Geomorphological modelling and mapping of the Peru-Chile Trench by GMT

The author presents a geospatial analysis of the Peru-Chile Trench located in the South Pacific Ocean by the Generic Mapping Tool (GMT) scripting toolset used to process and model data sets. The study goal is to perform geomorphological modelling by the comparison of two segments of the trench locat...

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Main Author: Lemenkova Polina
Format: Article
Language:English
Published: Sciendo 2019-12-01
Series:Polish Cartographical Review
Subjects:
Online Access:https://doi.org/10.2478/pcr-2019-0015
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author Lemenkova Polina
author_facet Lemenkova Polina
author_sort Lemenkova Polina
collection DOAJ
description The author presents a geospatial analysis of the Peru-Chile Trench located in the South Pacific Ocean by the Generic Mapping Tool (GMT) scripting toolset used to process and model data sets. The study goal is to perform geomorphological modelling by the comparison of two segments of the trench located in northern (Peruvian) and southern (Chilean) parts. The aim of the study is to perform automatic digitizing profiles using GMT and several scripting modules. Orthogonal cross-section profiles transecting the trench in a perpendicular direction were automatically digitized, and the profiles visualized and compared. The profiles show variations in the geomorphology of the trench in the northern and southern segments. To visualize geological and geophysical settings, a set of the thematic maps was visualized by GMT modules: free-air gravity anomaly, geoid, geology and bathymetry. The results of the descriptive statistical analysis of the bathymetry in both segments show that the most frequent depths for the Peruvian segment of the Peru-Chile Trench range from -4,000 to -4,200 (827 recorded samples) versus the range of -4,500 to -4,700 m for the Peruvian segment (1,410 samples). The Peruvian segment of the trench is deeper and its geomorphology steeper with abrupt slopes compared to the Chilean segment. A comparison of the data distribution for both segments gives the following results. The Peruvian segment has the majority of data (23%) reaching 1,410 (-4,500 m to -4,700 m). This peak shows a steep pattern in data distribution, while other data in the neighbouring diapason are significantly lower: 559 (-4,700 m to -5,000 m) and 807 (-4,200 m to -4,400 m). The Chilean segment has more unified data distribution for depths of -6,000 m to -7,000 m. This paper presents GMT workflow for the cartographic automatic modelling and mapping deep-sea trench geomorphology.
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spelling doaj.art-62d507d3e0d640ca89f8796710cd79d72022-12-22T03:44:28ZengSciendoPolish Cartographical Review0324-83212450-69662019-12-0151418119410.2478/pcr-2019-0015pcr-2019-0015Geomorphological modelling and mapping of the Peru-Chile Trench by GMTLemenkova Polina0Ocean University of China, College of Marine Geo-sciences, Qingdao, ChinaThe author presents a geospatial analysis of the Peru-Chile Trench located in the South Pacific Ocean by the Generic Mapping Tool (GMT) scripting toolset used to process and model data sets. The study goal is to perform geomorphological modelling by the comparison of two segments of the trench located in northern (Peruvian) and southern (Chilean) parts. The aim of the study is to perform automatic digitizing profiles using GMT and several scripting modules. Orthogonal cross-section profiles transecting the trench in a perpendicular direction were automatically digitized, and the profiles visualized and compared. The profiles show variations in the geomorphology of the trench in the northern and southern segments. To visualize geological and geophysical settings, a set of the thematic maps was visualized by GMT modules: free-air gravity anomaly, geoid, geology and bathymetry. The results of the descriptive statistical analysis of the bathymetry in both segments show that the most frequent depths for the Peruvian segment of the Peru-Chile Trench range from -4,000 to -4,200 (827 recorded samples) versus the range of -4,500 to -4,700 m for the Peruvian segment (1,410 samples). The Peruvian segment of the trench is deeper and its geomorphology steeper with abrupt slopes compared to the Chilean segment. A comparison of the data distribution for both segments gives the following results. The Peruvian segment has the majority of data (23%) reaching 1,410 (-4,500 m to -4,700 m). This peak shows a steep pattern in data distribution, while other data in the neighbouring diapason are significantly lower: 559 (-4,700 m to -5,000 m) and 807 (-4,200 m to -4,400 m). The Chilean segment has more unified data distribution for depths of -6,000 m to -7,000 m. This paper presents GMT workflow for the cartographic automatic modelling and mapping deep-sea trench geomorphology.https://doi.org/10.2478/pcr-2019-0015gmtmappingperu-chile trenchsubmarine geomorphology
spellingShingle Lemenkova Polina
Geomorphological modelling and mapping of the Peru-Chile Trench by GMT
Polish Cartographical Review
gmt
mapping
peru-chile trench
submarine geomorphology
title Geomorphological modelling and mapping of the Peru-Chile Trench by GMT
title_full Geomorphological modelling and mapping of the Peru-Chile Trench by GMT
title_fullStr Geomorphological modelling and mapping of the Peru-Chile Trench by GMT
title_full_unstemmed Geomorphological modelling and mapping of the Peru-Chile Trench by GMT
title_short Geomorphological modelling and mapping of the Peru-Chile Trench by GMT
title_sort geomorphological modelling and mapping of the peru chile trench by gmt
topic gmt
mapping
peru-chile trench
submarine geomorphology
url https://doi.org/10.2478/pcr-2019-0015
work_keys_str_mv AT lemenkovapolina geomorphologicalmodellingandmappingoftheperuchiletrenchbygmt