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These areas are named triple junctions and can be found in several places across the world today.
A triple junction is the point at which three plate boundaries meet.
It is the third arm of the triple junction rift system.
It is a triple junction and three subduction zones are involved.
It is an unusual type of triple junction in which the three plates do not meet at a simple intersection.
The point at which these lines meet, J, gives the overall motion of the triple junction with respect to the earth.
Triple junctions were once defined simply as the meeting point of three spreading ridges.
Triple junction stability is a term used in geology.
In the triple junction of the two walls and the ceiling was a closed circuit television camera, with a red light on under the lens.
The connecting three arms form a triple junction.
Alternatively the triple junction must move in such a way that it remains on all three of the plate boundaries involved.
It is a geologic triple junction where three tectonic plates come together.
There is a triple junction fault nearby and several andesitic volcanoes.
The grain boundaries intersect at 120 triple junctions under ideal conditions.
The Izu arc ends there at a tectonic triple junction.
Thus, analysis of triple junctions can usually be done on a flat surface with motions defined by vectors.
The plate boundaries which meet at this triple junction are all subduction zones (trenches).
The Niger River has formed in the failed rift arm of the triple junction.
The Cascadia subduction zone runs from triple junctions at its north and south ends.
Three major tectonic plates meet at this triple junction:
We also have, however, the shipping junction on the Danube, and in the long run this would become a triple junction.
This simplification applies when the Euler poles are distant from the triple junction concerned.
The movement may have been caused by absorption of lateral motion between the northern pair of triple junctions.
The islands are located at the Galapagos Triple Junction.
The origin of new divergent boundaries at triple junctions is sometimes thought to be associated with the phenomenon known as hotspots.
Wörterbuch für Geologie