Jump to content
 







Main menu
   


Navigation  



Main page
Contents
Current events
Random article
About Wikipedia
Contact us
Donate
 




Contribute  



Help
Learn to edit
Community portal
Recent changes
Upload file
 








Search  

































Create account

Log in
 









Create account
 Log in
 




Pages for logged out editors learn more  



Contributions
Talk
 



















Contents

   



(Top)
 


1 Etymology  





2 Description  





3 See also  





4 References  



4.1  Bibliography  



4.1.1  Maps  


















Garrapatas Fault Zone







Add links
 









Article
Talk
 

















Read
Edit
View history
 








Tools
   


Actions  



Read
Edit
View history
 




General  



What links here
Related changes
Upload file
Special pages
Permanent link
Page information
Cite this page
Get shortened URL
Download QR code
Wikidata item
 




Print/export  



Download as PDF
Printable version
 
















Appearance
   

 





Coordinates: 04°2447N 76°3006W / 4.41306°N 76.50167°W / 4.41306; -76.50167
 

From Wikipedia, the free encyclopedia
 


Garrapatas Fault
Falla de Garrapatas
Map showing the location of Garrapatas Fault
Map showing the location of Garrapatas Fault

EtymologyGarrapatas River
Coordinates04°24′47N 76°30′06W / 4.41306°N 76.50167°W / 4.41306; -76.50167
Country Colombia
RegionAndean, Pacific/Chocó
StateChocó, Valle del Cauca
Characteristics
RangeSerranía de Los Paraguas & Western Ranges, Andes
Part ofAndean oblique faults
Length138 km (86 mi)
Strike060.8 ± 14
DipNorthwest
Dip angle50
Displacement<0.2 mm (0.0079 in)/yr
Tectonics
PlateNorth Andean
StatusInactive
TypeOblique thrust fault
MovementDextral reverse
AgeQuaternary
OrogenyAndean

The Garrapatas Fault (Zone) (Spanish: (Zona de) Falla(s) de Garrapatas) is an inactive dextral oblique thrust fault in the departmentsofChocó and Valle del CaucainColombia. The fault has a total length of 138 kilometres (86 mi) and is crescent-shaped, running along an average east-northeast to west-southwest strike of 060.8 ± 14 in the Western Ranges of the Colombian Andes.

Etymology[edit]

The fault is named after the Garrapatas River.[1]

Description[edit]

The Garrapatas Fault runs between the axis of the Western Ranges of the Colombian Andes and the Serranía de Los Paraguas, to the west of the city of Buga. The fault displaces oceanic volcanic and sedimentary rocks and has a very well developed V-shaped valley along the upper parts of the Garrapatas and Las Vueltas Rivers and probably connects with the Argelia Fault. It causes alignment of drainage and parallel streams. Dextral movement in this fault is an exception to the common sinistral (left-lateral) movement of north–south trending faults in the region.[1]

See also[edit]

  • Earth sciences portal
  • iconGeology portal
  • References[edit]

    1. ^ a b Paris et al., 2000, p.52

    Bibliography[edit]

    Maps[edit]


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Garrapatas_Fault_Zone&oldid=1233528289"

    Categories: 
    Seismic faults of Colombia
    Thrust faults
    Strike-slip faults
    Inactive faults
    Geography of Chocó Department
    Geography of Valle del Cauca Department
    Hidden categories: 
    Pages using gadget WikiMiniAtlas
    Coordinates on Wikidata
    Articles containing Spanish-language text
     



    This page was last edited on 9 July 2024, at 15:15 (UTC).

    Text is available under the Creative Commons Attribution-ShareAlike License 4.0; additional terms may apply. By using this site, you agree to the Terms of Use and Privacy Policy. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc., a non-profit organization.



    Privacy policy

    About Wikipedia

    Disclaimers

    Contact Wikipedia

    Code of Conduct

    Developers

    Statistics

    Cookie statement

    Mobile view



    Wikimedia Foundation
    Powered by MediaWiki