Volcanic ash flow - kazan bairyu (English spelling) ash flow
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It is a high-temperature pyroclastic flow consisting mainly of volcanic ash. When large amounts of pyroclastic material and gas are erupted from a volcano, they can be found in the lower part of a thermal cloud (nuee ardente) [Fisher: 1954, MacGregor: 1955]. Source: Asakura Publishing Dictionary of Petrology Information |
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主として火山灰よりなる高温の火砕流である．大量の火山砕屑物とガスが火山から噴出することで，熱雲（nuee ardente）の下部に含まれることがある［Fisher : 1954, MacGregor : 1955］． 出典 朝倉書店岩石学辞典について 情報 |
>>: Volcanic Ash Chronology - Volcanic Ash Chronology
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