Deposits, character and timing of recent eruptions and gravitational collapses in Tatun Volcanic Group, Northern Taiwan: Hazard-related issues

article i nfo Taipei City, with a population of around 8 million, as well as two nuclear power plants is located in close proximity to the Quaternary, dominantly andesitic Tatun Volcanic Group (TVG) of Northern Taiwan. We have investigated the stratigraphy of the youngest volcaniclastic deposits, as well as the morphology of lava flows and domes of the TVG in order to reconstruct the character and timing of the most recent eruptions and related hazardous events in the area. Our data indicate that recent eruptions of the group were dominated by long-term, voluminous extrusions of crystal-rich, very viscous lavas. These eruptions formed closely spaced monogenetic domes and lava flows. Based on morphological parameters of the lava flows (thicknesses 80-150 m, lengths up to 5.6 km, and volumes up to 0.6 km 3

[1]  Mark Simons,et al.  Interseismic crustal deformation in the Taiwan plate boundary zone revealed by GPS observations, seismicity, and earthquake focal mechanisms , 2008 .

[2]  D. Pyle,et al.  Fumarole compositions and mercury emissions from the Tatun Volcanic Field, Taiwan: Results from multi-component gas analyser, portable mercury spectrometer and direct sampling techniques , 2008 .

[3]  G. Walker,et al.  Grain-Size Characteristics of Pyroclastic Deposits , 1971, The Journal of Geology.

[4]  C. S. Ho A synthesis of the geologic evolution of Taiwan , 1986 .

[5]  R. Stevenson,et al.  Rheological estimates of rhyolite lava flows from the Okataina Volcanic Centre, New Zealand , 1994 .

[6]  Dimitri Lague,et al.  Links between erosion, runoff variability and seismicity in the Taiwan orogen , 2003, Nature.

[7]  B. Voight,et al.  Directed blasts and blast-generated pyroclastic density currents: a comparison of the Bezymianny 1956, Mount St Helens 1980, and Soufrière Hills, Montserrat 1997 eruptions and deposits , 2007 .

[8]  D. Schneider,et al.  Growth of the 2004-2006 Lava-Dome Complex at Mount St. Helens, Washington , 2008 .

[9]  Matthew E. Pritchard,et al.  Uturuncu volcano, Bolivia: Volcanic unrest due to mid-crustal magma intrusion , 2008, American Journal of Science.

[10]  A. Belousov,et al.  Eruptive Process, Effects and Deposits of the 1996 and the Ancient Basaltic Phreatomagmatic Eruptions in Karymskoye Lake, Kamchatka, Russia , 2009 .

[11]  Shui-Beih Yu,et al.  Velocity field of GPS stations in the Taiwan area , 1997 .

[12]  C. Hong,et al.  Eruptions younger than 20 Ka of the Tatun Volcano Group as viewed from the sediments of the Sungshan Formation in Taipei Basin , 2002 .

[13]  D. Pyle The thickness, volume and grainsize of tephra fall deposits , 1989 .

[14]  Cheng‐Horng Lin,et al.  Seismicity characteristics of a potentially active Quaternary volcano: The Tatun Volcano Group, northern Taiwan , 2007 .

[15]  K. Ma,et al.  Modern Seismic Observations in the Tatun Volcano Region of Northern Taiwan: Seismic/Volcanic Hazard Adjacent to the Taipei Metropolitan Area , 2005 .

[16]  G. Zellmer,et al.  Using trace element correlation patterns to decipher a sanidine crystal growth chronology: an example from Taapaca volcano, Central Andes , 2006 .

[17]  Kuo‐Lung Wang Geochemical Constraints for the Genesis of Post-collisional Magmatism and the Geodynamic Evolution of the Northern Taiwan Region , 2004 .

[18]  S. Self,et al.  The volcanic explosivity index (VEI) an estimate of explosive magnitude for historical volcanism , 1982 .

[19]  Sheng-Rong Song,et al.  ^3He/^4He ratios of fumaroles and bubbling gases of hot springs in Tatun Volcano Group, North Taiwan , 1999 .

[20]  B. Houghton,et al.  A vesicularity index for pyroclastic deposits , 1989 .

[21]  Cheng-Hong Chen,et al.  The volcanology and fission track age dating of pyroclastic deposits in Tatun Volcanico group, Northern Taiwan , 1990 .

[22]  J. Fink,et al.  Predicting yield strengths and effusion rates of lava domes from morphology and underlying topography , 2004 .

[23]  Y. Yeh,et al.  The Tatun Volcano Group is active or extinct , 2000 .

[24]  Bruce F. Houghton,et al.  The encyclopedia of volcanoes , 1999 .

[25]  R. Shinjo,et al.  Post-collisional magmatism around northern Taiwan and its relation with opening of the Okinawa Trough , 1999 .

[26]  M. E. Mackay,et al.  Thick lava flows of Karisimbi Volcano, Rwanda: insights from SIR-C interferometric topography , 1998 .

[27]  N. A. Zharinov,et al.  The growth of an extrusive dome on Shiveluch Volcano, Kamchatka in 1980–2007: Geodetic observations and video surveys , 2008 .

[28]  Louis S. Teng Extensional collapse of the northern Taiwan mountain belt , 1996 .

[29]  H. Glicken Rockslide-debris avalanche of May 18, 1980, Mount St. Helens Volcano, Washington , 1996 .

[30]  P. Layer,et al.  Excess argon in Mount St. Helens plagioclase as a recorder of magmatic processes , 2001 .

[31]  H. Lo Compositions of tatun andesites, northern taiwan , 1982 .

[32]  L. Siebert Large volcanic debris avalanches: Characteristics of source areas, deposits, and associated eruptions , 1984 .

[33]  Wen-Tzong Liang,et al.  Preliminary analysis of volcanoseismic signals recorded at the Tatun Volcano Group, northern Taiwan , 2005 .

[34]  G. Walker Plinian eruptions and their products , 1981 .

[35]  H. Chen,et al.  Lahars in and around the Taipei basin: Implications for the activity of the Shanchiao fault , 2007 .

[36]  Sheng‐Rong Song,et al.  Fumarolic Gas Composition of the Tatun Volcano Group, Northern Taiwan , 2005 .

[37]  R. W. Griffiths,et al.  Morphology, eruption rates, and rheology of lava domes - Insights from laboratory models , 1998 .

[38]  Alexander Belousov,et al.  Multiple edifice failures, debris avalanches and associated eruptions in the Holocene history of Shiveluch volcano, Kamchatka, Russia , 1999 .

[39]  Rosaly M. C. Lopes,et al.  General patterns of flow field growth: Aa and blocky lavas , 1991 .

[40]  R. Sparks,et al.  Magma Emplacement and Remobilization Timescales Beneath Montserrat: Insights from Sr and Ba Zonation in Plagioclase Phenocrysts , 2003 .

[41]  H. Westrich,et al.  Non-explosive silicic volcanism , 1986, Nature.

[42]  C. Chen Geology and geothermal power potential of the Tatun volcanic region , 1970 .

[43]  K. Wohletz,et al.  Hydrovolcanic explosions; II, Evolution of basaltic tuff rings and tuff cones , 1983 .

[44]  M. Sheridan,et al.  Secondary electron imagery of microcracks and hackly fracture surfaces in sand-size clasts from the 1980 Mount St. Helens debris-avalanche deposit: Implications for particle-particle interactions , 1991 .

[45]  Jin-King Liu,et al.  Lidar DEM for characterizing the volcanic landforms of tatun volcanoes in metropolitan taipei , 2007, 2007 IEEE International Geoscience and Remote Sensing Symposium.

[46]  J. Eichelberger Silicic Volcanism: Ascent of Viscous Magmas from Crustal Reservoirs , 1995 .

[47]  A. Szakács Redefining active volcanoes: a discussion , 1994 .

[48]  Sheng‐Rong Song,et al.  Temporal variations of gas compositions of fumaroles in the Tatun Volcano Group, northern Taiwan , 2008 .