Slow-moving and far-travelled dense pyroclastic flows during the Peach Spring super-eruption
Pyroclastic flows of the 18.8 Ma Peach Spring Tuff super-eruption travelled >170 km and entrained substrate blocks up to ∼1 m diameter. Here, the authors show that these flows had a dense base and speeds of ∼5-20 m s−1, fed by an eruption discharging magma at rates up to ∼107-108 m3 s−1for at lea...
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| Autores principales: | , , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2016
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/bd1f5ed4262d4c17a9c9b273a4c85498 |
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| Sumario: | Pyroclastic flows of the 18.8 Ma Peach Spring Tuff super-eruption travelled >170 km and entrained substrate blocks up to ∼1 m diameter. Here, the authors show that these flows had a dense base and speeds of ∼5-20 m s−1, fed by an eruption discharging magma at rates up to ∼107-108 m3 s−1for at least 2.5-10 h. |
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