Modeling volcano growth on the Island of Hawaii: Deep-water perspectives

Recent ocean-bottom geophysical surveys, dredging, and dives, which complement surface data and scientific drilling at the Island of Hawaii, document that evolutionary stages during volcano growth are more diverse than previously described. Based on combining available composition, isotopic age, and geologically constrained volume data for each of the component volcanoes, this overview provides the first integrated models for overall growth of any Hawaiian island. In contrast to prior morphologic models for volcano evolution (preshield, shield, postshield), growth increasingly can be tracked by age and volume (magma supply), defining waxing alkalic, sustained tholeiitic, and waning alkalic stages. Data and estimates for individual volcanoes are used to model changing magma supply during successive compositional stages, to place limits on volcano life spans, and to interpret composite assembly of the island. Volcano volumes vary by an order of magnitude; peak magma supply also varies sizably among edifices but is challenging to quantify because of uncertainty about volcano life spans. Three alternative models are compared: (1) near-constant volcano propagation, (2) near-equal volcano durations, (3) high peak-tholeiite magma supply. These models define inconsistencies with prior geodynamic models, indicate that composite growth at Hawaii peaked ca. 800–400 ka, and demonstrate a lower current rate. Recent age determinations for Kilauea and Kohala define a volcano propagation rate of 8.6 cm/yr that yields plausible inception ages for other volcanoes of the Kea trend. In contrast, a similar propagation rate for the less-constrained Loa trend would require inception of Loihi Seamount in the future and ages that become implausibly large for the older volcanoes. An alternative rate of 10.6 cm/yr for Loa-trend volcanoes is reasonably consistent with ages and volcano spacing, but younger Loa volcanoes are offset from the Kea trend in age-distance plots. Variable magma flux at the Island of Hawaii, and longer-term growth of the Hawaiian chain as discrete islands rather than a continuous ridge, may record pulsed magma flow in the hotspot/plume source.

[1]  P. Renne,et al.  The 40Ar/39Ar and K/Ar dating of lavas from the Hilo 1‐km core hole, Hawaii Scientific Drilling Project , 1996 .

[2]  D. Swanson.  Magma Supply Rate at Kilauea Volcano, 1952-1971 , 1972, Science.

[3]  E. Wolfe,et al.  Geologic map of the Island of Hawaii , 1996 .

[4]  P. Renne,et al.  The 40Ar/39Ar dating of core recovered by the Hawaii Scientific Drilling Project (phase 2), Hilo, Hawaii , 2005 .

[5]  D. Clague,et al.  Volcano growth and evolution of the island of Hawaii , 1992 .

[6]  Submarine landslides and volcanic features on Kohala and Mauna Kea volcanoes and the hana ridge, Hawaii , 2013 .

[7]  D. Clague,et al.  Growth and degradation of Hawaiian volcanoes: Chapter 3 in Characteristics of Hawaiian volcanoes , 2014 .

[8]  P. Lipman.  Rates of volcanic activity along the southwest rift zone of Mauna Loa volcano, Hawaii , 1980 .

[9]  P. Lipman.  Declining Growth of Mauna Loa During the Last 100,000 Years: Rates of Lava Accumulation vs. Gravitational Subsidence , 2013 .

[10]  D. Clague,et al.  Geology and petrology of Mahukona Volcano, Hawaii , 1991 .

[11]  Kenneth R. Ludwig,et al.  Crustal subsidence rate off Hawaii determined from 234U/238U ages of drowned coral reefs , 1991 .

[12]  John J. Dvorak,et al.  Recent Inflation and Flank Movement of Mauna Loa Volcano , 2013 .

[13]  H. Stearns.  Geology of the Hawaiian islands , 1946 .

[14]  D. Clague,et al.  Postshield stage transitional volcanism on Mahukona Volcano, Hawaii , 2009 .

[15]  Michael O. Garcia,et al.  Magmatic history of the East Rift Zone of Kilauea Volcano, Hawaii based on drill core from SOH 1 , 2000 .

[16]  J. M. Rhodes,et al.  Olivine‐Rich Submarine Basalts from the Southwest Rift Zone of Mauna Loa Volcano: Implications for Magmatic Processes and Geochemical Evolution , 2013 .

[17]  Guangping Xu,et al.  Compositional diversity of Mauna Kea shield lavas recovered by the Hawaii Scientific Drilling Project: Inferences on source lithology, magma supply, and the role of multiple volcanoes , 2012 .

[18]  D. Dzurisin,et al.  Variations in magma supply rate at Kilauea Volcano, Hawaii , 1993 .

[19]  D. Clague,et al.  Subsidence and volcanism of the Haleakala Ridge, Hawaii , 1990 .

[20]  J. Sinton,et al.  Geologic map of the state of Hawai`i , 2007 .

[21]  J. Naka,et al.  Hawaiian Volcanoes: Deep Underwater Perspectives , 2002 .

[22]  D. Clague,et al.  Diverse basalt types from Loihi seamount, Hawaii , 1982 .

[23]  Dieterich,et al.  High magma storage rates before the 1983 eruption of kilauea, hawaii , 2000, Science.

[24]  G. A. Macdonald,et al.  Chemical Composition of Hawaiian Lavas1 , 1964 .

[25]  J. Lockwood,et al.  Geologic Map of the Summit Region of Kïlauea Volcano, Hawaii , 2003 .

[26]  D. Clague,et al.  Coastal lava flows from Mauna Loa and Hualalai volcanoes, Kona, Hawaii , 1987 .

[27]  J. Murray,et al.  A sagging-spreading continuum of large volcano structure , 2013 .

[28]  Kenneth L. Pierce,et al.  Is the track of the Yellowstone hotspot driven by a deep mantle plume? - Review of volcanism, faulting, and uplift in light of new data , 2009 .

[29]  P. Lipman,et al.  Mauna Loa lava accumulation rates at the Hilo drill site: Formation of lava deltas during a period of declining overall volcanic growth , 1996 .

[30]  J. M. Rhodes,et al.  Temporal Geochemical Evolution of Kilauea Volcano: Comparison of Hilina and Puna Basalt , 2013 .

[31]  Michael P. Poland,et al.  A mantle-driven surge in magma supply to Kīlauea Volcano during 2003–2007 , 2012 .

[32]  Michael O. Garcia,et al.  Rapid passage of a small-scale mantle heterogeneity through the melting regions of Kilauea and Mauna Loa Volcanoes , 2006 .

[33]  F. Klein,et al.  Deep magma transport at Kilauea volcano, Hawaii , 2006 .

[34]  J. P. Kauahikaua,et al.  Emplacement and inflation of pahoehoe sheet flows: observations and measurements of active lava flows on Kilauea volcano, Hawaii , 1994 .

[35]  D. Dzurisin,et al.  Magma supply and storage at Kilauea volcano, Hawaii, 1956 1983 , 1984 .

[36]  D. DePaolo,et al.  Deep Drilling into a Mantle Plume Volcano: The Hawaii Scientific Drilling Project , 2009 .

[37]  D. Swanson,et al.  Keanakākoʻi Tephra produced by 300 years of explosive eruptions following collapse of Kīlauea's caldera in about 1500 CE , 2012 .

[38]  J. M. Rhodes,et al.  Isotopic Evolution of Mauna Loa Volcano: A View From the Submarine Southwest Rift Zone , 2013 .

[39]  E. Wolfe.  The Puu Oo eruption of Kilauea Volcano, Hawaii; episodes 1 through 20, January 3, 1983, through June 8, 1984 , 1988 .

[40]  G. Walker.  Koolau Dike Complex, Oahu: Intensity and origin of a sheeted-dike complex high in a Hawaiian volcanic edifice , 1986 .

[41]  Dominique Weis,et al.  Role of the deep mantle in generating the compositional asymmetry of the Hawaiian mantle plume , 2011 .

[42]  J. Naka,et al.  Ancestral submarine growth of kïlauea volcano and instability of its south flank , 2013 .

[43]  Michael O. Garcia,et al.  Evolution of Mauna Kea Volcano, Hawaii: Petrologic and geochemical constraints on postshield volcanism , 1990 .

[44]  Kenneth G. Dueker,et al.  Hot mantle upwelling across the 660 beneath Yellowstone , 2012 .

[45]  John P. Lockwood,et al.  Mauna Loa Eruptive History—The Preliminary Radiocarbon Record , 2013 .

[46]  Deborah K. Smith,et al.  Petrological Systematics of Submarine Basalt Glasses from the Puna Ridge, Hawai'i: Implications for Rift Zone Plumbing and Magmatic Processes , 2013 .

[47]  J. Naka,et al.  Submarine Alkalic Through Tholeiitic Shield-Stage Development of KīLauea Volcano, Hawai'i , 2013 .

[48]  W. T. Kinoshita.  A Gravity Survey of the Island of Hawaii , 1965 .

[49]  G. A. Macdonald,et al.  Geology of the Hawaiian Islands@@@Geology and Ground-Water Resources of the Island of Hawaii , 1947 .

[50]  D. Sherrod,et al.  New K-Ar ages and the geologic evidence against rejuvenated-stage volcanism at Haleakalā, East Maui, a postshield-stage volcano of the Hawaiian island chain , 2003 .

[51]  J. M. Rhodes,et al.  Intershield geochemical differences among Hawaiian volcanoes: implications for source compositions, melting process and magma ascent paths , 1993, Philosophical Transactions of the Royal Society of London. Series A: Physical and Engineering Sciences.

[52]  J. Bryce,et al.  Isotopic evolution of Mauna Loa and the chemical structure of the Hawaiian plume , 2001 .

[53]  C. Wolfe,et al.  Coupling at Mauna Loa and Kīlauea by stress transfer in an asthenospheric melt layer , 2012 .

[54]  P. Lipman,et al.  Growth history of Kilauea inferred from volatile concentrations in submarine-collected basalts , 2006 .

[55]  G. B. Dalrymple,et al.  THE GEOLOGY AND PETROLOGY OF MAUNA KEA VOLCANO, HAWAII : A STUDY OF POSTSHIELD VOLCANISM , 1997 .

[56]  J. M. Rhodes,et al.  40Ar/39Ar geochronology of submarine Mauna Loa volcano, Hawaii , 2009 .

[57]  M. Poland,et al.  Magma supply, storage, and transport at shield-stage Hawaiian volcanoes: Chapter 5 in Characteristics of Hawaiian volcanoes , 2014 .

[58]  J. Rhodes,et al.  Composition of basaltic lavas sampled by phase‐2 of the Hawaii Scientific Drilling Project: Geochemical stratigraphy and magma types , 2004 .

[59]  T. Sisson,et al.  Source materials for inception stage Hawaiian magmas: Pb‐He isotope variations for early Kilauea , 2010 .

[60]  Fred W. Klein,et al.  Patterns of historical eruptions at Hawaiian volcanoes , 1982 .

[61]  D. Clague,et al.  Slope failure and volcanic spreading along the submarine south flank of Kilauea volcano, Hawaii , 2003 .

[62]  Michael O. Garcia,et al.  Age, geology, geophysics, and geochemistry of Mahukona Volcano, Hawai`i , 2012, Bulletin of Volcanology.

[63]  D. Clague.  Hawaiian xenolith populations, magma supply rates, and development of magma chambers , 1987 .

[64]  Michael O. Garcia,et al.  Glass in the submarine section of the HSDP2 drill core, Hilo, Hawaii , 2004 .

[65]  J. Lockwood,et al.  The Uwekahuna Ash Member of the Puna Basalt: product of violent phreatomagmatic eruptions at Kilauea volcano, Hawaii, between 2800 and 210014C years ago , 1995 .

[66]  G. B. Dalrymple,et al.  The tholeiite to alkalic basalt transition at Haleakala Volcano, Maui, Hawaii , 1991 .

[67]  G. B. Dalrymple,et al.  The Ninole Basalt — Implications for the structural evolution of Mauna Loa volcano, Hawaii , 1990 .

[68]  J. Naka,et al.  Deep‐Sea Volcaniclastic Sedimentation Around the Southern Flank of Hawaii , 2013 .

[69]  J. M. Rhodes,et al.  Episodic Trace Element and Isotopic Variations in Historical Mauna Loa Lavas: Implications for Magma and Plume Dynamics , 2013 .

[70]  T. L. Wright.  Chemistry of Kilauea and Mauna Loa lava in space and time , 1971 .

[71]  P. Cervelli,et al.  Vulcanology: Interaction between Kilauea and Mauna Loa , 2003, Nature.

[72]  D. Swanson,et al.  Potassium-Argon Ages of Lavas from the Hawi and Pololu Volcanic Series, Kohala Volcano, Hawaii , 1972 .

[73]  J. Morgan,et al.  Rift zone abandonment and reconfiguration in Hawaii: Mauna Loa's Ninole rift zone , 2010 .

[74]  H. Guillou,et al.  Unspiked K–Ar dating of Pleistocene tholeiitic basalts from the deep core SOH-4, Kilauea, Hawaii , 1997 .

[75]  B. Eakins,et al.  Calculated volumes of individual shield volcanoes at the young end of the Hawaiian Ridge , 2003 .

[76]  D. DePaolo,et al.  Models of Hawaiian volcano growth and plume structure: Implications of results from the Hawaii Scientific Drilling Project , 1996 .

[77]  F. Albarède,et al.  Mixing of isotopic heterogeneities in the Mauna Kea plume conduit , 2009 .

[78]  Michael O. Garcia,et al.  Mahukona: The missing Hawaiian volcano , 1990 .

[79]  D. DePaolo,et al.  Introduction to Special Section: Hawaii Scientific Drilling Project , 1996 .

[80]  P. Lipman,et al.  Piggyback tectonics: Long-term growth of Kilauea on the south flank of Mauna Loa , 2006 .

[81]  D. Swanson,et al.  Kulanaokuaiki Tephra (ca, A.D. 400-1000): Newly recognized evidence for highly explosive eruptions at Kilauea Volcano, Hawai'i , 2009 .

[82]  W. Normark,et al.  Reef growth and volcanism on the submarine southwest rift zone of Mauna Loa, Hawaii , 1990 .

[83]  Michael O. Garcia,et al.  Geochemical and Isotopic Evolution of Loihi Volcano, Hawaii , 1996 .

[84]  M. Lanphere,et al.  Geochemical evolution of Kohala Volcano, Hawaii , 1987 .

[85]  E. D. Jackson,et al.  Orientation and growth of Hawaiian volcanic rifts: the effect of regional structure and gravitational stresses , 1972, Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences.

[86]  P. Lipman,et al.  Early growth of Kohala volcano and formation of long Hawaiian rift zones , 2011 .

[87]  G. B. Dalrymple,et al.  Hawaiian-Emperor Chain and Its Relation to Cenozoic Circumpacific Tectonics , 1972 .

[88]  B. Eakins,et al.  Submarine geology of Hana Ridge and Haleakala Volcano's northeast flank, Maui , 2006 .

[89]  Kitty L. Milliken,et al.  Mauna Loa's submarine western flank: Landsliding, deep volcanic spreading, and hydrothermal alteration , 2007 .

[90]  U. Christensen,et al.  The dynamical origin of Hawaiian volcanism , 1999 .

[91]  J. Campbell,et al.  Age of tilted reefs, Hawaii , 1987 .

[92]  D. Clague,et al.  Chronology, chemistry, and origin of trachytes from Hualalai Volcano, Hawaii , 2003 .

[93]  M. Lanphere,et al.  Argon geochronology of Kilauea's early submarine history , 2006 .

[94]  Michael O. Garcia,et al.  Unspiked K-Ar dating of young volcanic rocks from Loihi and Pitcairn hot spot seamounts , 1997 .

[95]  J. Caplan‐Auerbach,et al.  Geology, Geochemistry and Earthquake History of Lṑihi Seamount, Hawaìi's Youngest Volcano , 2006 .

[96]  J. M. Rhodes,et al.  Shield-stage alkalic volcanism on Mauna Loa Volcano, Hawaii , 2006 .

[97]  D. Clague,et al.  Petrology of submarine lavas from Kilauea''s Puna ridge , 1995 .

[98]  J. C. Rose,et al.  An Analysis of the Gravity Field Over the Hawaiian Islands in Terms of Crustal Structure , 1965 .

[99]  Michael O. Garcia,et al.  A Rapid Fluctuation in the Mantle Source and Melting History of Kilauea Volcano Inferred from the Geochemistry of its Historical Summit Lavas (1790–1982) , 1999 .

[100]  G. B. Dalrymple,et al.  Argon-40: Excess in Submarine Pillow Basalts from Kilauea Volcano, Hawaii , 1968, Science.

[101]  T. Hildenbrand,et al.  Deep magmatic structures of Hawaiian volcanoes, imaged by three-dimensional gravity models , 2000 .