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Askja

Data series

Eruptions
  • series: Eruptions
  • series_type: Volc_Eruptions
eruptioneruption_typett_sigmat_sourcerefnotes
Askja AD1875Ultra-Plinian1875.51Calendardoi:10.1191/095968399669624108AD 1875 historical (see Sigvaldason et al. 1992; Larsen et al. 1999)
Askja-SUltra-Plinian-8859.5240IntCal04doi:10.1002/jqs.996c. 11,050-10,570 cal BP bayesian 14C wiggle-match (Wohlfarth et al. 2006).
NGRIP 1553.85mSub-Plinian-11579.51GICC05doi:10.1029/2005jd006079NGRIP GICC05 13580 ± 156 b2k.
Glen GarryPlinian-225.582IntCal04doi:10.1177/09596836070855942210-1966 yr cal BP 14C wiggle-match (2 sigma; Barber et al. 2008). The same authors conjecture that this tephra derives from the Askja volcanic system.

Eyjafallajokull

Data series

Eruptions
  • series: Eruptions
  • series_type: Volc_Eruptions
eruptioneruption_typett_sigmat_sourcerefnotes
Eyjafallajokull AD1821-23Sub-Plinian1822.52Calendardoi:10.1191/095968399669624108AD 1821-23 historical

Grimsvotn

Data series

Eruptions
  • series: Eruptions
  • series_type: Volc_Eruptions
eruptioneruption_typett_sigmat_sourcerefnotes
SaksunarvatnUltra-Plinian-8346.51GICC05doi:10.1029/2005jd006079c. 10347 ± 89 (GICC05 yr b2k) has been suggested by Rasmussen et al. (2006).
I-THOL-2 (Tv-1)Plinian-10649.51GICC05doi:10.1029/2005jd006079cf. NGRIP 1519.1 m layer. GICC05 age 12650 ± 130 b2k. Alternatively SS09 12450-12454 ice core yrs BP
HovFissure-4009.5207IntCal09doi:10.1002/jqs.724c. 5170 ± 85 14C yr BP (Wastegard 2002, JQS 17(8), 723-730). Calibrates to 6182-5730 yr cal BP (2 sigma). Same age as SILK A1 based on 14C data from Hovsdalur but basaltic in major element composition. Based on this an origin in the Grimsvotn system is more likely than Katla.
FMAZ IIIPlinian-36121.51GICC05doi:10.1016/j.epsl.2010.03.004c. 38122 ± 723 b2k yr BP by Davies et al. (2010) from NGRIP 2066.95 m. This replaces c. 33 ka 14C yr by Wastegard et al. (2006), QSR 25, p.2409-2419.
Saksunarvatn_Distribution
  • series: Saksunarvatn_Distribution
  • series_type: Tephra_Distribution
  • eruption: Saksunarvatn
sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
LykkjuvøtnFaroe Islands-6.84237003361.9093017652TerrestrialQUEST495/31distalfallashquest

Hekla

Data series

Eruptions
  • series: Eruptions
  • series_type: Volc_Eruptions
eruptioneruption_typett_sigmat_sourcerefnotes
Hekla AD1947Plinian1947.51Calendardoi:10.1191/095968399669624108AD 1947 historical
Hekla AD1845Plinian1845.51Calendardoi:10.1191/095968399669624108AD 1845 historical
Hekla AD1510Plinian1510.51Calendardoi:10.1191/095968399669624108AD 1510 historical
Hekla AD1300Plinian1300.51Calendardoi:10.1191/095968399669624108AD 1300 historical
Hekla AD1158Plinian1158.51Calendardoi:10.1191/095968399669624108AD 1158 historical
Hekla AD1104Ultra-Plinian1104.51Calendardoi:10.1191/095968399669624108AD 1104 historical (see Larsen and Thorarinsson 1977; Larsen et al. 1999)
MOR-T6Plinian840.5100doi:10.1191/0959683604hl749rpc. AD 840 interpolated (Chambers et al. 2004)
Tjornuvik AD800 APlinian800.550doi:10.1191/095968301668079904ninth century AD age suggested by Wastegard et al. (2001).
BMR-190Plinian-643.560IntCal04doi:10.1191/0959683604hl757rrc. 705-585 cal BC (Plunkett et al. 2004).
H3 HeklaUltra-Plinian-1054.5157IntCal09c. 2820 ± 70 14C yr BP, i.e. 3156-2772 yr cal BP (2 sigma; Larsen and Thorarinsson 1977)
KAL-XPlinian-1769.515IntCal04doi:10.1177/0959683608089208c. 3735-3705 cal BP wiggle-match. Proximal equivalent of Hekla Selsund, Hekla HS and Kebister distal tephras (Wastegard et al. 2008)
Hekla SelsundPlinian-1769.515IntCal04doi:10.1177/0959683608089208c. 3735-3705 cal BP wiggle-match. Distal equivalent of Hekla KAL-X proximal tephra (Wastegard et al. 2008).
KebisterPlinian-1769.515IntCal04doi:10.1177/0959683608089208c. 3735-3705 cal BP wiggle-match. Distal equivalent of Hekla KAL-X proximal tephra (Wastegard et al. 2008).
Hekla HSPlinian-1769.515IntCal04doi:10.1177/0959683608089208c. 3735-3705 cal BP wiggle-match. Distal equivalent of Hekla KAL-X proximal tephra (Wastegard et al. 2008).
H4 HeklaUltra-Plinian-2309.520doi:10.1177/095968369500500111c. 2310 ± 20 calBC wiggle-match at Sluggan
Lairg APlinian-4952.547doi:10.1191/0959683602hl538rrc. 4997-4902 cal BC 14C wiggle-match (Pilcher et al. 1996; Hall & Pilcher 2002).
H5 HeklaUltra-Plinian-5101.5105IntCal09ref:vilmundardottir1982hssc. 6185 ± 100 or 6070 ± 120 14C yr BP (respectively Thórarinsson 1971 and Vilmundardóttir & Kaldal 1982). Weighted mean age gives 7247-6800 yr cal BP (2 sigma).
Hekla AD1104_Distribution
  • series: Hekla AD1104_Distribution
  • series_type: Tephra_Distribution
  • eruption: Hekla AD1104
sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
Ballysculllian EastUK-6.46299982154.7975006144TerrestrialQUEST621/38distalfallashquest
Derrycunihy WoodIreland-9.41666984652.01670074TerrestrialQUEST580/38distalfallashquest
H4 Hekla_Distribution
  • series: H4 Hekla_Distribution
  • series_type: Tephra_Distribution
  • eruption: H4 Hekla
sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
BødalsvatnettNorway13.5620002768.196998642TerrestrialQUEST634/47distalfallashquest
Corlea Bog west Corlea IIreland-7.86667013253.59999847TerrestrialQUEST578/47distalfallashquest
Croaghaun EastIreland-9.45503044154.19200134TerrestrialQUEST581/47distalfallashquest
Red BogIreland-8.53328037352.51639938TerrestrialQUEST582/47distalfallashquest
ToomeUK-6.46179008554.75170135TerrestrialQUEST632/47distalfallashquest
Hekla AD1510_Distribution
  • series: Hekla AD1510_Distribution
  • series_type: Tephra_Distribution
  • eruption: Hekla AD1510
sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
Derrycunihy WoodIreland-9.41666984652.01670074TerrestrialQUEST580/35distalfallashquest
Lairg A_Distribution
  • series: Lairg A_Distribution
  • series_type: Tephra_Distribution
  • eruption: Lairg A
sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
ToomeUK-6.46179008554.75170135TerrestrialQUEST632/48distalfallashquest

Katla

Data series

Eruptions
  • series: Eruptions
  • series_type: Volc_Eruptions
eruptioneruption_typett_sigmat_sourcerefnotes
Vedde AshUltra-Plinian-10170.51GICC05doi:10.1029/2005jd006079Bi-model rhyolitic and basalt ash layer, c. 12171 ± 114 yr b2k (GICC05); alternatively NGRIP SS09 11985-11988 ice core yr BP. Norddahl and Haflidason (1992) have suggested that the Skogar tephra is the proximal correlate of the Vedde Ash.
Katla AD1625Plinian1625.51CalendarAD 1625 historical
Eldgja tephraSub-Plinian934.51GICC05doi:10.1177/095968369500500201
notes
c. AD 938 ± 4 (GISP2) or AD934 ± 2.

Katla~1000 and K-x are now believed to correspond to this eruption (G. Larsen, 2010, Katla: tephrochronology and eruption history, in Schomacker et al. [eds.] 'The Mýrdalsjökull Ice Cap, Iceland: glacial processes, sediments and landforms on an active volcano', Developments in Quaternary Science vol. 13, pp.23-49, Amsterdam: Elsevier).
  • GA4-85Plinian750.550doi:10.1191/0959683602hl538rrc. AD 700-800 interpolated (Hall & Pilcher 2002).
    Tjornuvik AD800 BPlinian800.550doi:10.1191/095968301668079904ninth century AD age suggested by Wastegard et al. (2001).
    GB4-150Plinian-777.521IntCal04doi:10.1191/0959683604hl757rrc. 800-758 cal BC (Plunkett et al. 2004).
    Mjauvotn APlinian-4399.5200doi:10.1191/095968301668079904c. 5300-5700 14C yr BP radiocarbon. A mid-distal basaltic tephra (Tv-5) dated to c. 6000 BP with a similar geochemistry to this tephra has been recorded in the sediment succession from Lake Torfadalsvatn on northern Iceland (Bjorck et al., 1992).
    Mjauvotn BPlinian-4399.5200doi:10.1191/095968301668079904c. 5300-5700 14C yr BP radiocarbon
    Torfadalsvatn (Tv-5)Sub-Plinian-4954.5240IntCal09doi:10.1111/j.1502-3885.1992.tb00009.xTransitional alkali basalt. Dated at Lake Torfadalsvatn to 6000 ± 140 14C yr BP (c.7240-6500 cal BP, 2 sigma). Possibly the mid-distal equivalent of Mjauvotn A tephra on the Faroes (Wastegard 2001). On the basis of major element geochemistry believed to be from Katla.
    SILK-A1Sub-Plinian-4009.5207IntCal09doi:10.1002/jqs.724c. 5170 ± 85 14C yr BP (Wastegard 2002, JQS 17(8), 723-730). Calibrates to 6182-5730 yr cal BP (2 sigma).
    SILK-A7Sub-Plinian-5189.5123IntCal09doi:10.1002/jqs.724c. 6245 ± 90 14C yr BP calibrates to 7415-6932 yr cal BP (2 sigma; Wastegard 2002)
    SILK-YNSub-Plinian310.570IntCal09doi:10.1179/env.2000.5.1.21There are three 14C ages for this tephra, from 1500 ± 70 to 1880 ± 60 14C yr BP. Dugmore et al. (2000) argue for an age of 1740 ± 50 14C yr BP. Calibrated age range of 1811-1539 cal BP (2 sigma).
    Suduroy tephraPlinian-6119.590IntCal09doi:10.1002/jqs.724Rhyolitic ash layer, c. 7240 ± 95 14C yr BP calibrates to 8310-7868 cal BP (2 sigma; Wastegard 2002, JQS 17(8), 723-730).
    NGRIP 1508.26mSub-Plinian-10249.51GICC05doi:10.1029/2005jd006079Rhyolitic ash layer. NGRIP GICC05 age of 12250 ± 117 b2k years
    NGRIP 1573.00mSub-Plinian-12019.51GICC05doi:10.1029/2005jd006079Basalt layer. NGRIP GICC05 14020 ± 167 b2k.
    Dimna AshPlinian-13149.5300IntCal04doi:10.1016/j.quascirev.2007.04.021Rhyolitic ash that is below radiocarbon age of 12780 ± 60 14C yr BP (15400-14850 cal BP) on terrestrial plant macrofossils (Koren et al. 2008)
    AF555Plinian-9544.5295IntCal09doi:10.1002/jqs.1498Rhyolitic ash layer. Bayesian age model 11.79-11.20 cal ka BP
    Solheimar IgnimbritePhreato-Plinian-10149.5700doi:10.1007/bf00298704correlated with Vedde Ash and dated to Younger Dryas Stadial.
    NGRIP 1861.55mSub-Plinian-25526.51GICC05doi:10.1016/j.epsl.2010.03.004Transitional alkali basalt; GICC05 age of 27527 ± 410 b2k
    NGRIP 1895.24mSub-Plinian-27129.51GICC05doi:10.1016/j.epsl.2010.03.004Transitional alkali basalt; GICC05 age of 29130 ± 456 b2k
    IA2Sub-Plinian-11199.5146Orbitaldoi:10.1016/s0277-3791(00)00146-3Ice rafted rhyolitic ash layer, Bond et al. (2001) assigns this to GI-1b which has a GICC05 age range of 13311-13099 b2k (± 146).
    Skopun tephraPlinian-7799.5100IntCal09doi:10.1016/j.quaint.2011.05.01414C modeled age of 9850-9650 yr cal BP (Lind & Wastegard 2011).
    St. 5a-TAB-1Plinian-73449.55000Orbitaldoi:10.1016/0012-821x(95)00145-3TAB geochemical composition
    St. 5a-TAB-2Plinian-75549.55000Orbitaldoi:10.1016/0012-821x(95)00145-3TAB geochemical composition
    Tjornuvik AD800 B_Distribution
    • series: Tjornuvik AD800 B_Distribution
    • series_type: Tephra_Distribution
    • eruption: Tjornuvik AD800 B
    sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
    Borg IndrepollenNorway13.4940004368.14499664TerrestrialQUEST636/54distalfallashquest
    Vedde Ash_Distribution
    • series: Vedde Ash_Distribution
    • series_type: Tephra_Distribution
    • eruption: Vedde Ash
    sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
    GurskøyNorway5.55788993862.3708992TerrestrialQUEST637/3distalfallashquest
    KvaltjernNorway4.98140001360.42309952TerrestrialQUEST639/3distalfallashquest
    Lake KullatorpssjönSweden12.4877004656.2941017289TerrestrialQUEST692/3distalfallashquest
    Lake MullsjönSweden14.3607997958.36930084133TerrestrialQUEST695/3distalfallashquest
    Lerstadvatn, ÅlesondNorway6.26099014362.36729813TerrestrialQUEST641/3distalfallashquest
    Lake GjølvatnNorway6.25216007262.43230057TerrestrialQUEST640/3distalfallashquest
    LillerestjønnNorway6.3170499862.46889877TerrestrialQUEST642/3distalfallashquest
    SaudedalsmyraNorway6.23669004462.43389893TerrestrialQUEST643/3distalfallashquest
    Lac de SewenFrance6.89722013547.81169891500TerrestrialQUEST823/3distalfallashquest

    Krafla

    Data series

    Oraefajokull

    Data series

    Eruptions
    • series: Eruptions
    • series_type: Volc_Eruptions
    eruptioneruption_typett_sigmat_sourcerefnotes
    Oraefajokull AD1727Plinian1727.51Calendardoi:10.1191/095968399669624108AD 1727 historical
    Oraefajokull AD1362Ultra-Plinian1362.51Calendardoi:10.1191/095968399669624108AD 1362 historical (see Thorarinsson 1958; Larsen et al. 1999)
    Oraefajokull AD1362_Distribution
    • series: Oraefajokull AD1362_Distribution
    • series_type: Tephra_Distribution
    • eruption: Oraefajokull AD1362
    sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
    BødalsvatnettNorway13.5620002768.196998642TerrestrialQUEST634/67distalfallashquest

    Snaefellsjokull

    Data series

    Eruptions
    • series: Eruptions
    • series_type: Volc_Eruptions
    eruptioneruption_typett_sigmat_sourcerefnotes
    Sn-2Sub-Plinian-2454.5163IntCal09ref:johannesson1981sahc. 3960 ± 100 14C yr BP (Jóhannesson et al. 1981). Calibrates to 4813-4095 yr cal BP (2 sigma).
    SSn (Svinavatn)Sub-Plinian-7499.550c. 7500 BC radiocarbon
    HogstorpsmossenPlinian-8347.5108IntCal09doi:10.1002/(sici)1099-1417(199908)14:5<399::aid-jqs448>3.0.co;2-rBracketed by two 14C ages in inverted sequence: 9255 ± 145 and 8980 ± 125 14C yr BP (Bjorck & Wastegard 1999). Weighted mean calibrated age range of 10,556-9931 yr cal BP (2 sigma).
    Hovsdalur tephraSub-Plinian-8524.5175IntCal09doi:10.1002/jqs.724c. 9300 ± 85 14C yr BP; i.e. 10,695-10,285 cal BP (2 sigma; Wastegard et al. 2002).
    Hasseldalen tephraPlinian-9437.5156IntCal04doi:10.1002/jqs.996c. 11,543-11,232 cal BP bayesian 14C wiggle-match (Wohlfarth et al. 2006).
    Sn-1Sub-Plinian170.545IntCal09doi:10.3402/polar.v21i2.6489c. 1855 ± 25 14C yr BP on peaty soil (Larsen et al. 2002). Calibrates to 1865-1720 yr cal BP (2 sigma).

    Torfajökull

    Data series

    Eruptions
    • series: Eruptions
    • series_type: Volc_Eruptions
    eruptioneruption_typett_sigmat_sourcerefnotes
    Landnam (silicic)Sub-Plinian871.51GICC05doi:10.1016/0012-821x(95)00145-3c. AD 871 ± 2 (GRIP). The Landnám tephra layer is characterised by two distinct tephra components: a lower rhyolitic tephra layer which is overlain by a basaltic tephra layer. Both of these were deposited following the ~AD 871 Vatnaöldur eruption which saw simultaneous eruptions of the basaltic Veidivötn-Bárðarbunga volcanic system and the silicic Torfajökull complex.
    HoyPlinian-4399.550doi:10.1191/0959683602hl538rrc. 4400 BC radiocarbon (Hall & Pilcher 2002).
    Lairg B / Torfajökull 4700 BCPlinian-4694.541doi:10.1191/0959683602hl538rrc. 4774-4677 cal BC 14C wiggle-match (Pilcher et al. 1996; Hall & Pilcher 2002).
    An DruimPlinian-7609.540IntCal09doi:10.1002/jqs.910c. 9633-9488 yr cal BP by Turney et al. (2006). Ranner et al. (2005) cites at age of 8590 ± 50 14C yr BP, which calibrates to 9671-9490 yr cal BP (2 sigma).
    Ashik ashPlinian-8449.5300doi:10.1002/jqs.1066position below the Saksunarvatn tephra and above the Vedde Ash indicates an early Holocene age. Pyne-O'Donnell (2007) places it above the Pre-Boreal Oscillation.
    Torfajökull AD1477Ultra-Plinian1477.51Calendardoi:10.1191/095968399669624108AD 1477 historical (the eruption was triggered by rifting within the Veidivotn volcanic system). Sometimes called Veidivotn AD1477. Larsen (1984) suggests an age of 1480 ± 11.
    Gullbergby tephraPlinian-749.5100doi:10.1016/j.quaint.2004.04.030c. 2700 cal yr BP interpolated (Wastegard 2005)
    Høvdarhagi tephraPlinian-7774.5125IntCal09doi:10.1016/j.quaint.2011.05.01414C modeled age of 9850-9600 yr cal BP (Lind & Wastegard 2011).
    Lairg B / Torfajökull 4700 BC_Distribution
    • series: Lairg B / Torfajökull 4700 BC_Distribution
    • series_type: Tephra_Distribution
    • eruption: Lairg B / Torfajökull 4700 BC
    sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
    ToomeUK-6.46179008554.75170135TerrestrialQUEST632/75distalfallashquest

    Veidivotn

    Data series

    Eruptions
    • series: Eruptions
    • series_type: Volc_Eruptions
    eruptioneruption_typett_sigmat_sourcerefnotes
    Veidivotn AD1717Sub-Plinian1717.51Calendardoi:10.1111/j.1502-3885.2007.tb01176.xAD 1717 historical
    SvVSub-Plinian-659.5300doi:10.1016/s0921-8181(99)00011-9c. 2500 14C yr BP at Svinavatn, N Iceland (Boygle 1999)
    FMAZ I-THOLPlinian-16649.5500Marine04doi:10.1016/j.quascirev.2006.03.001tholeiitic ash layer dated to c. 15,400 14C yr BP in Wastegard et al. (2006). Thought to be equivalent to 15.4 ka BAS-1 of Haflidarson et al. (2000).
    NGRIP 1595.1mSub-Plinian-12499.51GICC05doi:10.1002/jqs.908cf. 15.4 ka-BAS-1 tephra based on major element chemistry but SS09 age of 14428-14431 ice core years makes such a correlation highly unlikely. The depth suggests a GICC05 age of 14500 ± 180 b2k.
    I-THOL-1 (Tv-3)Sub-Plinian-9064.5225doi:10.1111/j.1502-3885.1992.tb00009.xOne of components of NAAZ I with age of ~10.4 ka 14C yr BP (Kvamme et al. 1989). Could be equivalent of Tv-3 in lake Torfadalsvatn with age of ~9.7 ka 14C yr BP (Bjorck et al., 1992).
    Sandoy BPlinian-9279.542IntCal09doi:10.1016/j.quaint.2011.05.01414C modeled age of 11,288-11,205 yr cal BP (Lind & Wastegard 2011)
    Sandoy APlinian-9379.542IntCal09doi:10.1016/j.quaint.2011.05.01414C modeled age of 11,388-11,305 yr cal BP
    Landnam (basaltic)Sub-Plinian871.51GICC05doi:10.1016/0012-821x(95)00145-3c. AD 871 ± 2 (GRIP). The Landnám tephra layer is characterised by two distinct tephra components: a lower rhyolitic tephra layer which is overlain by a basaltic tephra layer. Both of these were deposited following the ~AD 871 Vatnaöldur eruption which saw simultaneous eruptions of the basaltic Veidivötn-Bárðarbunga volcanic system and the silicic Torfajökull complex.

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