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Western Coastal & Marine Geology

Pacific Science (1997), vol. 51, no. 1:54-75. Reproduced by permission of the University of Hawaii Press.

Sea-Floor Geology of a Part of Mamala Bay, Hawaii 1

Monty A. Hampton, Michael E. Torresan, and John H. Barber, Jr. 2

U.S. Geological Survey, Menlo Park, California, USA

  Materials, 1
  Materials, 2
  Structures, 1
  Structures, 2
Discussion, 1
Discussion, 2
1 2 3 4 5
6 7 8A 8B 9
10 11 12 13 14
15 16 17 18 19

M.A. Hampton
M.E. Torresan

WCMG Publications

Honolulu Studies

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We surveyed the sea-floor geology within a 200-km2 area of Mamala Bay, off Honolulu, Hawaii by collecting and analyzing sidescan sonar images, 3.5-kHz profiles, video and still visual images, and box-core samples. The study area extends from 20-m water depth on the insular shelf to 600-m water depth in a southeast-trending trough. The sidescan images depict three principal types of sea-floor material: low-backscatter natural sediment, high-backscatter drowned carbonate reef, and intermediate-backscatter dredged-material deposits. Cores indicate that the natural sediment is muddy sand, composed of carbonate reef and microfauna debris with some volcanic grains. Vague areal trends in composition are evident. The dredged material comprises poorly sorted, cobble- to clay-size mixtures of reef, volcanic, and man-made debris, up to 35 cm thick. Dredged-material deposits are not evident in the 3.5-kHz profiles. In the sidescan images they appear as isolated, circular to subcircular imprints, apparently formed by individual drops, around the periphery of their occurrence, but they overlap and coalesce to a nearly continuous, intermediate-backscatter blanket toward the center of three disposal sites investigated.

We did not observe significant currents during our camera surveys, but there is abundant evidence of sediment reworking: symmetrical and asymmetrical ripples in the visual images, sand waves in the 3.5-kHz profiles and side-scan images, moats around the reefs in 3.5-kHz profiles, winnowed dredged material in the visual images, and burial of dredged material by natural sediment in cores. Most current indicators imply a westerly to northwesterly transport direction, along contours or up-slope, although there are a few areas of easterly indicators. Internal waves probably drive the transport; their possible existence is implied by measured water-column density gradients.

1 This study was supported by the U.S. Army Corps of Engineers and the Environmental Protection Agency. Manuscript accepted 5 April 1996.
2 U.S. Geological Survey, Menlo Park, California


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