Research Article| December 01, 1986 Possible effect of aspect ratios of magma chambers on eruption frequency Ågúst Gudmundsson Ågúst Gudmundsson 1Nordic Volcanological Institute, University of Iceland, 101 Reykjavík, Iceland Search for other works by this author on: GSW Google Scholar Author and Article Information Ågúst Gudmundsson 1Nordic Volcanological Institute, University of Iceland, 101 Reykjavík, Iceland Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1986) 14 (12): 991–994. https://doi.org/10.1130/0091-7613(1986)14<991:PEOARO>2.0.CO;2 Article history First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Ågúst Gudmundsson; Possible effect of aspect ratios of magma chambers on eruption frequency. Geology 1986;; 14 (12): 991–994. doi: https://doi.org/10.1130/0091-7613(1986)14<991:PEOARO>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The eruption frequency of volcanoes, even within the same region, is highly variable. In volcanic regions associated with stress fields that are essentially uniform (but anisotropic), as at plate boundaries, the explanation for the range in eruption frequency must lie within the volcanic systems themselves. I propose that differences in eruption frequency of volcanoes within the same volcanic region may be due to different aspect ratios of the magma chambers that feed the volcanoes. For a magma chamber of elliptical cross section with half-height h and half-width w, the higher the h/w ratio the more frequent will be the eruptions. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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Ágúst Guðmundsson (1986) studied this question.
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