Stress control of deep rift intrusion at Mauna Loa volcano, Hawaii

Falk Amelung, Sang Ho Yun, Thomas R. Walter, Paul Segall, Sang Wan Kim

Research output: Contribution to journalArticle

70 Scopus citations

Abstract

Mauna Loa volcano, Hawaii, deforms by a combination of shallow dike intrusions in the rift zones and earthquakes along the base of the volcano, but it is not known how the spreading is accommodated in the lower part of the volcanic edifice. We present evidence from interferometric synthetic aperture radar data for secular inflation of a dike-like magma body at intermediate depth in the southwest rift zone during 2002 to 2005. Magma accumulation occurred in a section of the rift zone that was undamped by previous dikes and earthquakes, suggesting that stress transfer plays an important role in controlling subsurface magma accumulation.

Original languageEnglish (US)
Pages (from-to)1026-1030
Number of pages5
JournalScience
Volume316
Issue number5827
DOIs
StatePublished - May 18 2007

ASJC Scopus subject areas

  • General

Fingerprint Dive into the research topics of 'Stress control of deep rift intrusion at Mauna Loa volcano, Hawaii'. Together they form a unique fingerprint.

  • Cite this

    Amelung, F., Yun, S. H., Walter, T. R., Segall, P., & Kim, S. W. (2007). Stress control of deep rift intrusion at Mauna Loa volcano, Hawaii. Science, 316(5827), 1026-1030. https://doi.org/10.1126/science.1140035