The Piendamó Fault () is an

oblique Oblique may refer to: * an alternative name for the character usually called a slash (punctuation) ( / ) *Oblique angle, in geometry * Oblique triangle, in geometry * Oblique lattice, in geometry * Oblique leaf base, a characteristic shape of the ...

dextral

strike-slip fault In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic ...

in the department of Cauca in southwestern

Colombia Colombia, officially the Republic of Colombia, is a country primarily located in South America with Insular region of Colombia, insular regions in North America. The Colombian mainland is bordered by the Caribbean Sea to the north, Venezuel ...

. The fault is part of the megaregional Romeral Fault System and has a total length of and runs along a variable average north to south

strike Strike may refer to: People *Strike (surname) * Hobart Huson, author of several drug related books Physical confrontation or removal *Strike (attack), attack with an inanimate object or a part of the human body intended to cause harm * Airstrike, ...

of 341.6 ± 18 in the

Central Ranges Central Ranges (code CER) is an Australian bioregion, with an area of 101,640.44 square kilometres (39,244 sq mi) spreading across two states and one territory: South Australia, Western Australia, and the Northern Territory.Andes The Andes ( ), Andes Mountains or Andean Mountain Range (; ) are the List of longest mountain chains on Earth, longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range ...

Etymology

The fault is named after Piendamó, Cauca.Paris et al., 2000a, p.23

Description

The Piendamó Fault is part of Romeral Fault System in southwestern Colombia. The fault is located at the base of the mountain front of the western slope of the Central Ranges, north of the city of

Popayán Popayán () is the capital of the Colombian department of Cauca. It is located in the Pubenza Valley in southwestern Colombia between the Western Mountain Range and Central Mountain Range. The municipality has a population of 318,059, an a ...

. The fault displaces volcanic

pyroclastic Pyroclast, Pyroclastic or Pyroclastics may refer to: Geology * Pyroclast, or airborne volcanic tephra fragments * Pyroclastic rock, rock fragments produced and ejected by explosive volcanic eruptions * Pyroclastic cone, landform of ejecta fro ...

deposits and

mud flow A mudflow, also known as mudslide or mud flow, is a form of mass wasting involving fast-moving flow of debris and dirt that has become liquified by the addition of water. Such flows can move at speeds ranging from 3 meters/minute to 5 meters/se ...

s of the

Tertiary Tertiary (from Latin, meaning 'third' or 'of the third degree/order..') may refer to: * Tertiary period, an obsolete geologic period spanning from 66 to 2.6 million years ago * Tertiary (chemistry), a term describing bonding patterns in organic ch ...

Quaternary The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS), as well as the current and most recent of the twelve periods of the ...

Popayán Formation. It forms an outstanding topographic and tectonic block bounded by two intersecting faults. The fault forms an outstanding prismatic-tectonic mountain block composed of pyroclastic flow and ash-fall deposits. This block is bounded by two well developed

fault scarp A fault scarp is a small step-like offset of the ground surface in which one side of a fault has shifted vertically in relation to the other. The topographic expression of fault scarps results from the differential erosion of rocks of contrastin ...

s of about height; one facing west-southwest and the other facing south-southwest. There is geomorphic evidence of scarp degradation and old

landslide Landslides, also known as landslips, rockslips or rockslides, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, mudflows, shallow or deep-seated slope failures and debris flows. Landslides ...

s on the face of these scarps. Deep canyons cut about into scarps formed against a flat-topped high mountain. Several close fault lines parallel the west-southwest-facing scarp. The high Piendamó scarp is one of the largest for neotectonic Quaternary faults in western Colombia.

Etymology

Description

See also

References

Bibliography

Maps

Further reading