Abstract
Deep-sea limu o Pele are shards of basaltic glass commonly described as “bubble walls.” When first identified they were inferred to form in submarine fire fountains, but were then reinterpreted as the products of hydrovolcanic volcanism, formed when submarine lava flows entrapped and vaporised seawater. Limu discovered below the c 3 km critical depth of seawater, where superheated water exists as a supercritical fluid instead of a vapour, led to the hydrovolcanic model of limu o Pele formation being discarded in favour of a magmatic CO2-driven, “strombolian-like” model. This revised magmatic mechanism has been widely accepted by the scientific community. We describe a newly discovered limu o Pele-rich deposit at ~1,052 mbsl on the northeast summit plateau region of Lō`ihi Seamount, Hawai`i. The limu at this site is concentrated in a chemically monomict ash lens interbedded with thin lava sheets that are separated from overlying volcaniclastic material by a discontinuity. The geometry and geochemistry of the deposit provide compelling evidence for a hydrovolcanic, sheet flow-related origin. The exceptional abundance and preservation of limu at this site allows 4 morphologic subtypes of limu- thin film, plateau-border, convex film, and Pele’s hair- to be identified and linked to portions of the isolated rupturing bubbles from which they are derived. We extend our discussion to beyond this new Lō`ihi deposit, by including a review of limu o Pele occurrences and thermodynamic considerations that demonstrate the hydrovolcanic model of limu formation to be more tenable than the magmatic model at all depths, including below the critical depth of seawater.
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References
Arai Y, Sako T, Takebayashi Y (eds) (2002) Supercritical fluids: molecular interactions, physical properties, and new applications. Springer-Verlag, Berlin
Batiza R, Fornari DJ, Vanko DA, Lonsdale P (1984) Craters, calderas and hyaloclastites on young Pacific seamounts. J Geophys Res 89:8371–8390
Bischoff JL, Rosenbauer RJ (1988) An empirical equation of state for hydrothermal seawater. Am J Sci 285:725–763
Blackburn EA, Wilson L, Sparks RSJ (1976) Mechanisms and dynamics of strombolian activity. J Geol Soc (Lond) 132:429–440
Burton M, Allard P, Muré F, La Spina A (2007) Magmatic gas composition reveals the source depth of slug-driven strombolian explosive activity. Science 317:227–230
Büttner R, Dellino P, Zimanowski B (1999) Identifying magma-water interaction from the surface features of ash particles. Nature 401:688–690
Clague DA (2009) Accumulation rates of volcaniclastic deposits on Lo`ihi Seamount, Hawai`i. Bull Volcanol. doi:10.1007/s00445-009-0281-y
Clague DA, Davis AS, Bischoff JL, Dixon JE, Geyer R (2000) Lava bubble-wall fragments formed by submarine hydrovolcanic explosions on Lō`ihi Seamount and Kilauea Volcano. Bull Volcanol 61:437–449
Clague DA, Davis AS, Dixon JE (2003a) Submarine strombolian eruptions on the Gorda Mid-Ocean Ridge. In: White JDL, Smellie JL, Clague DA (eds) Explosive subaqueous volcanism. Am Geophys Union Geophys Mon 140:111–128
Clague DA, Batiza R, Head JWI, Davis AS (2003b) Pyroclastic and hydroclastic deposits on Lō`ihi Seamount, Hawai`i. In: White JDL, Smellie JL, Clague DA (eds) Explosive subaqueous volcanism. Am Geophys Union Geophys Mon 140:73–95
Clague DA, Paduan JB, Davis AS (2008) Widespread strombolian eruptions of mid-ocean ridge basalt. J Volcanol Geotherm Res 180:171–188. doi:10.1016/j.jvolgeores.2008.08.007
Davis AS, Clague DA (1998) Changes in the hydrothermal system at Lo`ihi Seamount after the formation of Pele’s pit in 1996. Geology 26:399–402
Davis AS, Clague DA (2003) Hyaloclastite from miocene seamounts offshore central California: compositions, eruption styles, and depositional processes. In: White JDL, Smellie JL, Clague DA (eds) Explosive subaqueous volcanism. Am Geophys Union Geophys Mon 140:129–142
Davis AS, Clague DA (2006) Volcaniclastic deposits from the North Arch volcanic field, Hawai`i: explosive fragmentation of alkalic lava at abyssal depths. Bull Volcanol 68:294–307
Debrégeas G, de Gennes P-G, Borchard-Wyart F (1998) The life and death of “bare” viscous bubbles. Science 279:1704–1707
Dhir VK (1998) Boiling heat transfer. Ann Rev Fluid Mech 30:365–401
Garcia MO, Rubin KH, Norman MD, Rhodes JM, Graham DW, Muenow DW, Spencer K (1998) Petrology and geochronology of basalt breccia from the 1996 earthquake swarm of Lō`ihi seamount, Hawai`i: magmatic history of its 1996 eruption. Bull Volcanol 59:577–592
Garcia MO, Caplan-Auerbach J, De Carlo EH, Kurz MD, Becker N (2006) Geology, geochemistry and earthquake history of Lō`ihi Seamount, Hawai`i’s youngest volcano. Chem Erde-Geochem 66:81–108
Grunewald U, Zimanowski B, Büttner R, Phillips LF, Heide K, Buchel G (2007) MFCI experiments on the influence of NaCl-saturated water on phreatomagmatic explosions. J Volcanol Geotherm Res 159:126–137
Helo C, Clague DA, Stix J (2008) Pyroclastic eruptions from Axial caldera, Juan de Fuca Ridge, NE Pacific Ocean. IOP Conf Ser. Earth Environ Sci 3:012005. doi:10.1088/1755-1307/3/1/012005
Hon K, Heliker C, Kjargaard JI (1988) Limu O Pele; a new kind of hydroclastic tephra from Kilauea Volcano, Hawai`i. Abstracts with Programs. Geol Soc Am 20(7):112–113
Honnorez J, Kirst P (1975) Submarine basaltic volcanism: morphometric parameters for discriminating hyaloclastites from hyalotuffs. Bull Volcanol 39:441–465
Hovland M, Kuznetsova T, Rueslatten H, Kvamme B, Johnsen HK, Fladmark GE, Hebach A (2006) Sub-surface precipitation of salts in supercritical seawater. Basin Res 18:221–230
Karl DM, McMurtry GM, Malahoff A, Garcia MO (1988) Lō`ihi Seamount, Hawai`i: a mid-plate volcano with a distinctive hydrothermal system. Nature 335:532–535
Kokelaar P (1986) Magma-water interactions in subaqueous and emergent basaltic volcanism. Bull Volcanol 48:275–289
Lemmon EW, McLinden MO, Friend DG (2008) Thermophysical properties of fluid systems. In: Linstrom PJ, Mallard WG (eds) NIST Chemistry WebBook, NIST Standard Reference Database Number 69, National Institute of Standards and Technology, Gaithersburg, http://webbook.nist.gov
Lō`ihi Science Team (1997) Rapid response to submarine activity at Lō`ihi Volcano, Hawai`i. EOS Trans Am Geophys Union 78:229–233
Lonsdale P, Batiza R (1980) Hyaloclastite and lava flows on young seamounts examined with a submersible. Geol Soc Am Bull 91:1545–1554
MacDonald GA, Katsura T (1964) Chemical composition of Hawaiian Lavas. J Petrol 5:82–133
Maicher D, White JDL (2001) The formation of deep-sea Limu o Pele. Bull Volcanol 63:482–496
Maicher D, White JDL, Batiza R (2000) Sheet hyaloclastite; density-current deposits of quench and bubble-burst fragments from thin, glassy sheet lava flows, Seamount Six, eastern Pacific Ocean. Mar Geol 17:75–94
Mangan MT, Cashman KV (1996) The structure of basaltic scoria and reticulite and inferences for vesiculation, foam formation, and fragmentation in lava fountains. J Volcanol Geotherm Res 73:1–18
Mastin LG (2007) Generation of fine hydromagmatic ash by growth and disintergration of glassy rinds. J Geophys Res 112:B02203. doi:10.1029/2005JB003883
Mattox TN, Mangan MT (1997) Littoral hydrovolcanic explosions: a case study of lava-seawater interaction at Kilauea volcano. J Volcanol Geotherm Res 75:1–17
Moore JG, Phillips RL, Grigg RW, Peterson DW, Swanson DA (1973) Flow of lava into the sea, 1961–1971, Kīlauea Volcano, Hawai`i. Geol Soc Am Bull 84:573–546
Moore JG, Clague DA, Normark WR (1982) Diverse basalt types from Lō`ihi seamount, Hawai`i. Geology 10:88–92
Morgan P (2006) Seawater: a library of MATLAB computational routines for the properties of seawater. Release 3.2. CSIRO Marine Research, Perth, http://www.cmar.csiro.au/datacentre/ext_docs/seawater.htm
Moune S, Faure F, Gauthier P-J, Sims K (2007) Pele’s hairs and tears: natural probe of volcanic plume. J Volcanol Geotherm Res 164:244–253
Nichols ARL, Potuzak M, Dingwell DB (2009) Cooling rates of basaltic hyaloclastites and pillow lava glasses from the HSDP2 drill core. Geochim Cosmochim Acta 73:1052–1066
Papale P (1999) Strain-induced magma fragmentation in explosive eruptions. Nature 397:425–428
Parfitt EA (2004) A discussion of the mechanisms of explosive basaltic eruptions. J Volcanol Geotherm Res 134:77–107
Perfit MR, Cann JR, Fornari DJ, Engels J, Smith DK, Ridley WI, Edwards MH (2003) Interaction of sea water and lava during submarine eruptions at mid-ocean ridges. Nature 426:62–65
Potuzak M, Nichols ARL, Dingwell DB, Clague DA (2008) Hyperquenched volcanic glasses from Lo`ihi Seamount, Hawai`i. Earth Planet Sci Lett 270:54–62
Sohn RA, Willis C, Humphris S, Shank TM, Singh H, Edmonds HN, Kunz C, Hedman U, Helmke E, Jakuba M, Liljebladh B, Linder J, Murphy C, Nakamura K, Sato T, Schlindwein V, Stranne C, Tausenfreund M, Upchurch L, Winsor P, Jakobsson M, Soule A (2008) Explosive volcanism on the ultraslow-spreading Gakkel ridge, Arctic Ocean. Nature 453:1236–1238. doi:10.1038/nature07075
Sourirajan S, Kennedy GC (1962) The system H2O-NaCl at elevated temperatures and pressures. Am J Sci 260:115–141
Tribble GW (1991) Underwater observations of active lava flows from Kīlauea volcano, Hawai`i. Geology 19:633–636
White JDL, Houghton BF (2006) Primary volcaniclastic rocks. Geology 34:677–680
Wilding M, Dingwell D, Batiza R, Wilson L (2000) Cooling rates of hyaloclastites: applications of relaxation geospeedometry to undersea volcanic deposits. Bull Volcanol 61:527–536
Wohletz KH (2003) Water/magma interaction: physical considerations for the deep submarine environment. In: White JDL, Smellie JL, Clague DA (eds) Explosive subaqueous volcanism. Am Geophys Union Geophys Mon 140:25–49
Acknowledgements
We thank J.R. Smith, T. Kirby and the HURL crew for their help in making the October 2006 dive series successful. D.A. Clague generously supplied limu samples for comparison. This work was funded by HURL, GNS Science, and the University of Otago. Thanks also to B.F. Houghton for hosting C.I.S. for extended study and use of facilities at the University of Hawai`i, to W.K. Stovall and R. Murtagh for helpful discussions, and to K.R. Higbee for perspective. Thorough reviews by D.A. Clague and an anonymous reviewer helped to significantly improve the paper.
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Schipper, C.I., White, J.D.L. No depth limit to hydrovolcanic limu o Pele: analysis of limu from Lō`ihi Seamount, Hawai`i. Bull Volcanol 72, 149–164 (2010). https://doi.org/10.1007/s00445-009-0315-5
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DOI: https://doi.org/10.1007/s00445-009-0315-5