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Chapter 1 - Understanding the physical behavior of volcanoes

Published online by Cambridge University Press:  14 November 2009

Steven N. Carey
Affiliation:
Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 02882, USA
Joan Marti
Affiliation:
Institut de Ciències de la Terra 'Jaume Almera', Barcelona
Gerald G. J. Ernst
Affiliation:
Universiteit Gent, Belgium
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Summary

Introduction

Volcanism is a spectacular display of the complex way in which energy and materials are exchanged between three major components of our planet: the solid Earth, oceans, and atmosphere. Mankind has long been both fascinated and terrified by erupting volcanoes. Yet throughout history people have been drawn to their fertile slopes and have developed a unique symbiosis. In many cultures, volcanoes symbolize a source of tremendous power that must be placated by worship or sacrifice. Volcanologists, on the other hand, strive to understand how volcanoes work in order to better predict their behaviour and reduce the hazards to people who live near them. But volcanoes are not merely destructive and need to be viewed as an integral part of the dynamic Earth system. They create new land, replenish soil, and provide essential water and other gases to our oceans and atmosphere. Much of this book will focus on the relationship of volcanoes to the environment and to mankind. However, before these topics are addressed we need to begin with some fundamental concepts about the causes and processes of volcanism. In this chapter we explore how volcanoes work by examining the complex path that must be taken before an eruption takes place at the Earth's surface. This includes the generation of magma at depth, its rise, storage and evolution within the Earth's crust, and finally the factors that determine the nature of the eruption at the surface.

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Publisher: Cambridge University Press
Print publication year: 2005

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References

Anderson, A. T. Jr., Newman, S., Williams, S., et al. 1989. H2O, CO2, Cl, and gas in Plinian and ash-flow Bishop rhyolite. Geology, 17, 221–2252.3.CO;2>CrossRefGoogle Scholar
Ballard, R. and Moore, J. 1977. Photographic Atlas of the Mid-Atlantic Ridge Rift Valley. Berlin, Springer-VerlagCrossRefGoogle Scholar
Ballard, R., Holcomb, R., and Andel, T. 1979. The Galapagos Rift at 86° W. III. Sheet flows, collapse pits, and lava lakes of the rift valley. Journal of Geophysical Research, 84, 5407–5422CrossRefGoogle Scholar
Barker, S. and Malone, S. 1991. Magmatic system geometry at Mount St. Helens modeled from the stress field associated with posteruptive earthquakes. Journal of Geophysical Research, 96, 11883–11894CrossRefGoogle Scholar
Blackburn, E., Wilson, L., and Sparks, R. S. J. 1976. Mechanisms and dynamics of strombolian activity. Journal of the Geological Society of London, 132, 429–440CrossRefGoogle Scholar
Blake, S. 1989. Viscoplastic models of lava domes. IAVCEI Proceedings in Volcanology, Lava Flows and Domes, 2, 88–126CrossRefGoogle Scholar
Bonadonna, C., Ernst, G. G. J., and Sparks, R. S. J. 1998. Thickness variations and volume estimates of tephra fall deposits: the importance of particle Reynolds number. Journal of Volcanology and Geothermal Research, 81, 173–187CrossRefGoogle Scholar
Bottinga, Y. and Weill, D. 1972. The viscosity of magmatic silicate liquids: a model for calculation. American Journal of Science, 272, 438–475CrossRefGoogle Scholar
Brown, G. C., Hawkesworth, C., and Wilson, M. 1992. Understanding the Earth. Cambridge, UK, Cambridge University PressGoogle Scholar
Brown, J., Colling, A., Park, D., et al. 1989. The Ocean Basins: Their Structure and Evolution. New York, Pergamon PressGoogle Scholar
Burnham, C. W. 1979. The importance of volatile constituents. In , H. Yoder (ed.) The Evolution of Igneous Rocks. Princeton,NJ, Princeton University Press, pp. 439–478Google Scholar
Bursik, M. and Woods, A. 1996. The dynamics and thermodynamics of large ash flows. Bulletin of Volcanology, 58, 175–193CrossRefGoogle Scholar
Bursik, M. I., Sparks, R. S. J., Gilbert, J. S., et al. 1992a. Sedimentation of tephra by volcanic plumes. II. Theory and its comparison with a study of the Fogo A plinian deposit, São Miguel (Azores). Bulletin of Volcanology, 54, 329–344CrossRefGoogle Scholar
Bursik, M., Carey, S., and Sparks, R. S. J. 1992b. A gravity current model for the May 18, 1980 Mount St. Helens plume. Geophysical Research Letters, 19, 1663–1666CrossRefGoogle Scholar
Carey, S. N. 1991. Transport and deposition of tephra by pyroclastic flows and surges. In , R. V. Fisher and , G. Smith (eds.) Sedimentation in Volcanic Settings, Special Publication no. 45. Tulsa, OK, Society for Sedimentary Geology, pp. 39–57Google Scholar
Carey, S. N. and Sigurdsson, H. 1985. The May 18, 1980 eruption of Mount St. Helens. II. Modeling of dynamics of the plinian phase. Journal of Geophysical Research, 90, 2948–2958CrossRefGoogle Scholar
Carey, S. N. and Sigurdsson, H. 1987. Temporal variations in column height and magma discharge rate during the 79 AD eruption of Vesuvius. Geological Society of America Bulletin, 99, 303–3142.0.CO;2>CrossRefGoogle Scholar
Carey, S. N. and Sparks, R. S. J. 1986. Quantitative models of the fallout and dispersal of tephra from volcanic eruption columns. Bulletin of Volcanology, 48, 109–125CrossRefGoogle Scholar
Carey, S. N., Sigurdsson, H., and Sparks, R. S. J. 1988. Experimental studies of particle-laden plumes. Journal of Geophysical Research, 93, 15314–15328CrossRefGoogle Scholar
Caroll, M. and Rutherford, M. 1988. Sulfur speciation in hydrous experimental glasses of varying oxidation state: results from measured wavelength shifts of sulfur x-rays. American Mineralogist, 73, 845–849Google Scholar
Carr, M. J. 1984. Symmetrical and segmented variation of physical and geochemical characteristics of the Central American volcanic front. Journal of Volcanology and Geothermal Research, 20, 231–252CrossRefGoogle Scholar
Cashman, K. and Mangan, M. 1994. Physical aspects of magma degassing. II. Constraints on vesiculation processes from textural studies of eruptive processes. Reviews in Mineralogy, 30, 447–474Google Scholar
Chadwick, W. and Embley, R. 1994. Lava flows from a mid-1980s submarine eruption on the Cleft segment, Juan de Fuca Ridge. Journal of Geophysical Research, 99, 4761–4776CrossRefGoogle Scholar
Chadwick, W., Embley, R., and Fox, C. 1995. SeaBeam depth changes associated with recent lava flows, CoAxial segment, Juan de Fuca Ridge: evidence for multiple eruptions between 1981–1993. Geophysical Research Letters, 22, 167–170CrossRefGoogle Scholar
Chesner, C. and Rose, W. I. 1991. Stratigraphy of the Toba Tuffs and evolution of the Toba caldera complex, Sumatra, Indonesia. Bulletin of Volcanology, 53, 343–356CrossRefGoogle Scholar
Chouet, B., Hamisevicz, N., and McGuetchin, T. R. 1974. Photoballistics of volcanic jet activity at Stromboli, Italy. Journal of Geophysical Research, 79, 4961–4976CrossRefGoogle Scholar
Clague, D. and Dalrymple, G. B. 1987. The Hawaiian–Emperor volcanic chain. II. Geologic evolution. In Volcanism in Hawaii, US Geological Survey Professional Paper no. 1350. Washington, DC, US Government Printing Office, pp. 5–54Google Scholar
Coffin, M. and Eldholm, O. 1994. Large igneous provinces: crustal structure, dimensions, and environmental consequences. Reviews of Geophysics, 32, 1–36CrossRefGoogle Scholar
Colgate, S. and Sigurgeirsson, T. 1973. Dynamic mixing of water and lava. Nature, 244, 552–555CrossRefGoogle Scholar
Crisp, J. A. 1984. Rates of magma emplacement and volcanic output. Journal of Volcanology and Geothermal Research, 20, 177–211CrossRefGoogle Scholar
Decker, R. and Decker, B. 1997. Volcanoes. New York, W. H. FreemanGoogle Scholar
Dingwell, D. B. and Webb, S. L. 1989. Structural relaxation in silicate melts and non-Newtonian melt rheology in geologic processes. Physics and Chemistry of Minerals, 16, 508–516CrossRefGoogle Scholar
Dingwell, D. B. and Webb, S. L. 1990. Relaxation in silicate melts. European Journal of Mineralogy, 2, 427–449CrossRefGoogle Scholar
Druitt, T. and Sparks, R. S. J. 1984. On the formation of calderas during ignimbrite eruptions. Nature, 310, 679–681CrossRefGoogle Scholar
Duncan, R. and Richards, M. 1991. Hotspots, mantle plumes, flood basalts and true polar wanderings. Reviews of Geophysics, 29, 31–50CrossRefGoogle Scholar
Fisher, R. V. and Schmincke, H. U. 1984. Pyroclastic Rocks. New York, Springer-VerlagCrossRefGoogle Scholar
Fisher, R. V., Smith, A. L., and Roobol, M. J. 1980. Destruction of St. Pierre, Martinique, by ash cloud surges. Geology, 8, 472–4762.0.CO;2>CrossRefGoogle Scholar
Francheteau, J. and Ballard, R. 1983. The East Pacific Rise near 21° N, 13° N, and 20° N: inferences for along-strike variability of axial processes of the mid-ocean ridge. Earth and Planetary Science Letters, 64, 93–116CrossRefGoogle Scholar
Francheteau, J., Juteau, T., and Rangin, C. 1979. Basaltic pillars in collapsed lava-pools on the deep sea floor. Nature, 281, 209–211CrossRefGoogle Scholar
Francis, P. 1993. Volcanoes: A Planetary Perspective. Oxford, UK, Oxford University PressGoogle Scholar
Francis, P. W., Hammill, M., Kretzschmar, G., et al. 1978. The Cerro Galân Caldera, Northwest Argentina. Nature, 274, 749–751CrossRefGoogle Scholar
Frankel, C. 1996. Volcanoes of the Solar System. Cambridge, UK, Cambridge University PressGoogle Scholar
Greeley, R. 1982. The Snake River Plain, Idaho: representative of a new category of volcanism. Journal of Geophysical Research, 87, 2705–2712CrossRefGoogle Scholar
Gregg, T. and Fink, J. 1995. Quantification of submarine lava-flow morphology through analog experiments. Geology, 23, 73–762.3.CO;2>CrossRefGoogle Scholar
Griffiths, R. and Fink, J. 1992. Solidification and morphology of submarine lavas: a dependence in extrusion rate. Journal of Geophysical Research, 97, 19729–19737CrossRefGoogle Scholar
Gudmunsson, A. 1996. Volcanoes in Iceland. Reykjavik, Vaka-HelgafellGoogle Scholar
Head, J. and Wilson, L. 1987. Lava fountain heights at Pu'u ‘O'o, Kilauea, Hawaii: indicators of amount and variations of exsolved magma volatiles. Journal of Geophysical Research, 92, 13715–13719CrossRefGoogle Scholar
Head, J. and Wilson, L. 1992. Magma reservoirs and neutral buoyancy zones on Venus: implications for the formation and evoution of volcanic landforms. Journal of Geophysical Research, 97, 3877–3903CrossRefGoogle Scholar
Hekinian, R., Thompson, G., and Bidcau, D. 1989. Axial and off-axial heterogeneity of basaltic rocks from the East Pacific Rise at 12° 35ʹ N–12° 51ʹ N and 11° 26ʹ N–11° 30ʹ N. Journal of Geophysical Research, 94, 17437–17463CrossRefGoogle Scholar
Hulme, G. 1974. Interpretation of lava flow morphology. Royal Astronomical Society Geophysical Journal, 39, 361–383CrossRefGoogle Scholar
Humphris, S., Zierenberg, R., Mullineaux, L., et al. 1995. Seafloor Hydrothermal Systems: Physical, Chemical, Biological and Geological Interactions, Geophysical Monograph no. 91. Washington, DC, American Geophysical UnionCrossRefGoogle Scholar
Hurwitz, S. and Navon, O. 1994. Bubble nucleation in rhyolitic melts: experiments at high pressure, temperature and water content. Earth and Planetary Science Letters, 122, 267–280CrossRefGoogle Scholar
Iyer, H., Evans, J., Dawson, P., et al. 1990. Differences in magma storage in different volcanic environments as revealed by seismic tomography: silicic volcanic centers. In , M. Ryan (ed.) Magma Transport and Storage. Chichester, UK, John Wiley, pp. 293–316Google Scholar
Karig, D. 1971. Origin and development of marginal basins in the western Pacific. Journal of Geophysical Research, 76, 2542–2561CrossRefGoogle Scholar
Keary, P. and Vine, F. 1990. Global Tectonics. Oxford, UK, Blackwell Scientific PublicationsGoogle Scholar
Kokelaar, P. 1983. The mechanism of Surtseyan volcanism. Journal of the Geological Society of London, 140, 939–944CrossRefGoogle Scholar
Kokelaar, P. 1986. Magma–water interactions in subaqueous and emergent basaltic volcanism. Bulletin of Volcanology, 48, 275–289CrossRefGoogle Scholar
Koyaguchi, T. and Tokuno, M. 1993. Origin of the giant eruption cloud of Pinatubo, June 15, 1991. Journal of Volcanology and Geothermal Research, 55, 85–96CrossRefGoogle Scholar
Lacroix, A. 1904. La Montagne Pelée et ses eruptions. Paris, MassonGoogle Scholar
Maitre, R. 1976. The chemical variability of some common igneous rocks. Journal of Petrology, 17, 589–637CrossRefGoogle Scholar
Lipman, P. and Mullineaux, D. 1981. The 1980 Eruptions of Mount St. Helens, Washington, US Geological Survey Professional Paper no. 1250. Washington, DC, US Government Printing OfficeGoogle Scholar
Macdonald, K. C., Scheirer, C., and Carbotte, S. 1991. Mid-ocean ridges: discontinuities, segments, and giant cracks. Science, 253, 986–994CrossRefGoogle ScholarPubMed
Mader, H., Zhang, Y., Phillips, J., et al. 1994. Experimental simulations of explosive degassing of magma. Nature, 372, 85–88CrossRefGoogle Scholar
Malin, M. 1980. The lengths of Hawaiian lava flows. Geology, 8, 306–3082.0.CO;2>CrossRefGoogle Scholar
Marsh, B. 1979. Island-arc volcanism. American Scientist, 67, 161–172Google Scholar
Marsh, B. 1981. On the crystallinity, probability of occurrence, and rheology of lava and magma. Contributions to Mineralogy and Petrology, 78, 85–98CrossRefGoogle Scholar
McBirney, A. R. 1973. Factors governing the intensity of explosive andesitic eruptions. Bulletin of Volcanology, 36, 443–453CrossRefGoogle Scholar
Molnar, P. and Atwater, T. 1978. Interarc spreading and Cordilleran tectonics as alternates related to the age of subducted oceanic lithosphere. Earth and Planetary Science Letters, 41, 330–340CrossRefGoogle Scholar
Moore, J. 1975. Mechanism of formation of pillow lava. American Journal of Science, 63, 269–277Google Scholar
Moore, J. G. and Normark, W. 1994. Giant Hawaiian landslides. Annual Review of Earth and Planetary Sciences, 22, 119–144CrossRefGoogle Scholar
Moore, J. G., Bryan, W. B., and Ludwig, K. 1994. Chaotic deposition by a giant wave, Molokai, Hawaii. Geological Society of America Bulletin, 106, 962–9672.3.CO;2>CrossRefGoogle Scholar
Moore, J. G., Bryan, W., Beeson, M., et al. 1995. Giant blocks in the South Kona landslide, Hawaii. Geology, 23, 125–1282.3.CO;2>CrossRefGoogle Scholar
Pallister, J., Hoblitt, R., Crandell, D., et al. 1992. Mount St. Helens a decade after the 1980 eruptions: magmatic models, chemical cycles, and a revisted hazards assessment. Bulletin of Volcanology, 54, 126–146CrossRefGoogle Scholar
Parfitt, E. and Wilson, L. 1995. Explosive volcanic eruptions. IX. The transition between Hawaiian-style lava fountaining and strombolian explosive activity. Geophysical Journal International, 121, 226–232CrossRefGoogle Scholar
Peacock, S. M. 1996. Thermal and petrologic structure of subduction zones. In , G. Bebout, , D. Scholl, , S. Kirby, et al. (eds.) Subduction Top to Bottom. Geophysical Monograph no. 96. Washington, DC, American Geophysical Union, pp. 119–134Google Scholar
Peterson, D. and Tilling, R. 1980. Transition of basaltic lava from pahoehoe to aa, Kilauea volcano, Hawaii: field observations and key factors. Journal of Volcanology and Geothermal Research, 7, 271–293CrossRefGoogle Scholar
Pinkerton, H. and Sparks, R. S. J. 1976. The 1975 subterminal lavas, Mount Etna: a case history of the formation of a compound lava field. Journal of Volcanology and Geothermal Research, 1, 167–182CrossRefGoogle Scholar
Pinkerton, H. and Stevenson, R. 1992. Methods of determining the rheological properties of magmas at sub-liquidus temperatures. Journal of Volcanology and Geothermal Research, 53, 47–66CrossRefGoogle Scholar
Rampino, M. 1988. Introduction: the volcano/climate connection. Annual Reviews of Earth and Planetary Sciences, 16, 73–99CrossRefGoogle Scholar
Rampino, M. and Self, S. 1992. Volcanic winters and accelerated glaciations following the Toba super-eruption. Nature, 359, 50–52CrossRefGoogle Scholar
Richards, M., Duncan, R., and Courtillot, V. 1989. Flood basalts and hot spot tracks: plume heads and tails. Science, 246, 103–107CrossRefGoogle ScholarPubMed
Riedel, C., , Ernst G. G. J., and Riley, M. 2003. Controls on the growth and geometry of pyroclastic constructs. Journal of Volcanology and Geothermal Research, 127, 121–152CrossRefGoogle Scholar
Ringwood, A. E. 1975. Composition and Petrology of the Earth's Mantle. New York, McGraw-HillGoogle Scholar
Ross, C. and Smith, R. L. 1961. Ash-Flow Tuffs: Their Origin, Geological Reactions and Identification. US Geological Survey Professional Paper no. 366. Washington, DC, USGovernment Printing OfficeGoogle Scholar
Rowland, S. and Walker, G. P. L. 1990. Pahoehoe and aa in Hawaii: volumetric flow rate controls the lava structure. Bulletin of Volcanology, 52, 615–628CrossRefGoogle Scholar
Rutherford, M. J. and Devine, J. 1988. The May 18, 1980 eruption of Mount St. Helens. III. Stability and chemistry amphibole in the magma chamber. Journal of Geophysical Research, 93, 1310, 11949–11959CrossRefGoogle Scholar
Rutherford, M., Sigurdsson, H., Carey, S., et al. 1985. The May 18, 1980 eruption of Mount St. Helens. II. Melt composition and experimental phase equilibria. Journal of Geophysical Research, 90, 2929–2947CrossRefGoogle Scholar
Ryan, M. P. 1987. Neutral buoyancy and the mechanical evolution of magmatic systems. In , B. O. Mysen (ed.) Magmatic Processes: Physiochemical Principles. Special Publication no. 1. Chichester, UK, Geochemical Society, pp. 259–287Google Scholar
Ryan, M. P. 1988. The mechanics and 3-d internal structure of active magma systems: Kilauea volcano, Hawaii. Journal of Geophysical Research, 93, 4213–4248CrossRefGoogle Scholar
Ryan, M. P. and Blevins, J. Y. K. 1987. The viscosity of synthetic and natural silicate melts and glasses at high temperature and 1 bar (105 Pascals) pressure and at higher pressure. US Geological Survey Bulletin, 1764, 1–563Google Scholar
Scandone, R. and Malone, S. 1985. Magma supply, magma discharge and readjustment of the feeding system of Mount St. Helens during 1980. Journal of Volcanology and Geothermal Research, 23, 239–262CrossRefGoogle Scholar
Schmincke, H. U. 1994. Geological Field Guide of Gran Canaria, 6th edn. Kiel, Pluto PressGoogle Scholar
Schmincke, H. U., Weaver, P. P. E., Firth, J. V., et al. 1995. Proceeding of the ODP, Initial reports no. 157. College Station, TX, Ocean Drilling ProgramGoogle Scholar
Schouten, H., Klitgord, K., and Whitehead, J. 1985. Segmentation of mid-ocean ridges. Nature, 317, 225–229CrossRefGoogle Scholar
Self, S., Wilson, L., and Nairn, L. 1979. Vulcanian eruption mechanisms. Nature, 277, 440–443CrossRefGoogle Scholar
Siebert, L. 1984. Large volcanic debris avalanches: characteristics of source areas, deposits and associated eruptions. Journal of Volcanology and Geothermal Research, 22, 163–197CrossRefGoogle Scholar
Siebert, L., Glicken, H. X., and Ui, T. 1987. Volcanic hazards from Bezymianny- and Bandai-type eruptions. Bulletin of Volcanology, 49, 435–459CrossRefGoogle Scholar
Sigurdsson, H. 1990. Evidence of volcanic loading of the atmosphere and climate response. Paleogeography, Paleoclimatology, Paleoecology, 89, 277–289CrossRefGoogle Scholar
Sigurdsson, H., Carey, S., Cornell, W., et al. 1985. The eruption of Vesuvius in AD 79. National Geographic Research, 1(3), 332–387Google Scholar
Simpkin, T. 1993. Terrestrial volcanism in space and time. Annual Reviews of Earth and Planetary Sciences, 21, 427–452CrossRefGoogle Scholar
Sinton, J. M. and Detrick, R. S. 1992. Mid-ocean ridge magma chambers. Journal of Geophysical Research, 97, 197–216CrossRefGoogle Scholar
Sisson, T. and Grove, T. 1993. Experimental investigations of the role of H2O in calc–alkaline differentiation and subduction zone magmatism. Contributions to Mineralogy and Petrology, 113, 143–166CrossRefGoogle Scholar
Smith, R. L. 1979. Ash flow magmatism. Special Paper no. 180. Boulder, CO, Geological Society of America, pp. 5–27CrossRefGoogle Scholar
Smith, R. L. and Bailey, R. A. 1968. Resurgent cauldrons. In , R. L. Hay and , C. A. Anderson (eds.) Studies in Volcanology, Geological Society of America Memoir no. 116. Boulder, CO, Geological Society of America, pp. 153–210Google Scholar
Smith, T. and Batiza, R. 1989. New field and laboratory evidence for the origin of hyaloclastite flows on seamount summits. Bulletin of Volcanology, 51, 96–114CrossRefGoogle Scholar
Sparks, R. S. J. 1978. The dynamics of bubble formation and growth in magmas. Journal of Volcanology and Geothermal Research, 3, 1–37CrossRefGoogle Scholar
Sparks, R. S. J. 1986. The dimensions and dynamics of volcanic eruption columns. Bulletin of Volcanology, 48, 3–15CrossRefGoogle Scholar
Sparks, R. S. J. 1992. Magma generation in the Earth. In Understanding the Earth. Cambridge, UK, Cambridge University Press, pp. 91–114Google Scholar
Sparks, R. S. J. and Wilson, L. 1976. Model for the formation of ignimbrite by gravitational column collapse. Journal of the Geological Society of London, 132, 441–452CrossRefGoogle Scholar
Sparks, R. S. J., Moore, J. G., and Rice, C. J. 1986. The initial giant umbrella cloud of the May 18, 1980 explosive eruption of Mount St. Helens. Journal of Volcanology and Geothermal Research, 28, 257–274CrossRefGoogle Scholar
Sparks, R. S. J., Barclay, J., Jaupart, C., et al. 1994. Physical aspects of magma degassing. II. Experimental and theoretical constraints on vesiculation. Reviews in Mineralogy, 30, 413–443Google Scholar
Sparks, R. S. J., Bursik, M., Carey, S., et al. 1997. Volcanic Plumes. Chichester, UK, John WileyGoogle Scholar
Steven, T. A. and Lipman, P. W. 1976. Calderas of the San Juan Volcanic Field, Southwestern Colorado, US Geological Survey Professional Paper no. 958. Washington, DC, US Government Printing OfficeGoogle Scholar
Stolper, E. and Newman, S. 1994. The roll of water in the petrogenesis of Mariana Trough magmas. Earth and Planetary Science Letters, 121, 293–325CrossRefGoogle Scholar
Swanson, D., Wright, T., and Helz, R. 1975. Linear vent systems and estimated rates of eruption for the Yakima basalt on the Columbia Plateau. American Journal of Science, 275, 877–905CrossRefGoogle Scholar
Tighe, S. 1997. The morphological characteristics and geological implications of prime segments and axial volcanoes along the East Pacific Rise. Unpublished Ph. D. thesis, University of Rhode Island
Tilling, R. I. 1989. Introduction and overview. In , R. I. Tilling (ed.) Short Course in Geology, vol. 1, Volcanic Hazards. Washington, DC, American Geophysical Union, pp. 1–8Google Scholar
Uyeda, S. 1982. Subduction zones: an introduction to comparative subductology. Tectonophysics, 81, 133–159CrossRefGoogle Scholar
Uyeda, S. and Kanamori, H. 1978. Back-arc opening and the mode of subduction. Journal of Geophysical Research, 84, 1049–1061CrossRefGoogle Scholar
Verhoogen, J. 1951. Mechanics of ash formation. American Journal of Science, 249, 239–246CrossRefGoogle Scholar
Vine, F. J. and Matthews, D. H. 1963. Magnetic anomalies over oceanic ridges. Nature, 199, 947–949CrossRefGoogle Scholar
Walker, G. P. L. 1974. The lengths of lava flows. Philosophical Transactions of the Royal Society of London, Series A, 274, 107–118CrossRefGoogle Scholar
White, R. and McKenzie, D. 1989. Magmatism at rift zones: the generation of volcanic continental margins and flood basalts. Journal of Geophysical Research, 94, 7685–7729CrossRefGoogle Scholar
Whitehead, J. A., Dick, H. J. B., and Schouten, H. 1984. A mechanism for magmatic accretion under spreading centers. Nature, 312, 146–148CrossRefGoogle Scholar
Williams, H. and McBirney, A. R. 1979. Volcanology. San Francisco, CA, Freeman, Cooper and CoGoogle Scholar
Wilson, J. T. 1973. Mantle plumes and plate motions. Tectonophysics, 19, 149–164CrossRefGoogle Scholar
Wilson, L. 1980. Relationships between pressure, volatile content and ejecta velocity in three types of volcanic explosion. Journal of Volcanology and Geothermal Research, 8, 297–313CrossRefGoogle Scholar
Wilson, L., Sparks, R. S. J., and Walker, G. P. L. 1980. Explosive volcanic eruptions. IV. The control of magma properties and conduit geometry on eruption column behaviour. Geophysical Journal of the Royal Astronomy Society, 63, 117–148CrossRefGoogle Scholar
Wilson, M. 1989. Igneous Petrogenesis: A Global Tectonic Approach. London, Unwin HymanCrossRefGoogle Scholar
Wohletz, K. 1986. Explosive magma–water interactions: thermodynamics, explosion mechanisms, and field studies. Bulletin of Volcanology, 48, 245–264CrossRefGoogle Scholar
Wohletz, K. and McQueen, R. 1984. Experimental studies of hydromagmatic volcanism. In Explosive Volcanism: Inception, Evolution, and Hazards. Washington, DC, National Academy Press, pp. 158–169Google Scholar
Wolff, J. and Wright, J. 1981. Rheomorphism of welded tuffs. Journal of Volcanology and Geothermal Research, 10, 13–34CrossRefGoogle Scholar
Woods, A. W. 1988. The dynamics and thermodynamics of eruption columns. Bulletin of Volcanology, 50, 169–191CrossRefGoogle Scholar
Woods, A. and Wohletz, K. 1991. Dimensions and dynamics of co-ignimbrite eruption columns. Nature, 350, 225–227CrossRefGoogle Scholar
Yoder, H. S. 1976. Generation of Basaltic Magma. Washington, DC, National Academy of SciencesGoogle Scholar
Young, S., Sparks, R. S. J., Robertson, R., et al. 1997. Eruption of Soufrière Hills volcano in Montserrat continues. Eos, 78, 401–409CrossRefGoogle Scholar

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