Topography of the Aleutian Trench south-east off Bowers Ridge, Bering Sea, in the context of the geological development of North Pacific Ocean

Baltica, Volume 34 Number 1 June 2021: 27–46. DOI: 10.5200/baltica.2021.1.3

20 Pages Posted: 28 May 2021

See all articles by Polina Lemenkova

Polina Lemenkova

Université Libre de Bruxelles (ULB), École polytechnique de Bruxelles

Date Written: June 20, 2021

Abstract

The research is focused on the topographic modelling and mapping of the Aleutian Trench. The study area is situated in the Bering Sea, a marginal sea located northernmost of the Pacific Ocean, between Alaska and Kamchatka Peninsula. The geological setting of the region is characterized by the subduction of the oceanic Pacific Plate below the continental North American Plate. Other features include high seismic activity along the Aleutian island arcs bordering the oceanic seafloor. The objective of this paper is to explore the inter- action between the geophysical setting affecting the relief of the seafloor by using geoinformation techniques and geological analysis. In the hypothesis of this study, variations in the geophysical fields as independent variables are reflected in the morphology of the seafloor, which can be observed using data visualization by the advanced cartographic scripting solutions. The open source high-resolution topographic map (ETOPO1), marine free-air gravity and Bouguer gravity anomaly data were used and integrated to investigate the po- tential correlation between the geophysical, geological, tectonic and topographic settings of the Bering Sea. Our main method includes bathymetric mapping of the area with publicly available bathymetric data using GMT. Materials include open source data: ETOPO1 raster grid with 1 arc-minute resolution, EGM96 gravity and vector contour layers of GMT. The research included complex thematic mapping of the region, includ- ing topographic, contour, geodetic and geophysical mapping, 3D modelling and geomorphological plotting of the 30 cross-section segments of the trench located SE off the Bowers Ridge. According to the processed ETOPO1 dataset, the minimal depth is -8480 m and the mean is -3089.154 m. The geoid undulations model shows that the majority of the gravity values lie in the interval between -10 and 20 m with the lowest values along the trench. The statistical histogram shows that the most common depth value in the segment of the Aleutian Trench is -4800 m, occurring 1722 times. The profile linear trend modelling was done with four dif- ferent approaches of the regression model (y = f(x) + e) by weighted least squares (WLS) with arguments: 1) m2t = a + bt (polynomial model degree one); 2) m3t = a + bt + ct2 (polynomial model degree two); 3) m4t = a + bt + ct2 + dcos2π*t + esin2π*t (polynomial model with Fourier series one); and 4) additional plotting residuals. Surface modelling was performed using xyz modelling from the ASCII data enlarging fragment towards SE of the Bowers Ridge. The tested functionality of modules of GMT presented an effective cartographic scripting toolset enabling a precise topographic mapping and 3D modelling. The paper contributes to a more detailed understanding of the Pacific Ocean seafloor bathymetry, more specifically of the selected segment of the Aleu- tian Trench near Bowers Ridge area.

Keywords: GMT; cartography; geology; 3D modelling; geophysics; gravity

JEL Classification: Y92, Q00, Q01, Q22, Q23, Q24, Q33, Q34, Q35, Q54, Q55, C00, C02, C30, C31, C60, C61, C90

Suggested Citation

Lemenkova, Polina, Topography of the Aleutian Trench south-east off Bowers Ridge, Bering Sea, in the context of the geological development of North Pacific Ocean (June 20, 2021). Baltica, Volume 34 Number 1 June 2021: 27–46. DOI: 10.5200/baltica.2021.1.3, Available at SSRN: https://ssrn.com/abstract=3854076

Polina Lemenkova (Contact Author)

Université Libre de Bruxelles (ULB), École polytechnique de Bruxelles ( email )

CP 132 Av FD Roosevelt 50
Brussels, Brussels 1050
Belgium
+32 471 86 04 59 (Phone)

HOME PAGE: http://https://www.ulb.be/

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