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Journal of the Oceanographical Society of Japan

, Volume 35, Issue 6, pp 261–267 | Cite as

Sedimentation rates in Funka Bay, HokkaidÔ

  • Eiji Matsumoto
  • Shigeko Togashi
Article

Abstract

Undisturbed sediment cores were collected by a modified gravity corer from Funka Bay. The sedimentation rate is determined by both210Pb and pumice chronological methods. The sedimentation rates by210Pb method are concordant with those by pumice methods. The derived rate varies from 0.06 to 0.22 g cm−2 y−1, and an average is 0.09 g cm−2 y−1.

Keywords

Sedimentation Sedimentation Rate Sediment Core Gravity Corer Undisturbed Sediment 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

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Copyright information

© Oceanographical Society of Japan 1980

Authors and Affiliations

  • Eiji Matsumoto
    • 1
  • Shigeko Togashi
    • 1
  1. 1.Geological Survey of JapanIbarakiJapan

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