IntChron > doi > 10.1191 > 0959683604hl757rr
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| QUEST562/111/01 | QUEST-30 | QUEST-WDS | 69.95 | 0.27 | 14.11 | 1.55 | 0 | 0.47 | 1.97 | 4.27 | 3.14 | 0 | 0 | 0 | 95.72 | 1 | ||
| QUEST562/111/02 | QUEST-30 | QUEST-WDS | 69.99 | 0.25 | 14.17 | 1.46 | 0 | 0.41 | 1.84 | 3.94 | 3.01 | 0 | 0 | 0 | 95.05 | 1 | ||
| QUEST562/111/03 | QUEST-30 | QUEST-WDS | 70.91 | 0.26 | 14.28 | 1.46 | 0 | 0.44 | 1.92 | 4.25 | 2.96 | 0 | 0 | 0 | 96.48 | 1 | ||
| QUEST562/111/04 | QUEST-30 | QUEST-WDS | 71.06 | 0.27 | 14.48 | 1.62 | 0 | 0.44 | 1.88 | 4.32 | 3.09 | 0 | 0 | 0 | 97.17 | 1 | ||
| QUEST562/111/05 | QUEST-30 | QUEST-WDS | 71.07 | 0.25 | 14.45 | 1.46 | 0 | 0.42 | 1.82 | 4.16 | 3.2 | 0 | 0 | 0 | 96.82 | 1 | ||
| QUEST562/111/06 | QUEST-30 | QUEST-WDS | 71.35 | 0.27 | 14.58 | 1.58 | 0 | 0.48 | 1.98 | 4.34 | 3.15 | 0 | 0 | 0 | 97.73 | 1 | ||
| QUEST562/111/07 | QUEST-30 | QUEST-WDS | 71.56 | 0.27 | 14.74 | 1.6 | 0 | 0.48 | 1.88 | 4.21 | 3 | 0 | 0 | 0 | 97.73 | 1 | ||
| QUEST562/111/08 | QUEST-30 | QUEST-WDS | 71.68 | 0.29 | 14.6 | 1.63 | 0 | 0.45 | 1.93 | 4.25 | 3.08 | 0 | 0 | 0 | 97.9 | 1 | ||
| QUEST562/111/09 | QUEST-30 | QUEST-WDS | 72.19 | 0.26 | 14.58 | 1.54 | 0 | 0.46 | 2.01 | 4.31 | 3.09 | 0 | 0 | 0 | 98.45 | 1 | ||
| QUEST562/111/10 | QUEST-30 | QUEST-WDS | 72.42 | 0.29 | 14.64 | 1.55 | 0 | 0.42 | 1.95 | 4.18 | 3.05 | 0 | 0 | 0 | 98.49 | 1 | ||
| QUEST562/111/11 | QUEST-30 | QUEST-WDS | 72.52 | 0.27 | 14.74 | 1.56 | 0 | 0.44 | 2.05 | 4.32 | 3.03 | 0 | 0 | 0 | 98.92 | 1 | ||
| QUEST562/111/12 | QUEST-30 | QUEST-WDS | 72.53 | 0.3 | 14.57 | 1.51 | 0 | 0.46 | 1.97 | 4.45 | 3.2 | 0 | 0 | 0 | 98.98 | 1 | ||
| QUEST562/111/13 | QUEST-30 | QUEST-WDS | 72.73 | 0.31 | 14.73 | 1.57 | 0 | 0.46 | 1.93 | 4.41 | 3.1 | 0 | 0 | 0 | 99.25 | 1 | ||
| QUEST562/111/14 | QUEST-30 | QUEST-WDS | 72.9 | 0.3 | 14.54 | 1.5 | 0 | 0.4 | 1.93 | 4.43 | 3.09 | 0 | 0 | 0 | 99.08 | 1 | ||
| QUEST562/111/15out | QUEST-30 | QUEST-WDS | 67.79 | 0.97 | 13.89 | 4.82 | 0 | 0.74 | 2.19 | 4.61 | 3.11 | 0 | 0 | 0 | 99.13 | 1 | ||
| QUEST562/111/16out | QUEST-30 | QUEST-WDS | 69.26 | 0.82 | 14.34 | 4.78 | 0 | 0.69 | 2.05 | 4.56 | 3.2 | 0 | 0 | 0 | 99.71 | 1 |
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| QUEST562/112/01pop1 | QUEST-30 | QUEST-WDS | 69.68 | 0.21 | 12.33 | 1.28 | 0 | 0.16 | 0.9 | 2.87 | 3.97 | 0 | 0 | 0 | 91.39 | 1 | ||
| QUEST562/112/02pop1 | QUEST-30 | QUEST-WDS | 70.58 | 0.23 | 12.28 | 1.54 | 0 | 0.1 | 0.95 | 2.78 | 3.92 | 0 | 0 | 0 | 92.38 | 1 | ||
| QUEST562/112/03pop1 | QUEST-30 | QUEST-WDS | 70.65 | 0.19 | 12.24 | 1.55 | 0 | 0.1 | 0.84 | 3.66 | 3.95 | 0 | 0 | 0 | 93.17 | 1 | ||
| QUEST562/112/04pop1 | QUEST-30 | QUEST-WDS | 70.69 | 0.19 | 12.13 | 1.26 | 0 | 0.14 | 0.94 | 2.7 | 4.18 | 0 | 0 | 0 | 92.23 | 1 | ||
| QUEST562/112/05pop1 | QUEST-30 | QUEST-WDS | 72.05 | 0.19 | 12.12 | 1.55 | 0 | 0.18 | 0.94 | 3.81 | 3.61 | 0 | 0 | 0 | 94.45 | 1 | ||
| QUEST562/112/06pop1 | QUEST-30 | QUEST-WDS | 73.43 | 0.23 | 12.2 | 1.43 | 0 | 0.13 | 0.96 | 3.86 | 3.66 | 0 | 0 | 0 | 95.9 | 1 | ||
| QUEST562/112/07pop2 | QUEST-30 | QUEST-WDS | 70.98 | 0.63 | 12.77 | 3.02 | 0 | 0.45 | 1.2 | 3.51 | 3.83 | 0 | 0 | 0 | 96.4 | 1 | ||
| QUEST562/112/08out | QUEST-30 | QUEST-WDS | 71.96 | 0.28 | 13.07 | 1.22 | 0 | 0.33 | 1.63 | 4.24 | 2.76 | 0 | 0 | 0 | 95.48 | 1 | ||
| QUEST562/112/09out | QUEST-30 | QUEST-WDS | 71.33 | 0.4 | 12.91 | 1.56 | 0 | 0.34 | 1.74 | 4.22 | 2.54 | 0 | 0 | 0 | 95.04 | 1 |
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| QUEST562/41/01 | QUEST-30 | QUEST-WDS | 62.64 | 0.73 | 14.9 | 8.79 | 0 | 0.99 | 3.77 | 4.8 | 1.4 | 0 | 0 | 0 | 98.02 | 1 | ||
| QUEST562/41/02 | QUEST-30 | QUEST-WDS | 62.99 | 0.58 | 17.55 | 5.7 | 0 | 2.16 | 4.9 | 4.62 | 1.17 | 0 | 0 | 0 | 99.67 | 1 | ||
| QUEST562/41/03 | QUEST-30 | QUEST-WDS | 63.56 | 0.8 | 15.42 | 5.44 | 0 | 1.33 | 4.21 | 4.49 | 1.7 | 0 | 0 | 0 | 96.95 | 1 | ||
| QUEST562/41/04 | QUEST-30 | QUEST-WDS | 64.12 | 0.66 | 17.28 | 4.94 | 0 | 0.96 | 4.66 | 5.07 | 1.3 | 0 | 0 | 0 | 98.98 | 1 | ||
| QUEST562/41/05 | QUEST-30 | QUEST-WDS | 64.27 | 0.7 | 15.4 | 5.36 | 0 | 1.36 | 4.19 | 4.45 | 1.52 | 0 | 0 | 0 | 97.24 | 1 | ||
| QUEST562/41/06 | QUEST-30 | QUEST-WDS | 64.57 | 0.9 | 15.58 | 6.23 | 0 | 1.33 | 4.32 | 4.34 | 1.71 | 0 | 0 | 0 | 99.97 | 1 | ||
| QUEST562/41/07 | QUEST-30 | QUEST-WDS | 64.83 | 0.82 | 16.02 | 6.75 | 0 | 1.49 | 3.86 | 4.38 | 1.52 | 0 | 0 | 0 | 99.66 | 1 | ||
| QUEST562/41/08 | QUEST-30 | QUEST-WDS | 65.07 | 0.86 | 15.68 | 5.76 | 0 | 1.36 | 4.41 | 4.74 | 1.6 | 0 | 0 | 0 | 99.48 | 1 | ||
| QUEST562/41/09 | QUEST-30 | QUEST-WDS | 65.22 | 0.86 | 15.38 | 6.31 | 0 | 1.32 | 4.09 | 4.22 | 1.5 | 0 | 0 | 0 | 98.91 | 1 | ||
| QUEST562/41/10 | QUEST-30 | QUEST-WDS | 65.38 | 0.82 | 15.85 | 5.95 | 0 | 1.34 | 3.59 | 4.35 | 1.47 | 0 | 0 | 0 | 98.73 | 1 | ||
| QUEST562/41/11 | QUEST-30 | QUEST-WDS | 65.39 | 0.87 | 15.54 | 6.35 | 0 | 1.26 | 4.09 | 4.61 | 1.56 | 0 | 0 | 0 | 99.67 | 1 | ||
| QUEST562/41/12 | QUEST-30 | QUEST-WDS | 65.41 | 0.87 | 15.64 | 5.84 | 0 | 1.34 | 3.84 | 4.11 | 1.7 | 0 | 0 | 0 | 98.76 | 1 | ||
| QUEST562/41/13 | QUEST-30 | QUEST-WDS | 65.52 | 0.8 | 15.72 | 5.88 | 0 | 1.3 | 3.6 | 4.32 | 1.46 | 0 | 0 | 0 | 98.59 | 1 | ||
| QUEST562/41/14 | QUEST-30 | QUEST-WDS | 65.68 | 0.89 | 15.27 | 6.11 | 0 | 1.26 | 4.46 | 4 | 1.73 | 0 | 0 | 0 | 99.39 | 1 | ||
| QUEST562/41/15 | QUEST-30 | QUEST-WDS | 65.96 | 0.87 | 15.47 | 6.18 | 0 | 1.29 | 4.21 | 3.78 | 1.72 | 0 | 0 | 0 | 99.48 | 1 | ||
| QUEST562/41/16 | QUEST-30 | QUEST-WDS | 66.53 | 1.04 | 14.23 | 7.06 | 0 | 1.34 | 3.85 | 4.07 | 1.73 | 0 | 0 | 0 | 99.85 | 1 | ||
| QUEST562/41/17 | QUEST-30 | QUEST-WDS | 66.87 | 0.81 | 15.78 | 5.49 | 0 | 1.31 | 3.77 | 4.32 | 1.51 | 0 | 0 | 0 | 98.86 | 1 |
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| QUEST562/47/01 | QUEST-30 | QUEST-WDS | 71.7 | 0.16 | 12.99 | 1.98 | 0 | 0 | 1.56 | 4.44 | 2.95 | 0 | 0 | 0 | 95.78 | 1 | ||
| QUEST562/47/02 | QUEST-30 | QUEST-WDS | 71.86 | 0.17 | 12.92 | 1.84 | 0 | 0 | 1.34 | 4.43 | 2.65 | 0 | 0 | 0 | 95.21 | 1 | ||
| QUEST562/47/03 | QUEST-30 | QUEST-WDS | 72.34 | 0.15 | 13.03 | 1.87 | 0 | 0.04 | 1.42 | 4.52 | 2.62 | 0 | 0 | 0 | 95.99 | 1 | ||
| QUEST562/47/04 | QUEST-30 | QUEST-WDS | 72.68 | 0.13 | 13.15 | 1.87 | 0 | 0.05 | 1.4 | 4.32 | 2.66 | 0 | 0 | 0 | 99.24 | 1 | ||
| QUEST562/47/05 | QUEST-30 | QUEST-WDS | 73.35 | 0.19 | 13.04 | 1.87 | 0 | 0.04 | 1.41 | 4.53 | 2.75 | 0 | 0 | 0 | 97.18 | 1 | ||
| QUEST562/47/06 | QUEST-30 | QUEST-WDS | 73.41 | 0.12 | 12.34 | 1.61 | 0 | 0.04 | 1.2 | 3.95 | 3.46 | 0 | 0 | 0 | 96.14 | 1 |
| labcode | batch | instrument | SiO2 | TiO2 | Al2O3 | FeOt | MnO | MgO | CaO | Na2O | K2O | P2O5 | Cl | F | total | ok | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| QUEST562/78/01 | QUEST-30 | QUEST-WDS | 65.79 | 1.47 | 14.4 | 5.69 | 0 | 1.44 | 3.45 | 4.67 | 2.67 | 0 | 0 | 0 | 99.58 | 1 | ||
| QUEST562/78/02 | QUEST-30 | QUEST-WDS | 65.59 | 1.5 | 14.28 | 5.91 | 0 | 1.45 | 3.67 | 4.57 | 2.55 | 0 | 0 | 0 | 99.52 | 1 |
| z | z_range | sample | t | t_sigma | context | sector | tephra_type | tephra_deposit | material | tephra_shards | tephra_shards_abs | volc_region | volcano | eruption | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 1.095 | 0.01 | QUEST562/78 | -777.5 | 21 | GB4-150 | distal | fall | ash | 9999 | 0 | EVZ | Katla | GB4-150 | QUB493 | |||
| 0.1 | 0.02 | QUEST562/111 | 860.5 | 20 | AD860 Layer part B | distal | fall | ash | 9999 | 0 | Iceland | Iceland_volcanoes | AD860 Layer part B | QUB483; includes 2 outliers | |||
| 0.98 | 0.02 | QUEST562/41 | -643.5 | 60 | BMR-190 | distal | fall | ash | 9999 | 0 | EVZ | Hekla | BMR-190 | QUB447 | |||
| 1.74 | 0.02 | QUEST562/47 | -2309.5 | 20 | H4 Hekla | distal | fall | ash | 9999 | 0 | EVZ | Hekla | H4 Hekla | QUB454; 4 other analyses not entered as they seem to derive from an eruption of Katla | |||
| 1.035 | 0.01 | QUEST562/112 | -716.5 | 38 | OMH-185 (Barnsmore) | distal | fall | ash | 9999 | 0 | Iceland | Iceland_volcanoes | OMH-185 (Barnsmore) | QUB473; 2 populations and 2 outliers |
| z | z_range | t | t_sigma | sample | volc_region | volcano | eruption | ref | ||
|---|---|---|---|---|---|---|---|---|---|---|
| 0.1 | 0.02 | 860.5 | 20 | QUEST562/111 | Iceland | Iceland_volcanoes | AD860 Layer part B | doi:10.1191/0959683604hl757rr | ||
| 1.035 | 0.01 | -716.5 | 38 | QUEST562/112 | Iceland | Iceland_volcanoes | OMH-185 (Barnsmore) | doi:10.1191/0959683604hl757rr | ||
| 0.98 | 0.02 | -643.5 | 60 | QUEST562/41 | EVZ | Hekla | BMR-190 | doi:10.1191/0959683604hl757rr | ||
| 1.74 | 0.02 | -2309.5 | 20 | QUEST562/47 | EVZ | Hekla | H4 Hekla | doi:10.1191/0959683604hl757rr | ||
| 1.095 | 0.01 | -777.5 | 21 | QUEST562/78 | EVZ | Katla | GB4-150 | doi:10.1191/0959683604hl757rr |
| eruption | eruption_type | t | t_sigma | t_source | ref | notes | ||
|---|---|---|---|---|---|---|---|---|
| Hekla AD1947 | Plinian | 1947.5 | 1 | Calendar | doi:10.1191/095968399669624108 | AD 1947 historical | ||
| Hekla AD1845 | Plinian | 1845.5 | 1 | Calendar | doi:10.1191/095968399669624108 | AD 1845 historical | ||
| Hekla AD1510 | Plinian | 1510.5 | 1 | Calendar | doi:10.1191/095968399669624108 | AD 1510 historical | ||
| Hekla AD1300 | Plinian | 1300.5 | 1 | Calendar | doi:10.1191/095968399669624108 | AD 1300 historical | ||
| Hekla AD1158 | Plinian | 1158.5 | 1 | Calendar | doi:10.1191/095968399669624108 | AD 1158 historical | ||
| Hekla AD1104 | Ultra-Plinian | 1104.5 | 1 | Calendar | doi:10.1191/095968399669624108 | AD 1104 historical (see Larsen and Thorarinsson 1977; Larsen et al. 1999) | ||
| MOR-T6 | Plinian | 840.5 | 100 | doi:10.1191/0959683604hl749rp | c. AD 840 interpolated (Chambers et al. 2004) | |||
| Tjornuvik AD800 A | Plinian | 800.5 | 50 | doi:10.1191/095968301668079904 | ninth century AD age suggested by Wastegard et al. (2001). | |||
| BMR-190 | Plinian | -643.5 | 60 | IntCal04 | doi:10.1191/0959683604hl757rr | c. 705-585 cal BC (Plunkett et al. 2004). | ||
| H3 Hekla | Ultra-Plinian | -1054.5 | 157 | IntCal09 | c. 2820 ± 70 14C yr BP, i.e. 3156-2772 yr cal BP (2 sigma; Larsen and Thorarinsson 1977) | |||
| KAL-X | Plinian | -1769.5 | 15 | IntCal04 | doi:10.1177/0959683608089208 | c. 3735-3705 cal BP wiggle-match. Proximal equivalent of Hekla Selsund, Hekla HS and Kebister distal tephras (Wastegard et al. 2008) | ||
| Hekla Selsund | Plinian | -1769.5 | 15 | IntCal04 | doi:10.1177/0959683608089208 | c. 3735-3705 cal BP wiggle-match. Distal equivalent of Hekla KAL-X proximal tephra (Wastegard et al. 2008). | ||
| Kebister | Plinian | -1769.5 | 15 | IntCal04 | doi:10.1177/0959683608089208 | c. 3735-3705 cal BP wiggle-match. Distal equivalent of Hekla KAL-X proximal tephra (Wastegard et al. 2008). | ||
| Hekla HS | Plinian | -1769.5 | 15 | IntCal04 | doi:10.1177/0959683608089208 | c. 3735-3705 cal BP wiggle-match. Distal equivalent of Hekla KAL-X proximal tephra (Wastegard et al. 2008). | ||
| H4 Hekla | Ultra-Plinian | -2309.5 | 20 | doi:10.1177/095968369500500111 | c. 2310 ± 20 calBC wiggle-match at Sluggan | |||
| Lairg A | Plinian | -4952.5 | 47 | doi:10.1191/0959683602hl538rr | c. 4997-4902 cal BC 14C wiggle-match (Pilcher et al. 1996; Hall & Pilcher 2002). | |||
| H5 Hekla | Ultra-Plinian | -5101.5 | 105 | IntCal09 | ref:vilmundardottir1982hss | c. 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). |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ballysculllian East | UK | -6.462999821 | 54.79750061 | 44 | Terrestrial | QUEST621/38 | distal | fall | ash | quest | |||||
| Derrycunihy Wood | Ireland | -9.416669846 | 52.01670074 | Terrestrial | QUEST580/38 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Bødalsvatnett | Norway | 13.56200027 | 68.1969986 | 42 | Terrestrial | QUEST634/47 | distal | fall | ash | quest | |||||
| Corlea Bog west Corlea I | Ireland | -7.866670132 | 53.59999847 | Terrestrial | QUEST578/47 | distal | fall | ash | quest | ||||||
| Croaghaun East | Ireland | -9.455030441 | 54.19200134 | Terrestrial | QUEST581/47 | distal | fall | ash | quest | ||||||
| Red Bog | Ireland | -8.533280373 | 52.51639938 | Terrestrial | QUEST582/47 | distal | fall | ash | quest | ||||||
| Toome | UK | -6.461790085 | 54.75170135 | Terrestrial | QUEST632/47 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Derrycunihy Wood | Ireland | -9.416669846 | 52.01670074 | Terrestrial | QUEST580/35 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Toome | UK | -6.461790085 | 54.75170135 | Terrestrial | QUEST632/48 | distal | fall | ash | quest |
| eruption | eruption_type | t | t_sigma | t_source | ref | notes | ||
|---|---|---|---|---|---|---|---|---|
| PMG-5 | Plinian | 1600.5 | 100 | doi:10.1191/0959683602hl538rr | possibly c. AD 1600 interpolated (Hall & Pilcher 2002). | |||
| BIP-24 | Plinian | 900.5 | 100 | doi:10.1111/j.1502-3885.2005.tb01011.x | c. AD 900 interpolated | |||
| AD860 Layer part B | Plinian | 860.5 | 20 | doi:10.1177/095968369500500111 | c. AD 860 ± 20 radiocarbon wiggle-match at Sluggan (AD lower layer, colourless tephra shards, two populations) | |||
| OMH-185 (Barnsmore) | Plinian | -716.5 | 38 | IntCal04 | doi:10.1191/0959683604hl757rr | c. 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-1 | Plinian | |||||||
| FMAZ II (Fugloyarbanki) | Plinian | -24739.5 | 1 | GICC05 | doi:10.1002/jqs.1182 | 26740 ± 390 yr b2k in NGRIP 1848.05 | ||
| Borrobol | Plinian | -12094.5 | 95 | IntCal09 | doi:10.1002/jqs.1498 | Best 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). | ||
| L3574 | Plinian | No 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 AD700 | Plinian | 700.5 | 100 | doi:10.1191/0959683602hl538rr | c. AD 700 interpolated (Hall & Pilcher 2002). | |||
| Penifiler Tephra | Plinian | -11929.5 | 200 | IntCal09 | doi:10.1002/jqs.1498 | 14.08-13.68 cal ka BP (Bayesian age model) | ||
| Sluggan A | Plinian | -12549.5 | 500 | doi:10.1002/jqs.990 | c. 14500 cal BP suggested by Turney et al. (2006) | |||
| Sluggan B | Plinian | -10849.5 | 500 | doi:10.1002/jqs.990 | c. 12800 cal BP suggested by Turney et al. (2006) | |||
| AD860 Layer part A | Plinian | 860.5 | 20 | doi:10.1177/095968369500500111 | c. AD 860 ± 20 radiocarbon wiggle-match at Sluggan (AD lower layer, colourless tephra shards, two populations) | |||
| BMR-90 AD920 | Plinian | 920.5 | 100 | doi:10.1191/0959683602hl538rr | c. AD 920 interpolated (Hall & Pilcher 2002) | |||
| Breakish Tephra | Plinian | doi:10.1002/jqs.1066 | no date suggested although position above the Ashik tephra and Saksunarvatn indicates an age in the early-mid Holocene. | |||||
| DOM-6 'microlite' tephra | Plinian | -696.5 | 35 | doi:10.1006/qres.2002.2325 | c. 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. | |||
| GB4-182 | Plinian | -1349.5 | 200 | doi:10.1191/0959683602hl538rr | c. 1350 cal BC interpolated (Hall & Pilcher 2002) | |||
| GB4-50 AD1250 | Plinian | 1250.5 | 100 | doi:10.1191/0959683602hl538rr | c. AD 1250 interpolated (Hall & Pilcher 2002) | |||
| Harthorpe Moss tephra | Plinian | doi:10.1177/095968369600600112 | ||||||
| Lough Portain B | Plinian | 0 | doi:10.1177/095968369500500301 | sub-population of Hekla AD 1510 eruption (Lough Portain A). Status is unclear, not a distinct isochrone | ||||
| MOR-T4 | Plinian | 1000.5 | 100 | doi:10.1191/0959683604hl749rp | c. cal AD 1000 interpolated (Chambers et al. 2004) | |||
| Roddans Port A | Plinian | doi:10.1002/jqs.990 | two sub-populations (A & B) at 63-64 cm depth, dating unclear, pre-Vedde Ash. | |||||
| Roddans Port B | Plinian | doi:10.1002/jqs.990 | two sub-populations (A & B) at 63-64 cm depth, dating unclear, pre-Vedde Ash. | |||||
| SLU-5 | Plinian | 1650.5 | 50 | doi:10.1191/0959683602hl538rr | c. AD 1600-1700 interpolated (Hall & Pilcher 2002) | |||
| Stomyren tephra | Plinian | -149.5 | 100 | doi:10.1016/j.quaint.2004.04.030 | c. 2100 cal yr BP interpolated (Wastegard 2005) | |||
| Vallensgard Mose tephra | Plinian | doi:10.1002/jqs.990 | Stratigraphic 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 I | Plinian | -10449.5 | 500 | Marine04 | doi:10.1016/j.quascirev.2006.03.001 | Diffuse 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-274 | Plinian | -8274.5 | 100 | IntCal09 | doi:10.1016/j.quaint.2011.05.014 | 14C modeled age of 10,325-10,125 yr cal BP (Lind & Wastegard 2011). | ||
| 5d-BAS | Plinian | -109549.5 | 5000 | Orbital | doi:10.1016/s0277-3791(98)00038-9 | Probably represents an eruption complex. Several geochemical populations: BAS-I, BAS-II, BAS-III. | ||
| 5e-Midt | Plinian | -123049.5 | 5000 | Orbital | doi:10.1016/s0277-3791(98)00038-9 | Probably 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-Low | Plinian | -127549.5 | 5000 | Orbital | doi:10.1016/s0277-3791(98)00038-9 | Probably represents an eruption complex. Several geochemical populations. Wallrabe-Adams & Lackschewitz (2002) suggest either Vatnafjoll or Vestmannaeyjar may be the source. | ||
| St. 5a-THOL-1 | Plinian | -74549.5 | 5000 | Orbital | doi:10.1016/0012-821x(95)00145-3 | THOL geochemical composition | ||
| St. 7-RHY-I & II | Plinian | -208049.5 | 20000 | Orbital | doi:10.1002/jqs.3390060205 | RHY-I & RHY-II geochemical compositions | ||
| St. 7-BAS/INT-I | Plinian | -208549.5 | 20000 | Orbital | doi:10.1002/jqs.3390060205 | INT-I & INT/BAS-I geochemical compositions | ||
| St. 9-RHY-I | Plinian | -328049.5 | 30000 | Orbital | doi:10.1002/jqs.3390060205 | RHY geochemical composition; possible equivalent to NAAZ III (III-RHY-I, c.320 ka) | ||
| St. 9-BAS-I | Plinian | -328049.5 | 30000 | Orbital | doi:10.1002/jqs.3390060205 | BAS geochemcial composition |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ballysculllian East | UK | -6.462999821 | 54.79750061 | 44 | Terrestrial | QUEST621/111 | distal | fall | ash | quest | |||||
| Borg Indrepollen | Norway | 13.49400043 | 68.14499664 | Terrestrial | QUEST636/111 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Borg Indrepollen | Norway | 13.49400043 | 68.14499664 | Terrestrial | QUEST636/110 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Derrycunihy Wood | Ireland | -9.416669846 | 52.01670074 | Terrestrial | QUEST580/113 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| K708-1 | -23.75 | 50 | -4053 | Marine | QUEST709/3 | distal | fall | ash | quest |
| eruption | eruption_type | t | t_sigma | t_source | ref | notes | ||
|---|---|---|---|---|---|---|---|---|
| Vedde Ash | Ultra-Plinian | -10170.5 | 1 | GICC05 | doi:10.1029/2005jd006079 | Bi-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 AD1625 | Plinian | 1625.5 | 1 | Calendar | AD 1625 historical | |||
| Eldgja tephra | Sub-Plinian | 934.5 | 1 | GICC05 | doi:10.1177/095968369500500201 | 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). | ||
| GA4-85 | Plinian | 750.5 | 50 | doi:10.1191/0959683602hl538rr | c. AD 700-800 interpolated (Hall & Pilcher 2002). | |||
| Tjornuvik AD800 B | Plinian | 800.5 | 50 | doi:10.1191/095968301668079904 | ninth century AD age suggested by Wastegard et al. (2001). | |||
| GB4-150 | Plinian | -777.5 | 21 | IntCal04 | doi:10.1191/0959683604hl757rr | c. 800-758 cal BC (Plunkett et al. 2004). | ||
| Mjauvotn A | Plinian | -4399.5 | 200 | doi:10.1191/095968301668079904 | c. 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 B | Plinian | -4399.5 | 200 | doi:10.1191/095968301668079904 | c. 5300-5700 14C yr BP radiocarbon | |||
| Torfadalsvatn (Tv-5) | Sub-Plinian | -4954.5 | 240 | IntCal09 | doi:10.1111/j.1502-3885.1992.tb00009.x | Transitional 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-A1 | Sub-Plinian | -4009.5 | 207 | IntCal09 | doi:10.1002/jqs.724 | c. 5170 ± 85 14C yr BP (Wastegard 2002, JQS 17(8), 723-730). Calibrates to 6182-5730 yr cal BP (2 sigma). | ||
| SILK-A7 | Sub-Plinian | -5189.5 | 123 | IntCal09 | doi:10.1002/jqs.724 | c. 6245 ± 90 14C yr BP calibrates to 7415-6932 yr cal BP (2 sigma; Wastegard 2002) | ||
| SILK-YN | Sub-Plinian | 310.5 | 70 | IntCal09 | doi:10.1179/env.2000.5.1.21 | There 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 tephra | Plinian | -6119.5 | 90 | IntCal09 | doi:10.1002/jqs.724 | Rhyolitic ash layer, c. 7240 ± 95 14C yr BP calibrates to 8310-7868 cal BP (2 sigma; Wastegard 2002, JQS 17(8), 723-730). | ||
| NGRIP 1508.26m | Sub-Plinian | -10249.5 | 1 | GICC05 | doi:10.1029/2005jd006079 | Rhyolitic ash layer. NGRIP GICC05 age of 12250 ± 117 b2k years | ||
| NGRIP 1573.00m | Sub-Plinian | -12019.5 | 1 | GICC05 | doi:10.1029/2005jd006079 | Basalt layer. NGRIP GICC05 14020 ± 167 b2k. | ||
| Dimna Ash | Plinian | -13149.5 | 300 | IntCal04 | doi:10.1016/j.quascirev.2007.04.021 | Rhyolitic ash that is below radiocarbon age of 12780 ± 60 14C yr BP (15400-14850 cal BP) on terrestrial plant macrofossils (Koren et al. 2008) | ||
| AF555 | Plinian | -9544.5 | 295 | IntCal09 | doi:10.1002/jqs.1498 | Rhyolitic ash layer. Bayesian age model 11.79-11.20 cal ka BP | ||
| Solheimar Ignimbrite | Phreato-Plinian | -10149.5 | 700 | doi:10.1007/bf00298704 | correlated with Vedde Ash and dated to Younger Dryas Stadial. | |||
| NGRIP 1861.55m | Sub-Plinian | -25526.5 | 1 | GICC05 | doi:10.1016/j.epsl.2010.03.004 | Transitional alkali basalt; GICC05 age of 27527 ± 410 b2k | ||
| NGRIP 1895.24m | Sub-Plinian | -27129.5 | 1 | GICC05 | doi:10.1016/j.epsl.2010.03.004 | Transitional alkali basalt; GICC05 age of 29130 ± 456 b2k | ||
| IA2 | Sub-Plinian | -11199.5 | 146 | Orbital | doi:10.1016/s0277-3791(00)00146-3 | Ice 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 tephra | Plinian | -7799.5 | 100 | IntCal09 | doi:10.1016/j.quaint.2011.05.014 | 14C modeled age of 9850-9650 yr cal BP (Lind & Wastegard 2011). | ||
| St. 5a-TAB-1 | Plinian | -73449.5 | 5000 | Orbital | doi:10.1016/0012-821x(95)00145-3 | TAB geochemical composition | ||
| St. 5a-TAB-2 | Plinian | -75549.5 | 5000 | Orbital | doi:10.1016/0012-821x(95)00145-3 | TAB geochemical composition |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Borg Indrepollen | Norway | 13.49400043 | 68.14499664 | Terrestrial | QUEST636/54 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Gurskøy | Norway | 5.557889938 | 62.3708992 | Terrestrial | QUEST637/3 | distal | fall | ash | quest | ||||||
| Kvaltjern | Norway | 4.981400013 | 60.42309952 | Terrestrial | QUEST639/3 | distal | fall | ash | quest | ||||||
| Lake Kullatorpssjön | Sweden | 12.48770046 | 56.29410172 | 89 | Terrestrial | QUEST692/3 | distal | fall | ash | quest | |||||
| Lake Mullsjön | Sweden | 14.36079979 | 58.36930084 | 133 | Terrestrial | QUEST695/3 | distal | fall | ash | quest | |||||
| Lerstadvatn, Ålesond | Norway | 6.260990143 | 62.36729813 | Terrestrial | QUEST641/3 | distal | fall | ash | quest | ||||||
| Lake Gjølvatn | Norway | 6.252160072 | 62.43230057 | Terrestrial | QUEST640/3 | distal | fall | ash | quest | ||||||
| Lillerestjønn | Norway | 6.31704998 | 62.46889877 | Terrestrial | QUEST642/3 | distal | fall | ash | quest | ||||||
| Saudedalsmyra | Norway | 6.236690044 | 62.43389893 | Terrestrial | QUEST643/3 | distal | fall | ash | quest | ||||||
| Lac de Sewen | France | 6.897220135 | 47.81169891 | 500 | Terrestrial | QUEST823/3 | distal | fall | ash | quest |