017-09-18}}
{{Tectonism in Colombia}}{{DEFAULTSORT:Guaitara Fault}}

4 : Seismic faults of Colombia|Strike-slip faults|Inactive faults|Geography of Nariño Department

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