Bottom Sediment Distribution in Certain Inshore Waters of Hong Kong

Authors

  • W. D. Chesterman University of Hong Kong
  • H. K. Wong University of Hong Kong

Abstract

The continental shelf in the vicinity of Hong Kong is about 100 miles wide, trending northeast-southwest roughly parallel to the Chinese coast. The bottom slope averages 0° 02' seawards, increasing to 1° 50' near the shelf break. Several extensive studies of the area have been carried out (Shepard et al., 1949; Klenova, 1958; Niino and Emery, 1961; Wang, 1961; Ching, 1963; and USNOO, 1968), but none of them extended into the inshore waters of Hong Kong. In 1964, a programme to study the bottom sediment distribution in these inshore areas using a side-scan sonar was initiated by the Denartment of Physics at the University of Hong Kong. Results of the early phases of the work have already been reported (Chesterman et al., 1967). This paper summarizes the findings of the latter part of the study.

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Published

2015-07-02

How to Cite

Chesterman, W. D., & Wong, H. K. (2015). Bottom Sediment Distribution in Certain Inshore Waters of Hong Kong. The International Hydrographic Review, 48(2). Retrieved from https://journals.lib.unb.ca/index.php/ihr/article/view/23882

Issue

1971: Vol. XLVIII, No. 2

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Articles

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 Anders, F.J. and Byrnes, M.R.(1991). “Accuracy of shoreline change rates as determined from maps and aerial photographs”, Shore and Beach, 59, pp. 17-26.

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Foley, J.D., van Dam, A., Feiner, S. K. and Hughes, J.F. (1990), Computer Graphics – Principles and Practice, 2nd ed., Addison-Wesley, Reading, MA.

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Smith, A. (1988). Colour photomapping. Report NRC-01-512. National Research Centre. Ottawa, Canada.

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desJardins, M. (2005). How to succeed in postgraduate  study, Applied Ecology Research Group, University of Canberra, viewed 26 April 2009, http://aerg.canberra.edu.au/jardins.t.htm.

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