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Tim R. Orr

United States Geological Survey

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M. R. Patrick

United States Geological Survey

B. F. Houghton

University of Hawaii System

Donald A. Swanson

The University of Texas MD Anderson Cancer Center

M. P. Poland

United States Geological Survey

Rebecca Carey

University of Tasmania

Jacopo Taddeucci

Istituto Nazionale di Geofisica e Vulcanologia

David Fee

University of Alaska Fairbanks

Piergiorgio Scarlato

Istituto Nazionale di Geofisica e Vulcanologia

A. J. Sutton

Christian Brothers University

A. Miklius

United States Geological Survey

Cooperative Institutions

United States Geological Survey

Hawaiian Volcano Observatory

University of Hawaiʻi at Mānoa

Cascades Volcano Observatory

Alaska Volcano Observatory

University of Hawaii System

University of Hawaii at Hilo

Volcano Science Center

Istituto Nazionale di Geofisica e Vulcanologia

University of Alaska Fairbanks

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Techniques for constraining short term eruptive processes at Kilauea's Overlook Vent

A. J. Sutton Tamar Elias H. Garbeil K. A. Horton Christoph Kern

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Citations (2)

Dimmuborgir: a rootless shield complex in northern Iceland

Bulletin of Volcanology (2016)

Alasdair Skelton Erik Sturkell Martin Jakobsson D. Einarsson Elin Tollefsen

Shield volcano

Lava dome

Lava field

Shields

10.1007/s00445-016-1032-5

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Citations (4)

Sinuous Ridges and Plateaus as Evidence for Lava Flow Inflation in the Tharsis Plains of Mars: Insights from Analogous Features on the Coastal Plain of Kilauea Volcano, HI

J. E. Bleacher Tim R. Orr W. B. Garry Christopher W. Hamilton J. R. Zimbelman

Tharsis

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Chronology-based Physical Volcanology of the 2011 Kamoamoa Eruption of Kilauea

C. E. Parcheta Tim R. Orr B. F. Houghton

Volcanology

Chronology

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A Tale of Two Reservoirs: Kı̄lauea's April-May 2015 Events

I. A. Johanson A. Miklius K. R. Anderson Tim R. Orr M. R. Patrick

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Pre-existing ground cracks as lava flow pathways at Kīlauea in 2014

Bulletin of Volcanology (2024)

Tim R. Orr Edward W. Llewellin K. R. Anderson M. R. Patrick

10.1007/s00445-024-01725-9

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Componentry of pyroclastic fall deposits from 2008-2012 small explosive eruptions at Kilauea summit crater: insights into the dynamics of an open basaltic lava column

AGU Fall Meeting Abstracts (2012)

Julia Eychenne B. F. Houghton David A. Swanson Tim R. Orr Rebecca Carey

Summit

Strombolian eruption

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A review of controls on lava lake level: insights from Halema‘uma‘u Crater, Kīlauea Volcano

Bulletin of Volcanology (2019)

M. R. Patrick Donald A. Swanson Tim R. Orr

Outgassing

Lateral eruption

Scoria

10.1007/s00445-019-1268-y

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Citations (35)

Characterizing active volcanic processes at Kilauea volcano using LiDAR scanning

AGU Fall Meeting Abstracts (2012)

A. L. LeWinter D. C. Finnegan M. R. Patrick Scott A. Anderson Tim R. Orr

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Primitive Components, Crustal Assimilation, and Magmatic Degassing During the Early 2008 Kīlauea Summit Eruptive Activity

Geophysical monograph (2015)

Michael C. Rowe Carl R. Thornber Tim R. Orr

Simultaneous summit and rift zone eruptions at Kīlauea starting in 2008 reflect a shallow eruptive plumbing system inundated by a bourgeoning supply of new magma from depth. Olivine-hosted melt inclusions, host glass, and bulk lava compositions of magma that erupted at both the summit and East Rift Zone demonstrate chemical continuity at both ends of a well-worn summit-to-rift pipeline. Analysis of glass within dense-cored lapilli that erupted from the summit in March–August 2008 show these are not samplings of compositionally distinct magmas stored in the shallow summit magma reservoir, but instead result from remelting and assimilation of fragments from conduit wall and vent blocks. Summit pyroclasts show the predominant and most primitive component erupted to be a homogenous, relatively trace-element-depleted melt that is compositionally indistinguishable from East Rift Zone lava. Based on a "top-down" model for the geochemical variation in East Rift Zone lava over the past 30 years, we suggest that the apparent absence of a 1982 enriched component in melt inclusions, as well as the proposed summit–rift zone connectivity based on sulfur and mineral chemistry, indicate that the last of the pre-1983 magma has been flushed out of the summit reservoir during the surge of mantle-derived magma from 2003 to 2007.

Rift zone

Magma chamber

Summit

Melt inclusions

10.1002/9781118872079.ch20

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Citations (12)

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