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  1. 広島大学の刊行物
  2. Journal of science of the Hiroshima University. Series C, Earth and planetary sciences
  3. 10巻4号

Risk Link to the Volcanic Activity of the Mt. Cameroon in Cameroon

https://doi.org/10.15027/53155
https://doi.org/10.15027/53155
24395dbd-95fa-46bc-bd09-6f09b3502432
名前 / ファイル ライセンス アクション
JSHUCE_10-4_593.pdf JSHUCE_10-4_593.pdf (1.4 MB)
Item type デフォルトアイテムタイプ_(フル)(1)
公開日 2023-03-18
タイトル
タイトル Risk Link to the Volcanic Activity of the Mt. Cameroon in Cameroon
言語 en
作成者 WOUATONG, Armand

× WOUATONG, Armand

en WOUATONG, Armand

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TCHOUA, Felix M.

× TCHOUA, Felix M.

en TCHOUA, Felix M.

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KITAGAWA, Ryuji

× KITAGAWA, Ryuji

en KITAGAWA, Ryuji

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TAKENO, Setsuo

× TAKENO, Setsuo

en TAKENO, Setsuo

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アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
内容記述
内容記述 The Mt. Cameroon is a large volcanic horst belonging to the majure tectonic line (Cameroon volcanic line). The geographical morphology of the mountain is controlled by regional tectonics. The Mt. Cameroon is consisted of precambrian metamorphic basement covered with Cretaceous to recent sediments distributed mainly in the Douala and Riodel Rey basin. The oldest lava could be of upper Miocene age. The Mt. Cameroon has erupted six times in the 20th century. The 1982 eruption took place inside the crater of an ancient cone. The lavas are picrites (with forsteritic olivine phenocrysts), alkali basalts (with salitic augite phenocrysts), hawaiites (with labrador-bytownite plagioclase phenocrysts) and mugearites (with scarce kaersutite phenocrysts and microlitic phlogopite or nosean). According to Deruelle et al.(1987), the Mt. Cameroon lava series is typically alkaline with no tholeiitic or transitional trend. Risk related to volcanism is actual for the human constructions especially along the axis of the horst. The severe volcanic risk has been limited to explosion, lava flows and lahar. It is possibility that explosion, laver flow and earthquarke take place anywhere on the volcanic mountain. Nevertheless, these explosions are most likely to occur in the delimited sector which is shown in a map presented in this paper. Even if we could divert the course of the lava flows to certain safer direction, flows caused by sudden earthquarke and explosion may cause serious damages.
言語 en
出版者
出版者 Hiroshima University
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ departmental bulletin paper
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
ID登録
ID登録 10.15027/53155
ID登録タイプ JaLC
収録物識別子
収録物識別子タイプ ISSN
収録物識別子 0075-4374
収録物識別子
収録物識別子タイプ NCID
収録物識別子 AA11095875
開始ページ
開始ページ 593
書誌情報 Journal of science of the Hiroshima University. Series C, Earth and planetary sciences
Journal of science of the Hiroshima University. Series C, Earth and planetary sciences

巻 10, 号 4, p. 593-605, 発行日 1996-08-07
旧ID 53155
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