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Geology; May 2008; v. 36; no. 5; p. 339-342; DOI: 10.1130/G24431A.1
© 2008 Geological Society of America
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Cracking of lithosphere north of the Galapagos triple junction

Hans Schouten1, Deborah K. Smith1, Laurent G.J. Montési2, Wenlu Zhu2 and Emily M. Klein3

1 Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA
2 Department of Geology, University of Maryland, College Park, Maryland 20742, USA
3 Division of Earth and Ocean Sciences, Duke University, Durham, North Carolina 27708, USA

The Galapagos triple junction is a ridge-ridge-ridge triple junction where the Cocos, Nazca, and Pacific plates meet around the Galapagos microplate. Directly north of the large scarps of the Cocos-Nazca Rift, a 250-km-long and 50-km-wide band of northwest-southeast–trending cracks with volcanics at their western ends crosscuts and blankets the north-south–trending abyssal hills of the East Pacific Rise. It appears that the roughly northeast-southwest extension of East Pacific Rise–generated seafloor has been accommodated by a succession of minor rifts that, during at least the past 4 m.y., had their triple junctions with the East Pacific Rise at distances of 50–100 km north of the tip of the propagating Cocos-Nazca Rift. We propose that the rift locations are controlled by stresses associated with the dominant Cocos-Nazca Rift, and scaled by the distance of its tip to the East Pacific Rise. We speculate that similar ephemeral rifts occurred south of the Cocos-Nazca Rift and were instrumental in the origin of the rotating Galapagos microplate ca. 1.5 Ma.

Key Words: Galapagos triple junction • plate boundaries • lithospheric stress






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