Mid-Cayman Rise
The Mid-Cayman Rise or Mid-Cayman Spreading Center is a relatively short (110 km long) divergent plate boundary in the middle of the Cayman Trough. It forms part of a dominantly transform boundary that is part of the southern margin to the North American Plate. It is an ultra-slow spreading center with an opening rate of 15–17 mm per year.[1]
Formation
The Mid-Cayman Rise developed during the Eocene when the northern part of the Caribbean Plate collided with the Bahamas Platform, forcing the southern boundary to propagate southwards. This boundary initially formed as two strike-slip faults with a large left-stepping offset between them, generating a pull-apart basin. Continuing movement on the boundary and extension within the pull-apart led to the formation of an area of oceanic crust containing a north-south trending spreading center that remains active to the present day.
When the spreading center formed, all the displacement on the Swan Islands Transform Fault was transferred by the Mid-Cayman Rise to the Septentrional-Oriente fault zone. During the Late Miocene, the leading edge of the Caribbean Plate began to collide with the Bahamas Platform. This led to the development of a new fault system, formed of the Walton fault zone and the Enriquillo–Plantain Garden fault zone, carrying some of the plate boundary displacement and creating the Gonâve Microplate. Eventually all the displacement on the plate boundary is expected to move onto the southern fault system as the microplate becomes accreted to the North American Plate, at which point the Mid-Cayman Rise will become extinct.[2]
Hydrothermal Vents
The Mid-Cayman Rise is a particularly unique location as there are two confirmed hydrothermal fields in close proximity of each other. The Von Damm vent field, named after geological oceanographer Karen Von Damm, is located on the ocean core complex Mount Dent, and features unique chimney structures of talc. The Beebe Vent field, after William Beebe, is the world's deepest hydrothermal system with extremely hot vent fluids.[3] There is activity in the water column to suggest a third vent field, though it has not yet been identified.[4]
We know hydrothermal vents appear along ridges approximately every 100 kilometers [62 miles]. But this ridge crest is only 100 kilometers long, so we should only have expected to find evidence for one site at most. So finding evidence for three sites was quite unexpected – but then finding out that our data indicated that each site represents a different style of venting – one of every kind known, all in pretty much the same place – was extraordinarily cool.
— Chris German, 2010, Astrobiology Magazine [5]
References
- ^ Hayman N.W.; Grindlay N.R.; Perfit M.R.; Mann P.; Leroy S.; de Lépinay B.M. (2011). "Oceanic core complex development at the ultraslow spreading Mid-Cayman Spreading Center". Geochemistry, Geophysics, Geosystems. 12 (3): n/a. Bibcode:2011GGG....12.AG02H. doi:10.1029/2010GC003240.
- ^ Mann, P.; Taylor, F.W.; Edwards, R. Lawrence; Ku, Teh Lung (1995). "Actively evolving microplate formation by oblique collision and sideways motion along strike-slip faults: An example from the northeastern Caribbean plate margin". Tectonophysics. 246 (1–3): 1–69. Bibcode:1995Tectp.246....1M. doi:10.1016/0040-1951(94)00268-E.
- ^ "Two new hydrothermal vent fields discovered". University of Bergen.
- ^ German, C. R.; Bowen, A.; Coleman, M. L.; Honig, D. L.; Huber, J. A.; Jakuba, M. V.; Kinsey, J. C.; Kurz, M. D.; Leroy, S.; McDermott, J. M.; de Lepinay, B. M.; Nakamura, K.; Seewald, J. S.; Smith, J. L.; Sylva, S. P.; Van Dover, C. L.; Whitcomb, L. L.; Yoerger, D. R. (21 July 2010). "Diverse styles of submarine venting on the ultraslow spreading Mid-Cayman Rise". Proceedings of the National Academy of Sciences. 107 (32): 14020–14025. doi:10.1073/pnas.1009205107.
- ^ "The World's Deepest Vent". Astrobiology Magazine. 25 July 2010.