Geomorphology of the small island of Tidore and Hiri (North Maluku, Indonesia)

Tidore and Hiri Islands in North Maluku Province is the result of a complex tectonic setting. In contrast with Ternate Island and its well-known volcano, Gamalama volcano, there is still a lack of research about volcanic information or volcanic landform in Tidore and Hiri Islands. Even though the tw...

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Autores principales: Mutaqin Bachtiar W, Marfai Muh Aris, Hadmoko Danang Sri, Lavigne Franck, Faral Audrey, Wijayanti Helvetia, Riasasi Widiyana
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Publicado: EDP Sciences 2021
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Acceso en línea:https://doaj.org/article/cfb1674dff31437e93a224839f6f0b58
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spelling oai:doaj.org-article:cfb1674dff31437e93a224839f6f0b582021-12-02T17:11:57ZGeomorphology of the small island of Tidore and Hiri (North Maluku, Indonesia)2267-124210.1051/e3sconf/202132503012https://doaj.org/article/cfb1674dff31437e93a224839f6f0b582021-01-01T00:00:00Zhttps://www.e3s-conferences.org/articles/e3sconf/pdf/2021/101/e3sconf_icst2021_03012.pdfhttps://doaj.org/toc/2267-1242Tidore and Hiri Islands in North Maluku Province is the result of a complex tectonic setting. In contrast with Ternate Island and its well-known volcano, Gamalama volcano, there is still a lack of research about volcanic information or volcanic landform in Tidore and Hiri Islands. Even though the two islands also have volcanoes, i.e., Hiri and Tidore/Kiematubu volcano. This study aims to provide geomorphological information, especially in Tidore and Hiri Islands, since this information is hard to find whereas it is very important to disaster mitigation and landuse planning. We used remote sensing images, digital elevation models (DEM), and geological maps to classify geomorphological information of the small island of Tidore and Hiri in the North Maluku based on geomorphological aspects, i.e., morphology, morphogenesis, morpho-chronology, and morpho-arrangement. As a volcanic island, the slope in Tidore and Hiri Island is dominated by a slightly steep (8°-16°) and a steep slope (16°-35°), while the relief is dominated by hills and mountainous. Volcanic landforms on Tidore and Hiri Islands are characterized by relatively symmetrical cone-shaped volcanic cones, which are accumulations of falling pyroclastic material and lava ejected from magma vents. Volcanic islands include the case of Tidore and Hiri Island have radial centrifugal river flow patterns. The material on Tidore and Hiri Islands is dominated by Holocene volcanic rocks. In Tidore, there is alluvial material on the west and east coasts of the island. This study result also can be developed into more detailed geomorphological maps, or landscape evolution in a volcanic island, or spatial planning.Mutaqin Bachtiar WMarfai Muh ArisHadmoko Danang SriLavigne FranckFaral AudreyWijayanti HelvetiaRiasasi WidiyanaEDP SciencesarticleEnvironmental sciencesGE1-350ENFRE3S Web of Conferences, Vol 325, p 03012 (2021)
institution DOAJ
collection DOAJ
language EN
FR
topic Environmental sciences
GE1-350
spellingShingle Environmental sciences
GE1-350
Mutaqin Bachtiar W
Marfai Muh Aris
Hadmoko Danang Sri
Lavigne Franck
Faral Audrey
Wijayanti Helvetia
Riasasi Widiyana
Geomorphology of the small island of Tidore and Hiri (North Maluku, Indonesia)
description Tidore and Hiri Islands in North Maluku Province is the result of a complex tectonic setting. In contrast with Ternate Island and its well-known volcano, Gamalama volcano, there is still a lack of research about volcanic information or volcanic landform in Tidore and Hiri Islands. Even though the two islands also have volcanoes, i.e., Hiri and Tidore/Kiematubu volcano. This study aims to provide geomorphological information, especially in Tidore and Hiri Islands, since this information is hard to find whereas it is very important to disaster mitigation and landuse planning. We used remote sensing images, digital elevation models (DEM), and geological maps to classify geomorphological information of the small island of Tidore and Hiri in the North Maluku based on geomorphological aspects, i.e., morphology, morphogenesis, morpho-chronology, and morpho-arrangement. As a volcanic island, the slope in Tidore and Hiri Island is dominated by a slightly steep (8°-16°) and a steep slope (16°-35°), while the relief is dominated by hills and mountainous. Volcanic landforms on Tidore and Hiri Islands are characterized by relatively symmetrical cone-shaped volcanic cones, which are accumulations of falling pyroclastic material and lava ejected from magma vents. Volcanic islands include the case of Tidore and Hiri Island have radial centrifugal river flow patterns. The material on Tidore and Hiri Islands is dominated by Holocene volcanic rocks. In Tidore, there is alluvial material on the west and east coasts of the island. This study result also can be developed into more detailed geomorphological maps, or landscape evolution in a volcanic island, or spatial planning.
format article
author Mutaqin Bachtiar W
Marfai Muh Aris
Hadmoko Danang Sri
Lavigne Franck
Faral Audrey
Wijayanti Helvetia
Riasasi Widiyana
author_facet Mutaqin Bachtiar W
Marfai Muh Aris
Hadmoko Danang Sri
Lavigne Franck
Faral Audrey
Wijayanti Helvetia
Riasasi Widiyana
author_sort Mutaqin Bachtiar W
title Geomorphology of the small island of Tidore and Hiri (North Maluku, Indonesia)
title_short Geomorphology of the small island of Tidore and Hiri (North Maluku, Indonesia)
title_full Geomorphology of the small island of Tidore and Hiri (North Maluku, Indonesia)
title_fullStr Geomorphology of the small island of Tidore and Hiri (North Maluku, Indonesia)
title_full_unstemmed Geomorphology of the small island of Tidore and Hiri (North Maluku, Indonesia)
title_sort geomorphology of the small island of tidore and hiri (north maluku, indonesia)
publisher EDP Sciences
publishDate 2021
url https://doaj.org/article/cfb1674dff31437e93a224839f6f0b58
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AT hadmokodanangsri geomorphologyofthesmallislandoftidoreandhirinorthmalukuindonesia
AT lavignefranck geomorphologyofthesmallislandoftidoreandhirinorthmalukuindonesia
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