Bulletin of Volcanology

, Volume 73, Issue 6, pp 639–653 | Cite as

Cyclic spattering, seismic tremor, and surface fluctuation within a perched lava channel, Kīlauea Volcano

  • Matthew R. Patrick
  • Tim Orr
  • David Wilson
  • David Dow
  • Richard Freeman
Research Article

Abstract

In late 2007, a perched lava channel, built up to 45 m above the preexisting surface, developed during the ongoing eruption near Pu‘u ‘Ō‘ō cone on Kīlauea Volcano’s east rift zone. The lava channel was segmented into four pools extending over a total of 1.4 km. From late October to mid-December, a cyclic behavior, consisting of steady lava level rise terminated by vigorous spattering and an abrupt drop in lava level, was commonly observed in pool 1. We use geologic observations, video, time-lapse camera images, and seismicity to characterize and understand this cyclic behavior. Spattering episodes occurred at intervals of 40–100 min during peak activity and involved small (5–10-m-high) fountains limited to the margins of the pool. Most spattering episodes had fountains which migrated downchannel. Each spattering episode was associated with a rapid lava level drop of about 1 m, which was concurrent with a conspicuous cigar-shaped tremor burst with peak frequencies of 4–5 Hz. We interpret this cyclic behavior to be gas pistoning, and this is the first documented instance of gas pistoning in lava well away from the deeper conduit. Our observations and data indicate that the gas pistoning was driven by gas accumulation beneath the visco-elastic component of the surface crust, contrary to other studies which attribute similar behavior to the periodic rise of gas slugs. The gas piston events typically had a gas mass of about 2,500 kg (similar to the explosions at Stromboli), with gas accumulation and release rates of about 1.1 and 5.7 kg s−1, respectively. The time-averaged gas output rate of the gas pistoning events accounted for about 1–2% of the total gas output rate of the east rift zone eruption.

Keywords

Cyclic spattering Seismic tremor Gas pistoning Kīlauea Volcano 

References

  1. Barker SR, Sherrod DR, Lisowski M, Heliker C, Nakata JS (2003) Correlation between lava-pond drainback, seismicity and ground deformation at Pu`u `O`o. In: Heliker C, Swanson DA, Takahashi TJ (eds) The Pu`u `O`o–Kupaianaha eruption of Kilauea Volcano, Hawai`i: the first 20 years. US Geol Surv Prof Pap 1676, pp 53–62Google Scholar
  2. Burton M, Allard P, Mure F, La Spina A (2007) Magmatic gas composition reveals the source depth of slug-driven Strombolian explosive activity. Science 317:227–230. doi:10.1126/science.1141900 CrossRefGoogle Scholar
  3. Chouet B, Hamisevicz N, McGetchin TR (1974) Photoballistics of volcanic jet activity at Stromboli, Italy. J Geophys Res 79:4931–4976CrossRefGoogle Scholar
  4. Dietel C, Chouet B, Aki K, Ferrazzini V, Roberts P, Koyanagi R (1989) Data summary for dense GEOS array observations of seismic activity associated with magma transport at Kīlauea Volcano, Hawai‘i. US Geol Surv Open File Rept 89–113, 171 ppGoogle Scholar
  5. Duffield WA (1972) A naturally occurring model of global plate tectonics. J Geophys Res 77:2543–2555CrossRefGoogle Scholar
  6. Edmonds M, Gerlach TM (2007) Vapor segregation and loss in basaltic melts. Geology 35:751–754CrossRefGoogle Scholar
  7. Ferrazzini V, Aki K, Chouet BA (1991) Characteristics of seismic waves composing Hawaiian volcanic tremor and gas-piston events observed by a near-source array. J Geophys Res 96:6199–6209CrossRefGoogle Scholar
  8. Flynn LP, Mouginis-Mark PJ, Gradie JC, Lucey PG (1993) Radiative temperature measurements at Kupaianaha lava lake, Kilauea Volcano, Hawaii. J Geophys Res 98:6461–6476CrossRefGoogle Scholar
  9. Gerlach TM, Graeber EJ (1985) Volatile budget of Kilauea volcano. Nature 313:273–277CrossRefGoogle Scholar
  10. Harris AJL, Ripepe M (2007a) Synergy of multiple geophysical approaches to unravel explosive eruption conduit and source dynamics—a case study from Stromboli. Chem Erde 67:1–35CrossRefGoogle Scholar
  11. Harris AJL, Ripepe M (2007b) Temperature and dynamics of degassing at Stromboli. J Geophys Res 112:B3. doi:10.1029/2006JB004393 Google Scholar
  12. Harris AJL, Carniel R, Jones J (2005) Identification of variable convective regimes at Erta Ale lava lake. J Volcanol Geotherm Res 142:207–223CrossRefGoogle Scholar
  13. Heliker C, Mattox TN (2003) The first two decades of the Pu‘u ‘Ō‘ō–Kupaianaha eruption: chronology and selected bibliography. In: Heliker C, Swanson DA, Takahashi TJ (eds) The Pu`u `O`o–Kupaianaha eruption of Kilauea Volcano, Hawai`i: the first 20 years. US Geol Surv Prof Pap 1676, pp 1–27Google Scholar
  14. Hon K, Kauahikaua J, Denlinger R, Mackay K (1994) Emplacement and inflation of pahoehoe sheet flows: observations and measurements of active lava flows on Kilauea Volcano, Hawaii. Geol Soc Am Bull 106:351–370CrossRefGoogle Scholar
  15. Jaggar TA (1912) Report of the Hawaiian Volcano Observatory of the Massachusetts Institute of Technology and the Hawaiian Volcano Research Association, January–March 1912. In: Bevens D, Takahashi TJ, Wright TL (eds) The early serial publications of the Hawaiian Volcano Observatory, volume 1, 1988. Hawaii Nat Hist Assoc, p 25Google Scholar
  16. Jaupart C, Vergniolle S (1988) Laboratory models of Hawaiian and Strombolian eruptions. Nature 331:58–60CrossRefGoogle Scholar
  17. Johnson JB, Harris AJL, Hoblitt RP (2005) Thermal observations of gas pistoning at Kilauea volcano. J Geophys Res 110:B11201. doi:10.1029/2005JB003944 CrossRefGoogle Scholar
  18. Kauahikaua J (2007) Lava flow hazard assessment, as of August 2007, for Kīlauea east rift zone eruptions, Hawai‘i Island. US Geol Surv Open-File Rept 2007-1264, 9 pp. http://pubs.usgs.gov/of/2007/1264
  19. Marchetti E, Harris AJL (2008) Trends in activity at Pu`u `O`o during 2001–2003: insights from the continuous thermal record. In: Lane SJ and Gilbert JS (eds) Fluid motions in volcanic conduits: a source of seismic and acoustic signals. Geol Soc London Spec Pub 307, pp 85–101Google Scholar
  20. Moore HJ (1987) Preliminary estimates of the rheological properties of 1984 Mauna Loa lava. In: Decker RW, Wright TL, Stauffer PH (eds) Volcanism in Hawaii. US Geol Surv Prof Pap 1350, pp 1569–1588Google Scholar
  21. Mori T, Burton M (2009) Quantification of the gas mass emitted during single explosions on Stromboli with the SO2 imaging camera. J Volcanol Geoth Res 188:395–400. doi:10.1016/j.jvolgeores.2009.10.005 CrossRefGoogle Scholar
  22. Oppenheimer C, Bani P, Calkins JA, Burton MR, Sawyer GM (2006) Rapid FTIR sensing of volcanic gases released by Strombolian explosions at Yasur volcano, Vanuatu. Appl Phys B 85:453–460CrossRefGoogle Scholar
  23. Oppenheimer C, Lomakina AS, Kyle PR, Kingsbury NG, Boichu M (2009) Pulsatory magma supply to a phonolite lava lake. Earth Planet Sci Lett 284:392–398. doi:10.1016/j.epsl.2009.04.043 CrossRefGoogle Scholar
  24. Orr T, Hoblitt RP (2008) A versatile time-lapse camera system developed by the Hawaiian Volcano Observatory for use at Kīlauea Volcano, Hawai‘i. US Geol Surv Sci Invest Rept 2008-5117, 8 pp. http://pubs.usgs.gov/sir/2008/5117
  25. Patrick M, Harris AJL, Ripepe M, Dehn J, Rothery D, Calvari S (2007) Strombolian explosive styles and source conditions: insights from thermal (FLIR) video. Bull Volcanol 69:769–784. doi:10.1007/s00445-006-0107-0 CrossRefGoogle Scholar
  26. Peck DL (1978) Cooling and vesiculation of Alae lava lake, Hawaii. US Geol Surv Prof Pap 935-B, 59 ppGoogle Scholar
  27. Perret FA (1913) The lava fountains of Kilauea. Am J Sci, 4th ser, 35:139–148Google Scholar
  28. Poland M, Miklius A, Orr T, Sutton AJ, Thornber C, Wilson D (2008) New episodes of volcanism at Kīlauea Volcano, Hawai‘i. EOS Trans AGU 89:37–38CrossRefGoogle Scholar
  29. Shaw HR, Kistler RW, Evernden JF (1971) Sierra Nevada plutonic cycle: part II, tidal energy and a hypothesis for orogenic–epeirogenic periodicities. Geol Soc Am Bull 82:869–896CrossRefGoogle Scholar
  30. Sutton AJ, Elias T, Kauahikaua J (2003) Lava-effusion rates for the Pu`u `O`o-Kupaianaha eruption derived from SO2 emissions and very low frequency (VLF) measurements. In: Heliker C, Swanson DA, Takahashi TJ (eds) The Pu`u `O`o-Kupaianaha eruption of Kilauea Volcano, Hawai`i: the first 20 years. US Geol Surv Prof Pap 1676, pp 137–148Google Scholar
  31. Swanson DA, Duffield WA, Jackson DB, Peterson DW (1979) Chronological narrative of the 1969–71 Mauna Ulu eruption of Kilauea volcano, Hawaii. US Geol Surv Prof Pap 1056, 55 ppGoogle Scholar
  32. Vergniolle S, Jaupart C (1990) Dynamics of degassing at Kilauea volcano, Hawaii. J Geophys Res 95:2793–2809CrossRefGoogle Scholar
  33. Wright TL, Kinoshita WT, Peck DL (1968) March 1965 eruption of Kilauea Volcano and the formation of Makaopuhi lava lake. J Geophys Res 73:3181–3205CrossRefGoogle Scholar

Copyright information

© Springer-Verlag (outside the USA) 2010

Authors and Affiliations

  • Matthew R. Patrick
    • 1
  • Tim Orr
    • 1
  • David Wilson
    • 2
  • David Dow
    • 1
  • Richard Freeman
    • 3
  1. 1.Hawaiian Volcano ObservatoryUS Geological SurveyHonoluluUSA
  2. 2.Albuquerque Seismological LaboratoryUS Geological SurveyAlbuquerqueUSA
  3. 3.Department of GeosciencesEast Tennessee State UniversityJohnson CityUSA

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