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1984 | OriginalPaper | Buchkapitel

Subaerial Fallout Tephra

verfasst von : Professor Richard V. Fisher, Professor Hans-Ulrich Schmincke

Erschienen in: Pyroclastic Rocks

Verlag: Springer Berlin Heidelberg

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The transport modes of subaerial fallout tephra are (1) by ballistic trajectory and (2) by turbulent suspension. Energy is supplied initially to fragments by the eruption and later by wind. Tephra that falls from the atmosphere onto land is called subaerial fallout or airfall tephra. Tephra deposited in standing water is called subaqueous fallout tephra and includes (1) submarine or marine tephra, and (2) sub- lacustrine tephra. Subaqueous fallout tephra originating from eruptions on land is discussed separately (Chap. 7) from pyroclastic materials originating wholly beneath water (Chap. 10). Island arc and oceanic island flank environments generally include both kinds.

Metadaten
Titel
Subaerial Fallout Tephra
verfasst von
Professor Richard V. Fisher
Professor Hans-Ulrich Schmincke
Copyright-Jahr
1984
Verlag
Springer Berlin Heidelberg
DOI
https://doi.org/10.1007/978-3-642-74864-6_6