Multiple dikes make eruptions easy

Dikes supply magma to most volcanic eruptions. Understanding how propagating dikes may, or may not, reach the surface is thus one of the fundamental tasks for volcanology. Many, perhaps most, dike segments injected from magma sources do not reach the surface to feed volcanic eruptions. Instead, the dike segments become arrested (stop their propagation), commonly at or close to contacts between mechanically dissimilar layers/units, at various crustal depths. This means that many and perhaps most volcanic unrest periods with dike injections do not result in eruptions. There are several conditions that make dike arrest likely, but the main one is layering where the layers have contrasting mechanical properties. Such layering means that local stresses are heterogeneous and anisotropic and, therefore, in some layers unfavourable for dike propagation – hence the dike arrest. Here I show that once a dike has formed, however, its very existence tends to make the local stress field along the dike homogeneous (with invariable orientation of principal stresses) and favourable (with dike-parallel orientation of the maximum compressive principal stress) for later dike injections. This means that subsequence dikes may use an earlier dike as a path, either along the margin or the centre of the earlier dike, thereby generating a multiple dike. Because earlier feeder-dikes form potential paths for later-injected dikes to the surface, many volcanic eruptions are fed by multiple dikes. Examples include recent eruptions in the volcanoes Etna (Italy) and Kilauea (Hawaii), and the Icelandic volcanoes Krafla, Hekla, Fagradalsfjall, and the Sundhnukur crater row. Thus, multiple dikes favour dike propagation to the surface; thereby making dike-fed eruptions easier. • Dikes supply magma to most volcanic eruptions. • Many injected dikes never reach the surface to feed eruptions. • An existing dike may provide a preferred path for further dike injections. • The resulting multiple dike tends to make eruptions easier.

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Publication Details

Journal
Journal of Volcanology and Geothermal Research
Published
2025-02-04
DOI
https://doi.org/10.1016/j.jvolgeores.2025.108284
Citations
10
Primary Topic
Microwave Engineering and Waveguides
Type
article
Field-Weighted Citation Impact
7.30
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article

Multiple dikes make eruptions easy

Ágúst Guðmundsson
10 citations
Journal of Volcanology and Geothermal Research
Microwave Engineering and Waveguides
7.30
article

Multiple dikes make eruptions easy

Ágúst Guðmundsson
article en
10 citations

Abstract

Dikes supply magma to most volcanic eruptions. Understanding how propagating dikes may, or may not, reach the surface is thus one of the fundamental tasks for volcanology. Many, perhaps most, dike segments injected from magma sources do not reach the surface to feed volcanic eruptions. Instead, the dike segments become arrested (stop their propagation), commonly at or close to contacts between mechanically dissimilar layers/units, at various crustal depths. This means that many and perhaps most volcanic unrest periods with dike injections do not result in eruptions. There are several conditions that make dike arrest likely, but the main one is layering where the layers have contrasting mechanical properties. Such layering means that local stresses are heterogeneous and anisotropic and, therefore, in some layers unfavourable for dike propagation – hence the dike arrest. Here I show that once a dike has formed, however, its very existence tends to make the local stress field along the dike homogeneous (with invariable orientation of principal stresses) and favourable (with dike-parallel orientation of the maximum compressive principal stress) for later dike injections. This means that subsequence dikes may use an earlier dike as a path, either along the margin or the centre of the earlier dike, thereby generating a multiple dike. Because earlier feeder-dikes form potential paths for later-injected dikes to the surface, many volcanic eruptions are fed by multiple dikes. Examples include recent eruptions in the volcanoes Etna (Italy) and Kilauea (Hawaii), and the Icelandic volcanoes Krafla, Hekla, Fagradalsfjall, and the Sundhnukur crater row. Thus, multiple dikes favour dike propagation to the surface; thereby making dike-fed eruptions easier. • Dikes supply magma to most volcanic eruptions. • Many injected dikes never reach the surface to feed eruptions. • An existing dike may provide a preferred path for further dike injections. • The resulting multiple dike tends to make eruptions easier.

Journal of Volcanology and Geothermal ResearchVol. 460
Royal Holloway University of London (GB)
Climate action
Openalex Percentile: Top 3%
Microwave Engineering and Waveguides
7.30
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