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Correction to: New constraints on coseismic slip during southern Cascadia subduction zone earthquakes over the past 4600 years implied by tsunami deposits and marine turbidites

Author

Listed:
  • George R. Priest

    (Oregon Department of Geology and Mineral Industries, Newport Coastal Field Office)

  • Robert C. Witter

    (U.S. Geological Survey, Alaska Science Center)

  • Yinglong J. Zhang

    (Virginia Institute of Marine Science)

  • Chris Goldfinger

    (Oregon State University)

  • Kelin Wang

    (Geological Survey of Canada, Pacific Geoscience Centre)

  • Jonathan C. Allan

    (Oregon Department of Geology and Mineral Industries, Newport Coastal Field Office)

Abstract

This correction stands to correct Figure 7c listing a low minimum slip of 12 m for Case 2 instead of the correct value of 8 m, as stated in the body of the text and depicted on the chart of cumulative slip. The corrected chart explanation and caption are shown below. This error did not affect any of the findings of the paper or the chart itself. This is a correction to the original article.

Suggested Citation

  • George R. Priest & Robert C. Witter & Yinglong J. Zhang & Chris Goldfinger & Kelin Wang & Jonathan C. Allan, 2018. "Correction to: New constraints on coseismic slip during southern Cascadia subduction zone earthquakes over the past 4600 years implied by tsunami deposits and marine turbidites," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 93(2), pages 1109-1111, September.
    • Handle: RePEc:spr:nathaz:v:93:y:2018:i:2:d:10.1007_s11069-018-3405-x
    DOI: 10.1007/s11069-018-3405-x
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