Using topographic slope distributions to infer seafloor patterns

The authors present a method for obtaining parameters for Sea Beam swath bathymetry which describe the characteristics of abyssal-hill topography. The basic quantity used in the analysis is the distribution of topographic slopes in a region. A convenient means for parameterizing these slopes is thro...

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Published inIEEE journal of oceanic engineering Vol. 14; no. 4; pp. 338 - 347
Main Authors Smith, D.K., Shaw, P.R.
Format Journal Article
LanguageEnglish
Published New York, NY IEEE 01.10.1989
Institute of Electrical and Electronics Engineers
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Abstract The authors present a method for obtaining parameters for Sea Beam swath bathymetry which describe the characteristics of abyssal-hill topography. The basic quantity used in the analysis is the distribution of topographic slopes in a region. A convenient means for parameterizing these slopes is through unit vectors that are normal to small patches of the seafloor; the normal vectors are decomposed into azimuthal and dip components. It is found that the azimuthal distribution of the vectors provides a first-order indication of the dominant elongation directions in the topography, including multiple lineations when they are present. It is shown that the slope statistics are relatively independent of long-wavelength depth variations and are robust even if large anomalous features such as seamounts and fracture zones are included in the section of bathymetry analyzed.< >
AbstractList At scales of tens to hundreds of kilometers, the most prevalent patterns on the seafloor are those formed by the succession of elongate abyssal hills. This seafloor fabric, generated at the ridge axis and modified by sedimentation, mass wasting, and volcanism as it moves away from the ridge, is a record of geologic interest. In this paper the authors describe a method for obtaining parameters from Sea Beam swath bathymetry which describe the characteristics of abyssal-hill topography. The basic quantity that they use in their analysis is the distribution of topographic slopes in a region. They apply the slope-analysis method to three regions in the Northeast Pacific Ocean and two regions in the Southwest Indian Ocean.
The authors present a method for obtaining parameters for Sea Beam swath bathymetry which describe the characteristics of abyssal-hill topography. The basic quantity used in the analysis is the distribution of topographic slopes in a region. A convenient means for parameterizing these slopes is through unit vectors that are normal to small patches of the seafloor; the normal vectors are decomposed into azimuthal and dip components. It is found that the azimuthal distribution of the vectors provides a first-order indication of the dominant elongation directions in the topography, including multiple lineations when they are present. It is shown that the slope statistics are relatively independent of long-wavelength depth variations and are robust even if large anomalous features such as seamounts and fracture zones are included in the section of bathymetry analyzed
The authors present a method for obtaining parameters for Sea Beam swath bathymetry which describe the characteristics of abyssal-hill topography. The basic quantity used in the analysis is the distribution of topographic slopes in a region. A convenient means for parameterizing these slopes is through unit vectors that are normal to small patches of the seafloor; the normal vectors are decomposed into azimuthal and dip components. It is found that the azimuthal distribution of the vectors provides a first-order indication of the dominant elongation directions in the topography, including multiple lineations when they are present. It is shown that the slope statistics are relatively independent of long-wavelength depth variations and are robust even if large anomalous features such as seamounts and fracture zones are included in the section of bathymetry analyzed.< >
Author Smith, D.K.
Shaw, P.R.
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Cites_doi 10.1029/JB093iB11p13589
10.1130/0016-7606(1977)88<621:DSOTSO>2.0.CO;2
10.1007/BF00285656
10.1016/0012-821X(67)90191-4
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Snippet The authors present a method for obtaining parameters for Sea Beam swath bathymetry which describe the characteristics of abyssal-hill topography. The basic...
At scales of tens to hundreds of kilometers, the most prevalent patterns on the seafloor are those formed by the succession of elongate abyssal hills. This...
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StartPage 338
SubjectTerms abyssal hills
Azimuth
bathymetry
Coastal oceanography, estuaries. Regional oceanography
Density functional theory
Earth, ocean, space
Exact sciences and technology
External geophysics
Fabrics
Geology
INE
Marine
mid-ocean ridges
Oceanographic techniques
oceanography
Oceans
Physics of the oceans
Robustness
Sea floor
Shape
signal processing
statistical analysis
Surfaces
swaths
topography
Title Using topographic slope distributions to infer seafloor patterns
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