To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

From Wikipedia, the free encyclopedia

Murrí Fault
Falla Murrí
EtymologyMurrí River
Coordinates06°41′21″N 76°22′11″W / 6.68917°N 76.36972°W / 6.68917; -76.36972
Country Colombia
RegionAndean
StateAntioquia
Characteristics
RangeCentral Ranges, Andes
Part ofAndean oblique faults
Length87.1 km (54.1 mi)
Strike001.4 ± 5
Dipunknown
Dip angleunknown
Displacement0.2–1 mm (0.0079–0.0394 in)/yr
Tectonics
PlateNorth Andean
StatusInactive
TypeOblique thrust fault
MovementReverse sinistral
AgeQuaternary
OrogenyAndean

The Murrí Fault (Spanish: Falla Murrí) is an oblique thrust fault in the department of Antioquia in northwestern Colombia. The fault has a total length of 87.1 kilometres (54.1 mi) and runs along an average north-south strike of 001.4 ± 5 along the Central Ranges of the Colombian Andes.

Etymology

The fault is named after the Murrí River in Antioquia.[1]

Description

Located in the western limb of the Western Ranges of the Colombian Andes. The fault puts Cretaceous mafic igneous rocks to the east in contact with Tertiary marine sedimentary rocks to the west. The fault cuts mud flows dated at about 10,000 to 15,000 years. It causes strong lineaments and offsets terraces and alluvial deposits. The fault forms well-developed scarps of about 20 metres (66 ft) high on late Quaternary alluvial deposits.[1]

The fault forms the course of the Penderisco River and cuts perpendicular to the Ocaidó Valley.[2] Some authors consider the fault the southern part of the Murrí-Mutatá Fault.[3][4]

See also

References

  1. ^ a b Paris et al., 2000, p.17
  2. ^ Plancha 145, 2002
  3. ^ Plancha 129, 2002
  4. ^ González, 2001, p.183

Bibliography

Maps

Further reading

  • Page, W.D. 1986. Seismic geology and seismicity of Northwestern Colombia, 1–200. San Francisco, California, Woodward-Clyde Consultants Report for ISA and Integral Ltda., Medellín.
This page was last edited on 9 December 2020, at 16:51
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.