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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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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