Synonyms
Definition
An axial summit trough (AST) is a narrow trough or volcanically modified graben that develops at the crest of a midocean ridge and typically is the locus of volcanic and hydrothermal activity.
Introduction
At the summit of magmatically robust midocean ridges (MORs), a narrow trough may develop that marks the location of the divergent plate boundary and is the locus of most magmatic and hydrothermal activity (Macdonald and Fox, 1988). This axial summit trough (AST) is typically less than 500 m in width and 50 m in depth and may be discontinuous along the ridge in terms of its width, depth, strike, and continuity. ASTs are common along fast- and intermediate-spreading rate ridges (e.g., East Pacific Rise, Juan de Fuca Ridge, Galapagos Spreading Center), and magma-rich, inflated portions of the slow-spreading Mid-Atlantic Ridge and Lau Basin back-arc spreading center.
Development of the Axial Summit Trough
The...
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Soule, S.A., Perfit, M. (2015). Axial Summit Trough. In: Harff, J., Meschede, M., Petersen, S., Thiede, J. (eds) Encyclopedia of Marine Geosciences. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-6644-0_3-2
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DOI: https://doi.org/10.1007/978-94-007-6644-0_3-2
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Axial Summit Trough- Published:
- 02 April 2015
DOI: https://doi.org/10.1007/978-94-007-6644-0_3-2
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Axial Summit Trough- Published:
- 01 December 2014
DOI: https://doi.org/10.1007/978-94-007-6644-0_3-1