Main tectonic plate boundaries – ridge (red), trench (green), fault (black) – and corresponding triple junctions (yellow dots)

A triple junction is the point where the boundaries of three tectonic plates meet. At the triple junction each of the three boundaries will be one of three types – a ridge (R), trench (T) or transform fault (F) – and triple junctions can be described according to the types of plate margin that meet at them (e.g. Fault-Fault-Trench, Ridge-Ridge-Ridge, or abbreviated F-F-T, R-R-R). Of the ten possible types of triple junctions only a few are stable through time ('stable' in this context means that the geometrical configuration of the triple junction will not change through geologic time). The meeting of four or more plates is also theoretically possible but junctions will only exist instantaneously.[1]


The first scientific paper detailing the triple junction concept was published in 1969 by Dan McKenzie and W. Jason Morgan.[2] The term had traditionally been used for the intersection of three divergent boundaries or spreading ridges. These three divergent boundaries ideally meet at near 120° angles.

In plate tectonics theory during the breakup of a continent, three divergent boundaries form, radiating out from a central point (the triple junction). One of these divergent plate boundaries fails (see aulacogen) and the other two continue spreading to form an ocean. The opening of the south Atlantic Ocean started at the south of the South American and African continents, reaching a triple junction in the present Gulf of Guinea, from where it continued to the west. The NE-trending Benue Trough is the failed arm of this junction.[3]

In the years since, the term triple-junction has come to refer to any point where three tectonic plates meet.


The properties of triple junctions are most easily understood from the purely kinematic point of view where the plates are rigid and moving over the surface of the Earth. No knowledge of the Earth's interior or the geological details of the crust are then needed. Another useful simplification is that the kinematics of triple junctions on a flat Earth are essentially the same as those on the surface of a sphere. On a sphere, plate motions are described as relative rotations about Euler Poles (see Plate reconstruction), and the relative motion at every point along a plate boundary can be calculated from this rotation. But the area around a triple junction is small enough (relative to the size of the sphere) and (usually) far enough from the pole of rotation, that the relative motion across a boundary can be assumed to be constant along that boundary. Thus, analysis of triple junctions can usually be done on a flat surface with motions defined by vectors.


Triple junctions may be described and their stability assessed without use of the geological details but simply by defining the properties of the ridges, trenches and transform faults involved, making some simplifying assumptions and applying simple velocity calculations. This assessment can generalise to most actual triple junction settings provided the assumptions and definitions broadly apply to the real Earth.

A stable junction is one at which the geometry of the junction is retained with time as the plates involved move. This places restrictions on relative velocities and plate boundary orientation. An unstable triple junction will change with time, either to become another form of triple junction (RRF junctions easily evolve to FFR junctions), will change geometry or are simply not feasible (as in the case of FFF junctions). The inherent instability of an FFF junction is believed to have caused the formation of the Pacific Plate about 190 million years ago.[4]

By assuming that plates are rigid and that the Earth is spherical, Leonhard Euler’s theorem of motion on a sphere can be used to reduce the stability assessment to determining boundaries and relative motions of the interacting plates. The rigid assumption holds very well in the case of oceanic crust, and the radius of the Earth at the equator and poles only varies by a factor of roughly one part in 300 so the Earth approximates very well to a sphere.

McKenzie and Morgan[5] first analysed the stability of triple junctions using these assumptions with the additional assumption that the Euler poles describing the motions of the plates were such that they approximated to straight line motion on a flat surface. This simplification applies when the Euler poles are distant from the triple junction concerned. The definitions they used for R, T and F are as follows:

Stability criteria

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For a triple junction between the plates A, B and C to exist, the following condition must be satisfied:

AvB + BvC + CvA = 0

where AvB is the relative motion of B with respect to A.

This condition can be represented in velocity space by constructing a velocity triangle ABC where the lengths AB, BC and CA are proportional to the velocities AvB, BvC and CvA respectively.

Further conditions must also be met for the triple junction to exist stably – the plates must move in a way that leaves their individual geometries unchanged. Alternatively the triple junction must move in such a way that it remains on all three of the plate boundaries involved.

McKenzie and Morgan[6] demonstrated that these criteria can be represented on the same velocity space diagrams in the following way. The lines ab, bc and ca join points in velocity space which will leave the geometry of AB, BC and CA unchanged. These lines are the same as those that join points in velocity space at which an observer could move at the given velocity and still remain on the plate boundary. When these are drawn onto the diagram containing the velocity triangle these lines must be able to meet at a single point, for the triple junction to exist stably.

These lines necessarily are parallel to the plate boundaries as to remain on the plate boundaries the observer must either move along the plate boundary or remain stationary on it.

The point at which these lines meet, J, gives the overall motion of the triple junction with respect to the Earth.

Using these criteria it can easily be shown why the FFF triple junction is not stable: the only case in which three lines lying along the sides of a triangle can meet at a point is the trivial case in which the triangle has sides lengths zero, corresponding to zero relative motion between the plates. As faults are required to be active for the purpose of this assessment, an FFF junction can never be stable.


McKenzie and Morgan determined that there were 16 types of triple junction theoretically possible, though several of these are speculative and have not necessarily been seen on Earth. These junctions were classified firstly by the types of plate boundaries meeting – for example RRR, TTR, RRT, FFT etc. – and secondly by the relative motion directions of the plates involved. Some configurations such as RRR can only have one set of relative motions whereas TTT junctions may be classified into TTT(a) and TTT(b). These differences in motion direction affect the stability criteria.

McKenzie and Morgan claimed that of these 16 types, 14 were stable with FFF and RRF configurations unstable, however, York[7] later showed that the RRF configuration could be stable under certain conditions.

Ridge-Ridge-Ridge junctions

A map of the Afar triangle, showing the East of Africa and the three ridges passing through the Red Sea, the Gulf of Aden and the East African Rift Valley.
A map of the Afar triangle in East Africa, an example of an RRR junction and the only triple junction on Earth that can be seen above sea level.

An RRR junction is always stable using these definitions and therefore very common on Earth, though in a geological sense ridge spreading is usually discontinued in one direction leaving a failed rift zone. There are many examples of these present both now and in the geological past such as the South Atlantic opening with ridges spreading North and South to form the Mid-Atlantic Ridge, and an associated aulacogen, the Benue Trough, in the Niger Delta region of Africa. RRR junctions are also common as rifting along three fractures at 120° is the best way to relieve stresses from uplift at the surface of a sphere; on Earth, stresses similar to these are believed to be caused by the mantle hotspots thought to initiate rifting in continents.

The stability of RRR junctions is demonstrated below – as the perpendicular bisectors of the sides of a triangle always meet at a single point, the lines ab, bc and ca can always be made to meet regardless of relative velocities.

Ridge-Trench-Fault junctions

RTF junctions are less common, an unstable junction of this type (an RTF(a)) is thought to have existed at roughly 12Ma at the mouth of the Gulf of California where the East Pacific Rise currently meets the San Andreas Fault zone.[8] The Guadeloupe and Farallon microplates were previously being subducted under the North American Plate and the northern end of this boundary met the San Andreas Fault. Material for this subduction was provided by a ridge equivalent to the modern East Pacific Rise slightly displaced to the west of the trench. As the ridge itself was subducted an RTF triple junction momentarily existed but subduction of the ridge caused the subducted lithosphere to weaken and ‘tear’ from the point of the triple junction. The loss of slab pull caused by the detachment of this lithosphere ended the RTF junction giving the present day ridge – fault system. An RTF(a) is stable if ab goes through the point in velocity space C, or if ac and bc are colinear.

Trench-Trench-Trench junctions

A TTT(a) junction can be found in central Japan where the Eurasian plate overrides the Philippine and Pacific plates, with the Philippine plate also overriding the Pacific. Here the Japan Trench effectively branches to form the Ryukyu and Bonin arcs. The stability criteria for this type of junction are either ab and ac form a straight line or that the line bc is parallel to CA.


The Nootka Fault at the triple junction of the North American Plate, the Explorer Plate, and the Juan de Fuca

See also


  1. ^ C. M. R. Fowler; Connie May Fowler; Clarence Mary R. Fowler (2005). The Solid Earth: An Introduction to Global Geophysics. Cambridge University Press. p. 26. ISBN 978-0-521-58409-8.
  2. ^ McKenzie, D. P.; Morgan, W. J. (11 October 1969). "Evolution of Triple Junctions". Nature. 224 (5215): 125–133. Bibcode:1969Natur.224..125M. doi:10.1038/224125a0. S2CID 4151329.
  3. ^ S. W. Petters (May 1978). "Stratigraphic Evolution of the Benue Trough and Its Implications for the Upper Cretaceous Paleogeography of West Africa". The Journal of Geology. 86 (3): 311–322. Bibcode:1978JG.....86..311P. doi:10.1086/649693. JSTOR 30061985. S2CID 129346979.
  4. ^ Boschman, Lydian M.; Hinsbergen, Douwe J. J. van (2016-07-01). "On the enigmatic birth of the Pacific Plate within the Panthalassa Ocean". Science Advances. 2 (7): e1600022. Bibcode:2016SciA....2E0022B. doi:10.1126/sciadv.1600022. ISSN 2375-2548. PMC 5919776. PMID 29713683.
  5. ^ Evolution of Triple Junctions, McKenzie, D. P., and Morgan, W. J., Nature, 224, 125 (1969)
  6. ^ Evolution of Triple Junctions, McKenzie, D. P., and Morgan, W. J., Nature, 224, 125 (1969)
  7. ^ York, Derek (1973). "Evolution of Triple Junctions". Nature. 244 (5415): 341–342. doi:10.1038/244341a0. ISSN 0028-0836. S2CID 4202607.
  8. ^ "Archived copy" (PDF). Archived from the original (PDF) on 2011-07-27. Retrieved 2009-11-21.((cite web)): CS1 maint: archived copy as title (link)
  9. ^ Sauter, D.; Mendel, V.; Rommeveaux-Jestin, C. (1997). "Propagation of the Southwest Indian Ridge at the Rodrigues Triple Junction". Journal Marine Geophysical Researches. 19 (6): 553–567. Bibcode:1997MarGR..19..553S. doi:10.1023/A:1004313109111. S2CID 127866775.
  10. ^ Carracedo, Juan Carlos; Troll, Valentin R. (2021-01-01), "North-East Atlantic Islands: The Macaronesian Archipelagos", in Alderton, David; Elias, Scott A. (eds.), Encyclopedia of Geology (Second Edition), Oxford: Academic Press, pp. 674–699, doi:10.1016/b978-0-08-102908-4.00027-8, ISBN 978-0-08-102909-1, S2CID 226588940, retrieved 2021-03-18
  11. ^ White, N.; Latin, D. (1993). "Subsidence analyses from the North Sea 'triple-junction'" (PDF). Journal of the Geological Society. 150 (3): 473–488. Bibcode:1993JGSoc.150..473W. doi:10.1144/gsjgs.150.3.0473. S2CID 129832756. Archived from the original (PDF) on 2011-08-12.
  12. ^ Oakey, Gordon N.; Stephenson, Randell (2008). "Crustal structure of the Innuitian region of Arctic Canada and Greenland from gravity modelling: implications for the Palaeogene Eurekan orogen" (PDF). Geophysical Journal International. 173 (3). Royal Astronomical Society: 1041. Bibcode:2008GeoJI.173.1039O. doi:10.1111/j.1365-246X.2008.03784.x. ISSN 0956-540X.