砥川溶岩について

• 松本 幡郎

  熊本大本理学部

書誌事項

タイトル別名

• The Source Volcano of Togawa Lava, Near Kumamoto City
• トガワ ヨウガン ニ ツイテ

抄録

The greater parts of aphanitic dark grey Togawa lava occur in underground. Its areal distribution is estimated about 40 km² mainly by boring data. Akai volcano is the source of Togawa lava and mainly consists of reddish scoria. It has a crater about 0.5km, across, the floor of which is cultivated. Akai volcano has first erupted a lava flow and then formed a small cinder cone. Akai volcano is closely connected with the neighbouring Oomine volcano in types of volcanic structure and eruptive activity. Akai and Oomine volcanoes may be regarded as parasitic cones of Aso gigantic caldera volcano.

収録刊行物

• 火山.第２集

  火山.第２集 19 (1), 19-24, 1974

  特定非営利活動法人 日本火山学会

詳細情報

• CRID: 1390001206120327808
• NII論文ID: 110002995539
• NII論文ID: 10004564327
• NII書誌ID: AN10512786
• ISSN: 04534360
• ISSN: 24330590
• DOI: 10.18940/kazanc.19.1_19
• NDL書誌ID: 7515022
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I7515022
• 本文言語コード: ja
• データソース種別:
  • JaLC
  • NDL
  • CiNii Articles
• 抄録ライセンスフラグ: 使用不可