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Circular Structures Observed in the Deep Sea by the Swathmap Long-Range Sidescan Sonar

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Bottom-Interacting Ocean Acoustics

Part of the book series: NATO Conference Series ((NATOCS,volume 5))

Abstract

The marine geologist/geophysicist’s principal tools for studying the seafloor are acoustic. The first major increase in understanding the seafloor following the original Challeger Expedition came in the 1950’s with the routine application of precision echo sounding techniques from research vessels.

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References

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© 1980 Plenum Press, New York

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Andrews, J.E., Humphrey, P. (1980). Circular Structures Observed in the Deep Sea by the Swathmap Long-Range Sidescan Sonar. In: Kuperman, W.A., Jensen, F.B. (eds) Bottom-Interacting Ocean Acoustics. NATO Conference Series, vol 5. Springer, Boston, MA. https://doi.org/10.1007/978-1-4684-9051-0_8

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  • DOI: https://doi.org/10.1007/978-1-4684-9051-0_8

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4684-9053-4

  • Online ISBN: 978-1-4684-9051-0

  • eBook Packages: Springer Book Archive

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