Abstract
The Incekaya hyaloclastite cone (eastern Anatolia, Turkey), the focal point along a major eruptive fissure, was the main source of an unusually large explosive basaltic eruption. The ca. 80 ka-old eruption began onshore with scoria cones from a 5 km N-S fracture propagating toward Lake Van (surface area of 3755 km2). At the intersection with the fault-bounded lake basin, a ca. 400-m-high subaerial hyaloclastite edifice formed, which can be crudely subdivided into a main lower massive bulk of hydrothermally altered lithic-rich hyaloclastites (CL) topped unconformably by a > 30-m-thick, well-bedded fallout tephra (CU). The CU tephras are correlated with (1) widespread onshore hyaloclastite fallout deposits mostly west-southwest of the cone and (2) a ca. 2-m-thick, ca 80-ka-old bedded hyaloclastite (V-60), part of a 220 m ICDP (International Continental Scientific Drilling Program) core, drilled in Lake Van, 27 km N of Incekaya. The hyaloclastite unit was seismically identified as being the most widespread and well-defined reflector throughout much of western Lake Van. A minimum volume of > 9 km3 fallout hyaloclastite tephra is estimated when the area of the seismic reflector is extrapolated to the coast and 2 km inland. Seismic reflectors also suggest at least two (hyaloclastite?) intralake cones rising up to 388 m above the lake sediment surface 1.5 km NW off Incekaya cone and were possibly erupted along the same fracture. The total volume of hyaloclastites includes (a) subaerial Incekaya cone, (b) the inferred subaqueous continuation of the cone(s), (c) the bedded intralake and onshore deposits, and, tentatively, (d) a widespread (seismically defined) mass flow deposits directly beneath Incekaya reflector of roughly 20 km3 and may represent the deposits of explosively erupted basaltic magma. Sideromelane shards, the main clast type, are dominantly angular, and most show ≪ 50 vol.% vesicles. Less common tachylite clasts are poorly vesicular (< 50 vol.%). Structural transitions and interlayering between tachylite and sideromelane are ubiquitous. Fluidal and pumiceous lapilli are present in the basal massive facies. Bulk rock and glass compositions indicate constant composition of the slightly evolved Al-rich basalt magma. Olivine (Fo78–82) and plagioclase (An70–80) microphenocrysts, many skeletal with growth features, and microlites make up < 1 vol.% and suggest rapid magma ascent. The high explosive energy of the eruption is interpreted to be due to (1) high magma discharge rates and shearing in the eruptive jet and (2) magma-water interaction conditions. Approximate temporal coincidences with the Incekaya eruption include the following: (a) an abrupt cessation in the supply of evolved tephra from the adjacent Süphan Volcano to the lake sediments, which ended abruptly for ca. 60 ky, (b) an extreme fall in lake level by ca. 150 m, and (c) a drastic increase in pore water salinity (Na+ and Cl− (g/L)) and pH.
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References
Bice DC (1985) Quaternary volcanic stratigraphy of Managua, Nicaragua: correlation and source assignment for multiple overlapping Plinian deposits. Geol Soc Am Bull 96:553–566. https://doi.org/10.1130/0016-7606(1985)96<553:QVSOMN>2.0.CO;2
Coltelli M, Del Carlo P, Vezzoli L (1998) Discovery of a Plinian basaltic eruption of Roman age at Etna Volcano, Italy. Geology 26:1095–1098. https://doi.org/10.1130/0091-7613(1998)026<1095:DOAPBE>2.3.CO;2
Costantini L, Bonadonna C, Houghton BF, Wehrmann H (2008) New physical characterization of the Fontana Lapilli basaltic Plinian eruption, Nicaragua. Bull Volcanol 71:337–355. https://doi.org/10.1007/s00445-008-0227-9
Cukur D, Krastel S, Schmincke H-U, Sumita M, Tomonaga Y, Çağatay N (2014a) Water level changes of Lake Van, Turkey, during the past ca. 600 ka: climatic, volcanic and tectonic controls. J Paleolimnol 52:201–214. https://doi.org/10.1007/s10933-014-9788-0
Cukur D, Krastel S, Schmincke H-U, Sumita M, Çağatay N, Meydan AF, Damcı E, Stockhecke M (2014b) Seismic stratigraphy of Lake Van, eastern Turkey. Quat Sci Rev 104:63–84. https://doi.org/10.1016/j.quascirev.2014.07.016
Cukur D, Krastel S, Tomonaga Y, Schmincke H-U, Sumita M, Meydan AF, Çağatay MN, Toker M, Kim S-O, Kong G-S, Horozal S (2017) Structural characteristics of the Lake Van Basin, eastern Turkey, from high resolution seismic reflection profiles and multibeam echosounder data: geologic and tectonic implications. Int J Earth Sci 106:1–15. https://doi.org/10.1007/s00531-016-1312-5
Dogan B, Karakas A (2013) Geometry of co-seismic surface ruptures and tectonic meaning of the 23 October 2011 Mw 7.1 Van earthquake (East Anatolian Region, Turkey). J Struct Geol 46:99–114. https://doi.org/10.1016/j.jsg.2012.10.001
Elliott JR, Copley AC, Holley R, Scharer K, Parsons B (2013) The 2011 Mw 7.1 Van (Eastern Turkey) earthquake. J Geophys Res Solid Earth 118:1–19. https://doi.org/10.1002/jgrb.50117
Fielding EJ, Lundgren PR, Taymaz T, Yolsal ÇS, Owen SE (2013) Fault-slip source models for the 2011 M7.1. Van earthquake in Turkey from SAR interferometry, pixel offset tracking, GPS and seismic waveform analysis. Seismol Res Lett 84:1–15. https://doi.org/10.1785/0220120164
Fisher RV, Schmincke H-U (1984) Pyroclastic Rocks. Springer, Berlin New York, pp 1–472
Goepfert K, Gardner JE (2010) Influence of pre-eruptive storage conditions and volatile contents on explosive Plinian style eruptions of basic magma. Bull Volcanol 72:511–521. https://doi.org/10.1007/s00445-010-0343-1
Houghton BF, Wilson CJN, Del Carlo P, Coltelli M, Sable JE, Carey R (2004) The influence of conduit processes on changes in style of basaltic Plinian eruptions: Tarawera 1886 and Etna 122 BC. J Volcanol Geotherm Res 137:1–14. https://doi.org/10.1016/j.jvolgeores.2004.05.009
Keskin M (2003) Magma generation by slab steepening and breakoff beneath a subduction-accretion complex: an alternative model for collision-related volcanism in Eastern Anatolia, Turkey. Geophys Res Lett 30:8046. https://doi.org/10.1029/2003GL018019
Keskin M (2007) Eastern Anatolia: a hot spot in a collision zone without a mantle plume. Geol Soc Am Spec Paper 430:693–722. https://doi.org/10.1130/2007.2430(32)
Kutterolf S, Freundt A, Perez T (2008) The Pacific offshore record of Plinian arc volcanism in Central America, part 2: tephra volumes and erupted masses. Geochem Geophys Geosyst 9:Q02S02. https://doi.org/10.1029/2007GC001791
Litt T, Anselmetti FS, Çağatay N, Kipfer R, Krastel S, Schmincke H-U, PALEOVAN Scientific Team (2011) A 500 000 year-long sedimentary archive drilled in Eastern Anatolia (Turkey): the PaleoVan Drilling Project. Eos 92:477–479. https://doi.org/10.1029/2011EO510002
Litt T, Anselmetti FS, Baumgarten H, Beer J, Cagatay N, Cukur D, Damci E, Glombitza C, Heumann G, Kallmeyer J, Kipfer R, Krastel S, Kwiecien O, Meydan AF, Orcen S, Pickarski N, Randlett M-E, Schmincke H-U, Schubert CJ, Sturm M, Sumita M, Stockhecke M, Tomonaga Y, Vigliotti L, Wonik T, the PALEOVAN Scientific Team (2012) 500,000 years of environmental history in eastern Anatolia: the PALEOVAN drilling project. Sci Drilling 14:18–29. https://doi.org/10.2204/iodp.sd.14.02.2012
Lorenz V (1974) Vesiculated tuffs. Sedimentology 21:273–291. https://doi.org/10.1111/j.1365-3091.1974.tb02059.x
Macdonald R, Sumita M, Schmincke H-U, Bagiński B, White JC (2015) Impact of volcanism on the evolution of Lake Van (Anatolia) IV: peralkaline felsic magmatism at the Nemrut Volcano, Turkey. Contrib Mineral Petrol 169(34). https://doi.org/10.1007/s00410-015-1127-6
Mackenzie D, Elliott JR, Altunel E, Walker RT, Kurban YC, Schwenninger J-L, Parsons B (2016) Seismotectonics and rupture process of the Mw 7.1 2011 Van reverse-faulting earthquake, Eastern Turkey, and implications for hazard in regions of distributed shortening. Geophys J Int 206:501–524. https://doi.org/10.1093/gji/ggw158
Miyaji N, Kan’no A, Kanamaru T, Mannen K (2011) High-resolution reconstruction of the Hoei eruption (AD 1707) of Fuji volcano, Japan. J Volcanol Geotherm Res 207:113–129. https://doi.org/10.1016/j.jvolgeores.2011.06.013
Notsu K, Fujitani T, Ui T, Matsuda J, Ercan T (1995) Geochemical features of collision-related volcanic rocks in central and eastern Anatolia, Turkey. J Volcanol Geotherm Res 64:171–192. https://doi.org/10.1016/0377-0273(94)00077-T
Oyan V, Keskin M, Lebedev VA, Chugaev AV, Sharkov E, Ünal E (2017) Petrology and geochemistry of the Quaternary mafic volcanism to the NE of Lake Van, eastern Anatolian collision zone, Turkey. J Petrol 58:1701–1728. https://doi.org/10.1093/petrology/egx070
Özdemir Y, Gulec N (2014) Geological and geochemical evolution of the Quaternary Süphan stratovolcano, eastern Anatolia, Turkey: evidence for the lithosphere–asthenosphere interaction in post-collisional volcanism. J Petrol 55:37–62. https://doi.org/10.1093/petrology/egt060
Özdemir Y, Blundy J, Gulec N (2011) The importance of fractional crystallization and magma mixing in controlling chemical differentiation at Süphan stratovolcano, eastern Anatolia, Turkey. Contrib Mineral Petrol 162:573–597. https://doi.org/10.1007/s00410-011-0613-8
Pearce JA, Bender JF, De Long SE, Kidd WSF, Low PJ, Guner Y, Şaroğlu F, Yılmaz Y, Moorbath S, Mitchell JG (1990) Genesis of collision volcanism in eastern Anatolia, Turkey. J Volcanol Geotherm Res 44:189–229. https://doi.org/10.1016/0377-0273(90)90018-B
Pérez W, Freundt A, Kutterolf S, Schmincke H-U (2009) The Masaya triple layer: a 2100 year old basaltic multi-episodic Plinian eruption from the Masaya caldera complex (Nicaragua). J Volcanol Geotherm Res 179:191–205. https://doi.org/10.1016/j.jvolgeores.2008.10.015
Pickarski N, Kwiecien O, Langgut D, Litt T (2015) Abrupt climate and vegetation variability of eastern Anatolia during the last glacial. Clim Past 11:1491–1505. https://doi.org/10.5194/cp-11-1491-2015
Rausch J, Schmincke H-U (2010) Nejapa tephra: the youngest (ca. 1 ka BP) highly explosive hydroclastic basaltic eruption in western Managua (Nicaragua). J Volcanol Geotherm Res 192:159–177. https://doi.org/10.1016/j.jvolgeores.2010.02.010
Schmincke H-U, Sumita M (2014) Impact of volcanism on the evolution of Lake Van (eastern Anatolia) III. Periodic (Nemrut) vs. episodic (Süphan) explosive eruptions and climate forcing reflected in a tephra gap between ca. 14 ka and ca. 30 ka. J Volcanol Geotherm Res 285:195–213. https://doi.org/10.1016/j.jvolgeores.2014.08.015
Şengör AMC, Özeren S, Zor E, Genç T (2003) East Anatolian high plateau as a mantle-supported, N-S shortened domal structure. Geophys Res Lett 30:8045. https://doi.org/10.1029/2003GL017858
Stockhecke M, Sturm M, Brunner I, Schmincke H-U, Sumita M, Kipfer R, Cukur D, Kwiecien O, Anselmetti FS (2014a) Sedimentary evolution and environmental history of Lake Van (Turkey) over the past 600 000 years. Sedimentology 61:1830–1861. https://doi.org/10.1111/sed.12118
Stockhecke M, Kwiecien O, Vigliotti L, Anselmetti FS, Beer J, Cagatay MN, Channell JET, Kipfer R, Lachner J, Litt T, Pickarski N, Sturm M (2014b) Chronostratigraphy of the 600,000 year old continental record of lake Van (Turkey). Quat Sci Rev 104:8–17. https://doi.org/10.1016/j.quascirev.2014.04.008
Sumita M, Schmincke H-U (2013a) Impact of volcanism on the evolution of Lake Van II: temporal evolution of explosive volcanism of Nemrut Volcano (eastern Anatolia) during the past ca. 0.4 Ma. J Volcanol Geotherm Res 253:15–34. https://doi.org/10.1016/j.jvolgeores.2012.12.009
Sumita M, Schmincke H-U (2013b) Erratum to “Impact of volcanism on the evolution of Lake Van II: Temporal evolution of explosive volcanism of Nemrut Volcano (eastern Anatolia) during the past ca. 0.4 Ma” [J Volcanol Geotherm Res 253:15–34]. J Volcanol Geotherm Res 253:131–133. https://doi.org/10.1016/j.jvolgeores.2013.01.008
Sumita M, Schmincke H-U (2013c) Impact of volcanism on the evolution of Lake Van I: evolution of explosive volcanism of Nemrut Volcano (eastern Anatolia) during the past ca. 0.4 Ma. Bull Volcanol 75:714–715. https://doi.org/10.1007/s00445-013-0714-5.
Thordarson G, Self S (1983) The Laki (Skalftar Fires) and Grimsvötn eruption in 1783-1785. Bull Volcanol 55:233–263. https://doi.org/10.1007/BF00624353
Tomonaga Y, Brennwald MS, Livingstone DM, Kwiecien O, Randlett M-E, Stockhecke M, Unwin K, Anselmetti F, Beer J, Haug GH, Schubert J, Sturm M, Kipfer R (2017) Porewater salinity reveals past lake-level changes in Lake Van, the Earth’s largest soda lake. Nature Sci Rep 7:313. https://doi.org/10.1038/s41598-017-00371-w
Ustaömer AD, Ustaömer T, Gerdes A, Robertson AHF, Collins AS (2012) Evidence of Precambrian sedimentation/magmatism and Cambrian metamorphism in the Bitlis Massif, SE Turkey utilising whole-rock geochemistry and U–Pb LA-ICP-MS zircon dating. Gondwana Res 21:1001–1018. https://doi.org/10.1016/j.gr.2011.07.012
Wehrmann H, Bonadonna C, Freundt A, Houghton BF, Kutterolf S (2006) Fontana tephra: a basaltic plinian eruption in Nicaragua. Geol Soc Am Spec Pap 412:209–223. https://doi.org/10.1130/2006.2412(11)
Williams SN (1983) Plinian airfall deposits of basaltic composition. Geology 11:211–214. https://doi.org/10.1130/0091-7613(1983)11<211:PADOBC>2.0.CO;2
Acknowledgments
Work by HUS and MS was supported by DFG projects SCHM250/87-1 and 92-1. DC was supported by DFG projects KR2222-9 and KR2222-15 to S. Krastel and by the Development of Integrated Geological Information based on Digital Mapping Project (GP2017-021) of the Korea Institute of Geoscience and Mineral Resources (KIGAM). We thank Steffen Kutterolf, an anonymous reviewer, and especially Andrew Harris and Larry Mastin for many helpful comments and suggestions that led to significant improvements of the manuscript.
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Schmincke, HU., Sumita, M. & Cukur, D. Large-volume basaltic hyaloclastite eruption along a propagating land/lake lithosphere fracture at Lake Van (Eastern Anatolia): impact of volcanism on the evolution of Lake Van V. Bull Volcanol 80, 82 (2018). https://doi.org/10.1007/s00445-018-1257-6
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DOI: https://doi.org/10.1007/s00445-018-1257-6