Klasifikasi gunung api aktif Indonesia, studi kasus dari beberapa letusan gunung api dalam sejarah

<p><a href="http://dx.doi.org/10.17014/ijog.vol1no4.20065">http://dx.doi.org/10.17014/ijog.vol1no4.20065</a></p><p><em>Indonesi</em><em>a is well known as a volcanic country, where more than 30% out of all the world volcanoes occupied this re...

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Main Author: Indyo Pratomo
Format: Article
Language:English
Published: Geological Agency 2014-06-01
Series:Indonesian Journal on Geoscience
Subjects:
Online Access:https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/23
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spelling doaj-90d321d4be3741a7a2c5ab7dae98a4e32020-11-24T23:08:34ZengGeological AgencyIndonesian Journal on Geoscience2355-93142355-93062014-06-011420922710.17014/ijog.1.4.209-22723Klasifikasi gunung api aktif Indonesia, studi kasus dari beberapa letusan gunung api dalam sejarahIndyo Pratomo0Museum Geologi, Pusat Survei Geologi, Jln. Diponegoro No. 57, Bandung<p><a href="http://dx.doi.org/10.17014/ijog.vol1no4.20065">http://dx.doi.org/10.17014/ijog.vol1no4.20065</a></p><p><em>Indonesi</em><em>a is well known as a volcanic country, where more than 30% out of all the world volcanoes occupied this region. Volcanic region is generally densely populated, because of their soil fertility and other land use. Based on their historical eruptions noted since and before 1600 A.D., the Indonesian active volcanoes are regrouped in to A type (79 volcanoes), which were defi ned as volcanoes erupted since 1600 A.D., B type (29 volcanoes) erupted before 1600 A.D., and C type (21 volcanoes) are solfatar fi elds (Bemmelen, 1949; van Padang 1951; Kusumadinata, 1979). Studies on parts of the Indonesian active volcanoes, show different eruptive characters, which are generally related to hazard potentials. A new classifi cation of Indonesian active volcanoes was proposed based on the combination of their physical properties, morphology, volcanic structure and eruptive styles to the eight differents types, those are Tambora (caldera formation), Merapi (lava dome), Agung (open crater), Papandayan (sector failure), Batur (post-caldera activities), Sangeangapi (lava fl ows) and Anak Krakatau types (volcano islands and submarine volcano).</em></p> <p><em>Thi</em><em>s classification would be make a better understanding to different characteristics of Indonesian active volcanoes, for the volcanic hazard and mitigation and also for the applied volcanological researches.</em></p> <p> </p>https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/23Indonesian active volcanoescharacteristicsclassificationvolcanic hazard mitigation
collection DOAJ
language English
format Article
sources DOAJ
author Indyo Pratomo
spellingShingle Indyo Pratomo
Klasifikasi gunung api aktif Indonesia, studi kasus dari beberapa letusan gunung api dalam sejarah
Indonesian Journal on Geoscience
Indonesian active volcanoes
characteristics
classification
volcanic hazard mitigation
author_facet Indyo Pratomo
author_sort Indyo Pratomo
title Klasifikasi gunung api aktif Indonesia, studi kasus dari beberapa letusan gunung api dalam sejarah
title_short Klasifikasi gunung api aktif Indonesia, studi kasus dari beberapa letusan gunung api dalam sejarah
title_full Klasifikasi gunung api aktif Indonesia, studi kasus dari beberapa letusan gunung api dalam sejarah
title_fullStr Klasifikasi gunung api aktif Indonesia, studi kasus dari beberapa letusan gunung api dalam sejarah
title_full_unstemmed Klasifikasi gunung api aktif Indonesia, studi kasus dari beberapa letusan gunung api dalam sejarah
title_sort klasifikasi gunung api aktif indonesia, studi kasus dari beberapa letusan gunung api dalam sejarah
publisher Geological Agency
series Indonesian Journal on Geoscience
issn 2355-9314
2355-9306
publishDate 2014-06-01
description <p><a href="http://dx.doi.org/10.17014/ijog.vol1no4.20065">http://dx.doi.org/10.17014/ijog.vol1no4.20065</a></p><p><em>Indonesi</em><em>a is well known as a volcanic country, where more than 30% out of all the world volcanoes occupied this region. Volcanic region is generally densely populated, because of their soil fertility and other land use. Based on their historical eruptions noted since and before 1600 A.D., the Indonesian active volcanoes are regrouped in to A type (79 volcanoes), which were defi ned as volcanoes erupted since 1600 A.D., B type (29 volcanoes) erupted before 1600 A.D., and C type (21 volcanoes) are solfatar fi elds (Bemmelen, 1949; van Padang 1951; Kusumadinata, 1979). Studies on parts of the Indonesian active volcanoes, show different eruptive characters, which are generally related to hazard potentials. A new classifi cation of Indonesian active volcanoes was proposed based on the combination of their physical properties, morphology, volcanic structure and eruptive styles to the eight differents types, those are Tambora (caldera formation), Merapi (lava dome), Agung (open crater), Papandayan (sector failure), Batur (post-caldera activities), Sangeangapi (lava fl ows) and Anak Krakatau types (volcano islands and submarine volcano).</em></p> <p><em>Thi</em><em>s classification would be make a better understanding to different characteristics of Indonesian active volcanoes, for the volcanic hazard and mitigation and also for the applied volcanological researches.</em></p> <p> </p>
topic Indonesian active volcanoes
characteristics
classification
volcanic hazard mitigation
url https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/23
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