Deep Magma Body Beneath the Summit and Rift Zones of Kilauea Volcano, Hawaii

• Published in: Science (American Association for the Advancement of Science) Vol. 247; no. 4948; pp. 1311 - 1316
• Main Authors: Delaney, Paul T., Fiske, Richard S., Miklius, Asta, Okamura, Arnold T., Sako, Maurice K.
• Format: Journal Article
• Language: English
• Published: United States American Society for the Advancement of Science 16.03.1990; American Association for the Advancement of Science; The American Association for the Advancement of Science
• Subjects: Calderas; Earthquakes; Fault lines; Geology; Hawaii; Inflation rates; Lava; Magma; Research Article; Rifts (Geology); Subsidence; Topographical elevation; Volcanoes; Volcanology; Hawaii; Kilauea; United States > US; Mauna Loa
• ISSN: 0036-8075; 1095-9203
• DOI: 10.1126/science.247.4948.1311

A magnitude 7.2 earthquake in 1975 caused the south flank of Kilauea Volcano, Hawaii, to move seaward in response to slippage along a deep fault. Since then, a large part of the volcano's edifice has been adjusting to this perturbation. The summit of Kilauea extended at a rate of 0.26 meter per year until 1983, the south flank uplifted more than 0.5 meter, and the axes of both the volcano's rift zones extended and subsided; the summit continues to subside. These ground-surface motions have been remarkably steady and much more widespread than those caused by either recurrent inflation and deflation of the summit magma chamber or the episodic propagation of dikes into the rift zones. Kilauea's magmatic system is, therefore, probably deeper and more extensive than previously thought; the summit and both rift zones may be underlain by a thick, near vertical dike-like magma system at a depth of 3 to 9 kilometers.