Coiba Plate

Coordinates: 06°41′N 80°04′W / 6.683°N 80.067°W / 6.683; -80.067
Source: Wikipedia, the free encyclopedia.
Coiba Plate
The Coiba Plate
Coiba Plate in dark red, Malpelo Plate in purple
CTF in green, PTF in red
TypeMicro
Coordinates06°41′N 80°04′W / 6.683°N 80.067°W / 6.683; -80.067
Movement1East
FeaturesBordering:
Panama Plate (north)
North Andes Plate (east)
Malpelo Plate (south)
Cocos Plate (west)
Basins:
Chocó Offshore Basin
Colombian Deep Pacific Basin
1Relative to the African Plate

The Coiba Plate is a

Serranía de Baudó, an isolated mountain chain in northwestern Chocó
, Colombia.

Description

The Coiba Plate was identified as early as 1981 by Pennington, and later in 1988 by Adamek et al.[1] It is named after Coiba, to the south of mainland Panama, bordering the plate. It was presented together with the newly defined Malpelo Plate by Tuo Zhang and lead-researcher Richard G. Gordon et al. of Rice University in a paper published in August 2017.[1] The Coiba Transform Fault (CTF) separates the Coiba Plate from the Malpelo Plate. The slab tear between the microplates could have happened during the fragmentation of the Farallon Plate, in the Oligocene, around 30 to 25 Ma.[2] The Coiba Ridge, a submerged part of the plate probably formed at the Galápagos hotspot, in contrast with the Malpelo Ridge, a product of volcanic activity.[3]

The researchers led by Gordon used a

plate boundary that runs from the Panama Transform Fault (PTF) eastward.[1]

Gallery

  • Former plate boundaries in the Pacific, offshore western South America
    Former plate boundaries in the Pacific, offshore western South America
  • Seismic activity map of Colombia
    Seismic activity map of Colombia
  • Coiba, namesake of the plate
    Coiba, namesake of the plate

References

  1. ^ a b c Zhang et al., 2017
  2. ^ Chiarabba et al., 2016, p.22
  3. ^ Meschede & Barckhausen, 2000, p.1

Bibliography

Further reading

External links