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Glen_West

Data series

QUEST562/111_Majors
  • series: QUEST562/111_Majors
  • series_type: Tephra_Sample_Majors
  • z: 0.1
  • z_range: 0.02
  • sample: QUEST562/111
  • context: AD860 Layer part B
  • tephra_type: distal
  • tephra_deposit: fall
  • material: ash
  • collected_by: quest
  • volc_region: Iceland
  • volcano: Iceland_volcanoes
  • eruption: AD860 Layer part B
  • notes: QUB483; includes 2 outliers
labcodebatchinstrumentSiO2TiO2Al2O3FeOtMnOMgOCaONa2OK2OP2O5ClFtotalok
QUEST562/111/01QUEST-30QUEST-WDS69.950.2714.111.5500.471.974.273.1400095.721
QUEST562/111/02QUEST-30QUEST-WDS69.990.2514.171.4600.411.843.943.0100095.051
QUEST562/111/03QUEST-30QUEST-WDS70.910.2614.281.4600.441.924.252.9600096.481
QUEST562/111/04QUEST-30QUEST-WDS71.060.2714.481.6200.441.884.323.0900097.171
QUEST562/111/05QUEST-30QUEST-WDS71.070.2514.451.4600.421.824.163.200096.821
QUEST562/111/06QUEST-30QUEST-WDS71.350.2714.581.5800.481.984.343.1500097.731
QUEST562/111/07QUEST-30QUEST-WDS71.560.2714.741.600.481.884.21300097.731
QUEST562/111/08QUEST-30QUEST-WDS71.680.2914.61.6300.451.934.253.0800097.91
QUEST562/111/09QUEST-30QUEST-WDS72.190.2614.581.5400.462.014.313.0900098.451
QUEST562/111/10QUEST-30QUEST-WDS72.420.2914.641.5500.421.954.183.0500098.491
QUEST562/111/11QUEST-30QUEST-WDS72.520.2714.741.5600.442.054.323.0300098.921
QUEST562/111/12QUEST-30QUEST-WDS72.530.314.571.5100.461.974.453.200098.981
QUEST562/111/13QUEST-30QUEST-WDS72.730.3114.731.5700.461.934.413.100099.251
QUEST562/111/14QUEST-30QUEST-WDS72.90.314.541.500.41.934.433.0900099.081
QUEST562/111/15outQUEST-30QUEST-WDS67.790.9713.894.8200.742.194.613.1100099.131
QUEST562/111/16outQUEST-30QUEST-WDS69.260.8214.344.7800.692.054.563.200099.711
QUEST562/112_Majors
  • series: QUEST562/112_Majors
  • series_type: Tephra_Sample_Majors
  • z: 1.035
  • z_range: 0.01
  • sample: QUEST562/112
  • context: OMH-185 (Barnsmore)
  • tephra_type: distal
  • tephra_deposit: fall
  • material: ash
  • collected_by: quest
  • volc_region: Iceland
  • volcano: Iceland_volcanoes
  • eruption: OMH-185 (Barnsmore)
  • notes: QUB473; 2 populations and 2 outliers
labcodebatchinstrumentSiO2TiO2Al2O3FeOtMnOMgOCaONa2OK2OP2O5ClFtotalok
QUEST562/112/01pop1QUEST-30QUEST-WDS69.680.2112.331.2800.160.92.873.9700091.391
QUEST562/112/02pop1QUEST-30QUEST-WDS70.580.2312.281.5400.10.952.783.9200092.381
QUEST562/112/03pop1QUEST-30QUEST-WDS70.650.1912.241.5500.10.843.663.9500093.171
QUEST562/112/04pop1QUEST-30QUEST-WDS70.690.1912.131.2600.140.942.74.1800092.231
QUEST562/112/05pop1QUEST-30QUEST-WDS72.050.1912.121.5500.180.943.813.6100094.451
QUEST562/112/06pop1QUEST-30QUEST-WDS73.430.2312.21.4300.130.963.863.6600095.91
QUEST562/112/07pop2QUEST-30QUEST-WDS70.980.6312.773.0200.451.23.513.8300096.41
QUEST562/112/08outQUEST-30QUEST-WDS71.960.2813.071.2200.331.634.242.7600095.481
QUEST562/112/09outQUEST-30QUEST-WDS71.330.412.911.5600.341.744.222.5400095.041
QUEST562/41_Majors
  • series: QUEST562/41_Majors
  • series_type: Tephra_Sample_Majors
  • z: 0.98
  • z_range: 0.02
  • sample: QUEST562/41
  • context: BMR-190
  • tephra_type: distal
  • tephra_deposit: fall
  • material: ash
  • collected_by: quest
  • volc_region: EVZ
  • volcano: Hekla
  • eruption: BMR-190
  • notes: QUB447
labcodebatchinstrumentSiO2TiO2Al2O3FeOtMnOMgOCaONa2OK2OP2O5ClFtotalok
QUEST562/41/01QUEST-30QUEST-WDS62.640.7314.98.7900.993.774.81.400098.021
QUEST562/41/02QUEST-30QUEST-WDS62.990.5817.555.702.164.94.621.1700099.671
QUEST562/41/03QUEST-30QUEST-WDS63.560.815.425.4401.334.214.491.700096.951
QUEST562/41/04QUEST-30QUEST-WDS64.120.6617.284.9400.964.665.071.300098.981
QUEST562/41/05QUEST-30QUEST-WDS64.270.715.45.3601.364.194.451.5200097.241
QUEST562/41/06QUEST-30QUEST-WDS64.570.915.586.2301.334.324.341.7100099.971
QUEST562/41/07QUEST-30QUEST-WDS64.830.8216.026.7501.493.864.381.5200099.661
QUEST562/41/08QUEST-30QUEST-WDS65.070.8615.685.7601.364.414.741.600099.481
QUEST562/41/09QUEST-30QUEST-WDS65.220.8615.386.3101.324.094.221.500098.911
QUEST562/41/10QUEST-30QUEST-WDS65.380.8215.855.9501.343.594.351.4700098.731
QUEST562/41/11QUEST-30QUEST-WDS65.390.8715.546.3501.264.094.611.5600099.671
QUEST562/41/12QUEST-30QUEST-WDS65.410.8715.645.8401.343.844.111.700098.761
QUEST562/41/13QUEST-30QUEST-WDS65.520.815.725.8801.33.64.321.4600098.591
QUEST562/41/14QUEST-30QUEST-WDS65.680.8915.276.1101.264.4641.7300099.391
QUEST562/41/15QUEST-30QUEST-WDS65.960.8715.476.1801.294.213.781.7200099.481
QUEST562/41/16QUEST-30QUEST-WDS66.531.0414.237.0601.343.854.071.7300099.851
QUEST562/41/17QUEST-30QUEST-WDS66.870.8115.785.4901.313.774.321.5100098.861
QUEST562/47_Majors
  • series: QUEST562/47_Majors
  • series_type: Tephra_Sample_Majors
  • z: 1.74
  • z_range: 0.02
  • sample: QUEST562/47
  • context: H4 Hekla
  • tephra_type: distal
  • tephra_deposit: fall
  • material: ash
  • collected_by: quest
  • volc_region: EVZ
  • volcano: Hekla
  • eruption: H4 Hekla
  • notes: QUB454; 4 other analyses not entered as they seem to derive from an eruption of Katla
labcodebatchinstrumentSiO2TiO2Al2O3FeOtMnOMgOCaONa2OK2OP2O5ClFtotalok
QUEST562/47/01QUEST-30QUEST-WDS71.70.1612.991.98001.564.442.9500095.781
QUEST562/47/02QUEST-30QUEST-WDS71.860.1712.921.84001.344.432.6500095.211
QUEST562/47/03QUEST-30QUEST-WDS72.340.1513.031.8700.041.424.522.6200095.991
QUEST562/47/04QUEST-30QUEST-WDS72.680.1313.151.8700.051.44.322.6600099.241
QUEST562/47/05QUEST-30QUEST-WDS73.350.1913.041.8700.041.414.532.7500097.181
QUEST562/47/06QUEST-30QUEST-WDS73.410.1212.341.6100.041.23.953.4600096.141
QUEST562/78_Majors
  • series: QUEST562/78_Majors
  • series_type: Tephra_Sample_Majors
  • z: 1.095
  • z_range: 0.01
  • sample: QUEST562/78
  • context: GB4-150
  • tephra_type: distal
  • tephra_deposit: fall
  • material: ash
  • collected_by: quest
  • volc_region: EVZ
  • volcano: Katla
  • eruption: GB4-150
  • notes: QUB493
labcodebatchinstrumentSiO2TiO2Al2O3FeOtMnOMgOCaONa2OK2OP2O5ClFtotalok
QUEST562/78/01QUEST-30QUEST-WDS65.791.4714.45.6901.443.454.672.6700099.581
QUEST562/78/02QUEST-30QUEST-WDS65.591.514.285.9101.453.674.572.5500099.521
Tephra_Samples
  • series: Tephra_Samples
  • series_type: Tephra_Samples
zz_rangesamplett_sigmacontextsectortephra_typetephra_depositmaterialtephra_shardstephra_shards_absvolc_regionvolcanoeruptionnotes
1.0950.01QUEST562/78-777.521GB4-150distalfallash99990EVZKatlaGB4-150QUB493
0.10.02QUEST562/111860.520AD860 Layer part Bdistalfallash99990IcelandIceland_volcanoesAD860 Layer part BQUB483; includes 2 outliers
0.980.02QUEST562/41-643.560BMR-190distalfallash99990EVZHeklaBMR-190QUB447
1.740.02QUEST562/47-2309.520H4 Hekladistalfallash99990EVZHeklaH4 HeklaQUB454; 4 other analyses not entered as they seem to derive from an eruption of Katla
1.0350.01QUEST562/112-716.538OMH-185 (Barnsmore)distalfallash99990IcelandIceland_volcanoesOMH-185 (Barnsmore)QUB473; 2 populations and 2 outliers
Tephras
  • series: Tephras
  • series_type: Tephras
zz_rangett_sigmasamplevolc_regionvolcanoeruptionref
0.10.02860.520QUEST562/111IcelandIceland_volcanoesAD860 Layer part Bdoi:10.1191/0959683604hl757rr
1.0350.01-716.538QUEST562/112IcelandIceland_volcanoesOMH-185 (Barnsmore)doi:10.1191/0959683604hl757rr
0.980.02-643.560QUEST562/41EVZHeklaBMR-190doi:10.1191/0959683604hl757rr
1.740.02-2309.520QUEST562/47EVZHeklaH4 Hekladoi:10.1191/0959683604hl757rr
1.0950.01-777.521QUEST562/78EVZKatlaGB4-150doi:10.1191/0959683604hl757rr

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

Iceland_volcanoes

Data series

Eruptions
  • series: Eruptions
  • series_type: Volc_Eruptions
eruptioneruption_typett_sigmat_sourcerefnotes
PMG-5Plinian1600.5100doi:10.1191/0959683602hl538rrpossibly c. AD 1600 interpolated (Hall & Pilcher 2002).
BIP-24Plinian900.5100doi:10.1111/j.1502-3885.2005.tb01011.xc. AD 900 interpolated
AD860 Layer part BPlinian860.520doi:10.1177/095968369500500111c. AD 860 ± 20 radiocarbon wiggle-match at Sluggan (AD lower layer, colourless tephra shards, two populations)
OMH-185 (Barnsmore)Plinian-716.538IntCal04doi:10.1191/0959683604hl757rrc. 755-680 cal BC (Plunkett et al. 2004). According to Hall and Pilcher (2002) this is probably equivalent to the DOM-6 'microlite' tephra in Germany.
Derrycunihy Wood SH-1Plinian
FMAZ II (Fugloyarbanki)Plinian-24739.51GICC05doi:10.1002/jqs.118226740 ± 390 yr b2k in NGRIP 1848.05
BorrobolPlinian-12094.595IntCal09doi:10.1002/jqs.1498Best current estimate is 14.14-13.95 cal ka BP (Bayesian age model). Replaces Turney et al. (1997) date of c.14.4 cal ka BP. Davies et al. (2004) suggestion of 2 eruptions has been revised by Matthews et al. (2011).
L3574PlinianNo age given, reported as 'older than Saksunarvatn tephra' by Dugmore and Newton (1997). Turney et al. (2006) suggests an age of c. 10.8 ka cal. BP.
OWB-105 AD700Plinian700.5100doi:10.1191/0959683602hl538rrc. AD 700 interpolated (Hall & Pilcher 2002).
Penifiler TephraPlinian-11929.5200IntCal09doi:10.1002/jqs.149814.08-13.68 cal ka BP (Bayesian age model)
Sluggan APlinian-12549.5500doi:10.1002/jqs.990c. 14500 cal BP suggested by Turney et al. (2006)
Sluggan BPlinian-10849.5500doi:10.1002/jqs.990c. 12800 cal BP suggested by Turney et al. (2006)
AD860 Layer part APlinian860.520doi:10.1177/095968369500500111c. AD 860 ± 20 radiocarbon wiggle-match at Sluggan (AD lower layer, colourless tephra shards, two populations)
BMR-90 AD920Plinian920.5100doi:10.1191/0959683602hl538rrc. AD 920 interpolated (Hall & Pilcher 2002)
Breakish TephraPliniandoi:10.1002/jqs.1066no date suggested although position above the Ashik tephra and Saksunarvatn indicates an age in the early-mid Holocene.
DOM-6 'microlite' tephraPlinian-696.535doi:10.1006/qres.2002.2325c. 730-664 cal BC radiocarbon (van den Bogaard et al. 2002). According to Hall & Pilcher (2002) this is probably equivalent to the OMH-185 (Barnsmore) tephra.
GB4-182Plinian-1349.5200doi:10.1191/0959683602hl538rrc. 1350 cal BC interpolated (Hall & Pilcher 2002)
GB4-50 AD1250Plinian1250.5100doi:10.1191/0959683602hl538rrc. AD 1250 interpolated (Hall & Pilcher 2002)
Harthorpe Moss tephraPliniandoi:10.1177/095968369600600112
Lough Portain BPlinian0doi:10.1177/095968369500500301sub-population of Hekla AD 1510 eruption (Lough Portain A). Status is unclear, not a distinct isochrone
MOR-T4Plinian1000.5100doi:10.1191/0959683604hl749rpc. cal AD 1000 interpolated (Chambers et al. 2004)
Roddans Port APliniandoi:10.1002/jqs.990two sub-populations (A & B) at 63-64 cm depth, dating unclear, pre-Vedde Ash.
Roddans Port BPliniandoi:10.1002/jqs.990two sub-populations (A & B) at 63-64 cm depth, dating unclear, pre-Vedde Ash.
SLU-5Plinian1650.550doi:10.1191/0959683602hl538rrc. AD 1600-1700 interpolated (Hall & Pilcher 2002)
Stomyren tephraPlinian-149.5100doi:10.1016/j.quaint.2004.04.030c. 2100 cal yr BP interpolated (Wastegard 2005)
Vallensgard Mose tephraPliniandoi:10.1002/jqs.990Stratigraphic position is similar to Vedde Ash, in the middle of the Younger Dryas, but geochemistry is different. Unclear if this is a significant tephra horizon.
NAAZ IPlinian-10449.5500Marine04doi:10.1016/j.quascirev.2006.03.001Diffuse layer representing c. 11 ka 14C yr GS-1 ash zone containing components from I-Thol-2 (Grímsvötn), I-Rhy.1 (Katla) and I-Thol-1 (Veidivötn). It is commonly believed that the biggest contributor is the rhyolitic component of the Vedde Ash.
L-274Plinian-8274.5100IntCal09doi:10.1016/j.quaint.2011.05.01414C modeled age of 10,325-10,125 yr cal BP (Lind & Wastegard 2011).
5d-BASPlinian-109549.55000Orbitaldoi:10.1016/s0277-3791(98)00038-9Probably represents an eruption complex. Several geochemical populations: BAS-I, BAS-II, BAS-III.
5e-MidtPlinian-123049.55000Orbitaldoi:10.1016/s0277-3791(98)00038-9Probably represents an eruption complex. Several geochemical populations: RHY, INT, BAS & TAB (the 5e-Midt/TRACHY is believed to be from Jan Mayen). Wallrabe-Adams & Lackschewitz (2002) suggest either Vatnafjoll or Vestmannaeyjar may be the source.
5e-LowPlinian-127549.55000Orbitaldoi:10.1016/s0277-3791(98)00038-9Probably represents an eruption complex. Several geochemical populations. Wallrabe-Adams & Lackschewitz (2002) suggest either Vatnafjoll or Vestmannaeyjar may be the source.
St. 5a-THOL-1Plinian-74549.55000Orbitaldoi:10.1016/0012-821x(95)00145-3THOL geochemical composition
St. 7-RHY-I & IIPlinian-208049.520000Orbitaldoi:10.1002/jqs.3390060205RHY-I & RHY-II geochemical compositions
St. 7-BAS/INT-IPlinian-208549.520000Orbitaldoi:10.1002/jqs.3390060205INT-I & INT/BAS-I geochemical compositions
St. 9-RHY-IPlinian-328049.530000Orbitaldoi:10.1002/jqs.3390060205RHY geochemical composition; possible equivalent to NAAZ III (III-RHY-I, c.320 ka)
St. 9-BAS-IPlinian-328049.530000Orbitaldoi:10.1002/jqs.3390060205BAS geochemcial composition
AD860 Layer part B_Distribution
  • series: AD860 Layer part B_Distribution
  • series_type: Tephra_Distribution
  • eruption: AD860 Layer part B
sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
Ballysculllian EastUK-6.46299982154.7975006144TerrestrialQUEST621/111distalfallashquest
Borg IndrepollenNorway13.4940004368.14499664TerrestrialQUEST636/111distalfallashquest
BIP-24_Distribution
  • series: BIP-24_Distribution
  • series_type: Tephra_Distribution
  • eruption: BIP-24
sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
Borg IndrepollenNorway13.4940004368.14499664TerrestrialQUEST636/110distalfallashquest
Derrycunihy Wood SH-1_Distribution
  • series: Derrycunihy Wood SH-1_Distribution
  • series_type: Tephra_Distribution
  • eruption: Derrycunihy Wood SH-1
sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
Derrycunihy WoodIreland-9.41666984652.01670074TerrestrialQUEST580/113distalfallashquest
NAAZ I_Distribution
  • series: NAAZ I_Distribution
  • series_type: Tephra_Distribution
  • eruption: NAAZ I
sitecountrylongitudelatitudeelevationsite_typesampletephra_typetephra_depositmaterialz_rangecollectedcollected_bynotes
K708-1-23.7550-4053MarineQUEST709/3distalfallashquest

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

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