FLOWGO: a kinematic thermo-rheological model for lava flowing in a channel

Harris. (2001). FLOWGO: a kinematic thermo-rheological model for lava flowing in a channel. Bulletin of Volcanology.

Type

Journal article

Intellectual base

Primary research

Year

2001

DOI

10.1007/s004450000120

Link

https://doi.org/10.1007/s004450000120

Cited by

1 citation across 1 artifact.

Each citation links to the sentence it supports in the citing article.

Domain-specific

• Geological Lava Flow
  • The flow front stops when the available driving stress can no longer overcome its evolving yield strength and viscous resistance

    This sourceEstablishes the arrest condition quantitatively: FLOWGO couples downflow cooling and crystallization to rising viscosity and yield strength and resolves the point at which the flowing volume becomes stationary, giving the flow's maximum channel-fed length.

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