IntChron > doi > 10.1016 > j.jvolgeores.2007.08.017
| eruption | eruption_type | t | t_sigma | t_source | ref | notes | ||
|---|---|---|---|---|---|---|---|---|
| Pomici Principali | Plinian | -10086.5 | 122 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | A revised age for the large PP eruption of 11,915-12,158 cal. yrs BP was obtained using the single published radiocarbon measurement (11,978-12,930 cal. yrs BP; uncalibrated date from Di Vito et al., 1999) and data of Lane et al. (2011) which was imported as a prior into an OxCal model. | ||
| TLm | Sub-Plinian | -43649.5 | 350 | ArAr | doi:10.1016/s0377-0273(99)00033-5 | One of more than 12 separate eruptions; TLm has Ar-Ar age of 45.6 ± 0.7 ka BP | ||
| Campanian Ignimbrite (Y5) | Ultra-Plinian | -37349.5 | 55 | ArAr | doi:10.1007/s007100170010 | Single crystal 40Ar/39Ar dating of insitu proximal deposits of 39,300 ± 110 yr BP. The CI is subdivided into fall, main flow and upper flow (see context field). The upper flow is unlikely to be significant at distal localities. The fall and main flow components are both represented at Monticchio. Y5 is the marine equivalent. | ||
| Neapolitan Yellow Tuff | Ultra-Plinian | -12239.5 | 680 | IntCal04 | doi:10.1016/j.quascirev.2004.06.004 | c. 12100 ± 170 14C yr BP (14,870-13,510 cal BP) (Siani et al. 2004, Quaternary Science Reviews 23, 2485-2500). Varve age for TM-8 at LGM of 14,120 ± 710 yr BP (Wulf et al. 2004, 2008). The NYT is subdivided into upper and lower members (see context field). The lower member is more likely to be significant distally and is recorded at Monticchio, however the upper member may also be represented at some localities. | ||
| Y3 | Plinian | -28579.5 | 160 | Marine09 | doi:10.1016/s0025-3227(02)00270-0 | c. 25,570 ± 110 14C yr BP in marine core C45 [30,530 ± 160 yr cal BP] and c. 26,030 ± 150 14C yr BP [30,820 ± 170 yr cal BP] in core C106 (Buccheri et al. 2002a & b), on foraminifera 3 & 4 cm below layer. Di Vito et al. (2008) argues this is the distal correlate of the VRa products in the Campi Flegrei. | ||
| UPA | Sub-Plinian | |||||||
| Tufi Biancastri (GM1) | Sub-Plinian | -12649.5 | 300 | ArAr | doi:10.1016/s0377-0273(99)00033-5 | From 17.9 ± 500 to 14.6 ± 600 ka BP, 39Ar/40Ar ages for a complex of more than 5 pre-NYT eruptions (Pappalardo et al. 1999). Varve age for TM-9 at Lago Grande di Moncchio of 14560 ± 730 yr BP (Wulf et al. 2004, 2008). | ||
| Astroni 1-6 | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00037-2 | ~3.5-4.4 ka cal BP; indicative age only, based on stratigraphic position in a Bayesian sequence (see Smith et al., 2011) | ||||
| Agnano Monte Spina | Plinian | -2603.5 | 72 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Published radiocarbon dates for AMS (4421-5299 cal. yrs BP; Rosi and Sbrana, 1987 and Di Vito et al., 1999; Passariello et al., 2010) were integrated with the SCTF 39Ar/40Ar age (5200 ± 900 yrs BP; de Vita et al., 1999) and modelled along with the ages of other eruption units to constrain the date of the AMS eruption to 4482-4625 cal. yrs BP (95% confidence level). | ||
| Lagno Amendolare | Plinian | -12513.5 | 189 | IntCal04 | doi:10.1016/j.quascirev.2004.06.004 | c. 13,070 ± 90 14C yr BP on terrestrial material (Siani et al. 2004; Andronico 1997) and 13,480 ± 90 14C yr BP on marine. Varve ages for TM-10a, TM-10b, TM-10c & TM-10d range from 15,030 ± 750 to 15,550 ± 780 yr BP at Lago Grande di Monticchio (Wulf et al. 2004; 2008). | ||
| Averno 1 | Sub-Plinian | -3297.5 | 184 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 5064-5431 cal. yr BP (Smith et al. 2011). | ||
| Fondi di Baia | Sub-Plinian | -7659.5 | 85 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 9525-9695 cal. yr BP (Smith et al. 2011) | ||
| Casale | Sub-Plinian | -8979.5 | 165 | IntCal09 | 9580 ± 100 14C yr BP on terrestrial material, calibrates to 11,200-10,606 yr cal BP (2 sigma; Di Vito et al. 1999). | |||
| Pre-Tufi Biancastri | Sub-Plinian | |||||||
| Santa Lucia (C15) | Plinian | -48999.5 | 1500 | IntCal09 | ref:vito2008ppd | c. 47,500 ± 2600 14C yrs BP; 50,950 ± 2980 cal BP (Di Vito et al. 2008). Alternatively, varve age for TM-18-12b of 49,410 ± 2470 yr BP at Lago Grande di Monticchio (Wulf et al. 2006). | ||
| TLa | Sub-Plinian | -56049.5 | 1500 | ArAr | doi:10.1016/s0377-0273(99)00033-5 | Pre-Campanian, one of more than 12 separate eruptions; TLa is 58 ± 3 ka on bulk crystal 40Ar/39Ar dating of insitu proximal deposits | ||
| TLc | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00033-5 | Pre-Campanian, one of more than 12 separate eruptions; >45.6±0.7 & <58±3 ka | ||||
| TLf | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00033-5 | Pre-Campanian, one of more than 12 separate eruptions; >45.6±0.7 & <58±3 ka | ||||
| TLo | Sub-Plinian | -15949.5 | 250 | ArAr | doi:10.1016/s0377-0273(99)00033-5 | Ar-Ar age on feldspars of 17.9 ± 0.5 ka; Pre-NYT, Biancastre | ||
| VRa | Sub-Plinian | -28299.5 | 100 | ArAr | doi:10.1016/s0377-0273(99)00033-5 | Pre-NYT, Biancastre. Di Vito et al (2008) argues that VRa is proximal equivalent of Y3/SMP1-e but this is unproven. 30.3 ± 0.2 ka (bulk crystal 40Ar/39Ar dating of insitu proximal deposits) | ||
| VRb | Sub-Plinian | Pre-NYT, Biancastre | ||||||
| PRa | Sub-Plinian | -14149.5 | 100 | ArAr | doi:10.1016/s0377-0273(99)00033-5 | Pre-NYT, Biancastre 16.1 ± 0.2 ka (or 15.5 ± 1.7 ka based on single-crystal total fusion) bulk crystal 40Ar/39Ar dating of insitu proximal deposits | ||
| X-5 Tephra | Plinian | -103049.5 | 1000 | ArAr | doi:10.1038/23432 | Ar-Ar date on sanidine of 105 ± 2 ka BP | ||
| Soccavo 5 | Sub-Plinian | -9719.5 | 290 | Varve | ref:wulf2007dts | ash fall; c. 11.67 ± 0.58 ka BP (varve yrs), Wulf et al. (2007) | ||
| Soccavo 4 | Sub-Plinian | -9939.5 | 295 | Varve | ref:wulf2007dts | basal seq. pumice fall; upper seq. mainly pdc; c. 11.89 ± 0.59 ka BP (varve yrs), Wulf et al. (2007) | ||
| Monte Nuovo | Sub-Plinian | 1538.5 | 1 | Calendar | doi:10.1016/s0377-0273(99)00037-2 | pdc & scoria fall in upper seq; AD 1538 historical | ||
| Astroni 7 | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00037-2 | ~3.5-4.4 ka cal BP; indicative age only, based on stratigraphic position in a Bayesian sequence (see Smith et al., 2011); pdc & ash fall | ||||
| Astroni 6 | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00037-2 | ~3.5-4.4 ka cal BP; indicative age only, based on stratigraphic position in a Bayesian sequence (see Smith et al., 2011); mainly pdc; basal subplinian pumice fall; upper scoria fall | ||||
| Astroni 5 | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00037-2 | ~3.5-4.4 ka cal BP; indicative age only, based on stratigraphic position in a Bayesian sequence (see Smith et al., 2011); mainly pdc & minor pumice fall in basal seq. | ||||
| Astroni 4 | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00037-2 | ~3.5-4.4 ka cal BP; indicative age only, based on stratigraphic position in a Bayesian sequence (see Smith et al., 2011); mainly pdc interbedded with pumice fall | ||||
| Astroni 3 | Sub-Plinian | -2271.5 | 123 | IntCal09 | doi:10.1016/s0377-0273(99)00037-2 | Charcoal in thin humified layer underlying Astroni 3 tephra gives 14C age of 3820 ± 50 yr BP (CAMS-38439) which calibrates to 4409-4089 cal BP (2 sigma). Mainly pdc interbedded with pumice fallout | ||
| Astroni 2 | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~3.5-4.4 ka cal BP; pdc & minor ash fall | |||||
| Astroni 1 | Sub-Plinian | -2298.5 | 96 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 4153-4345 cal. yr BP (Smith et al. 2011); pdc & ash fall | ||
| Averno 2 | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~3.5-4.4 ka cal BP | |||||
| Solfatara | Sub-Plinian | -2333 | 103 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 4181-4386 cal. yr BP (Smith et al. 2011); pdc; upper seq. mainly coarse fall & breccia | ||
| Paleoastroni 3 | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~3.5-4.4 ka cal BP; ash & pumice fall; minor pdc | |||||
| Paleoastroni 2 | Sub-Plinian | -2784 | 23 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 4712-4757 cal. yr BP (Smith et al. 2011); sub-plinian fall & minor pdc | ||
| Paleoastroni 1 | Sub-Plinian | -2839 | 45 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 4745-4834 cal. yr BP (Smith et al. 2011); alt. ash & pumice fall | ||
| Monte Sant’Angelo 5-ka | Sub-Plinian | -2970.5 | 89 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 4832-5010 cal. yr BP (Smith et al. 2011); alt. pumice fall & pdc; upper seq. mostly pdc | ||
| Pignatiello 2 | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~4.5-5.5 ka cal BP; mainly pdc | |||||
| Agnano 3 | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~4.5-5.5 ka cal BP; mainly pdc; some pumice fall at base | |||||
| Cigliano | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~4.5-5.5 ka cal BP; mainly pdc; some pumice fall at base | |||||
| Agnano 2 | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~4.5-5.5 ka cal BP; ash fall & minor pdc | |||||
| Agnano 1 | Sub-Plinian | -3496.5 | 181 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 5266-5628 cal. yr BP (Smith et al. 2011); alt. ash & pumice fall | ||
| St Martino | Sub-Plinian | -7247.5 | 172 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 9026-9370 cal. yr BP (Smith et al. 2011); basal seq. pumice fall; upper seq. mainly pdc | ||
| Sartania 2 | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~9.1-9.6 ka cal BP; mainly pumice fall interbedded with pdc | |||||
| Pigna San Nicola | Sub-Plinian | -7416.5 | 166 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 9201-9533 cal. yr BP (Smith et al. 2011); mainly pumice fall interbedded with pdc | ||
| Sartania 1 | Sub-Plinian | -7626.5 | 77 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 9500-9654 cal. yr BP (Smith et al. 2011); mainly pdc | ||
| Pisani 3 | Sub-Plinian | -8946.5 | 200 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 10,697-11,098 cal. yr BP (Smith et al. 2011); ash fall | ||
| Montagna Spaccata | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; scoria & minor ash fall | |||||
| Pisani 2 | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; scoria & minor ash fall | |||||
| Pisani 1 | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; coarse scoria & minor ash fall | |||||
| Minopoli 2 | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; coarse scoria & minor ash fall | |||||
| Paleo San Martino | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; coarse scoria & minor ash fall | |||||
| Soccavo 3 | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; indicative age only, based on stratigraphic position in a Bayesian sequence (see Smith et al., 2011); mainly pdc | ||||
| Soccavo 2 | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; indicative age only, based on stratigraphic position in a Bayesian sequence (see Smith et al., 2011); mainly pdc | ||||
| Paleopisani 2 | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; indicative age only, based on stratigraphic position in a Bayesian sequence (see Smith et al., 2011); alt. pumice & ash fall | ||||
| Paleopisani 1 | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; indicative age only, based on stratigraphic position in a Bayesian sequence (see Smith et al., 2011); basal seq. pdc; upper seq. scoria fall | ||||
| Gaiola | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; pumice and minor ash fall layers | |||||
| Soccavo 1 | Sub-Plinian | -10261.5 | 164 | IntCal09 | doi:10.1016/s0377-0273(99)00037-2 | Charcoal in palaeosol underlying Soccavo 1 tephra gives 14C age of 10,330 ± 50 yr BP (CAMS-38438) which calibrates to 12,390-11,990 cal BP (2 sigma). Pyroclastic density currents interbedded with pumice lenses; upper massive ash | ||
| Paradiso | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; minor pdc interbedded with pumice fall | |||||
| Minopoli 1 | Sub-Plinian | doi:10.1016/s0377-0273(99)00037-2 | ~10.6-15.0 ka cal BP; coarse scoria fall | |||||
| La Pigna 1 | Sub-Plinian | -11029.5 | 109 | IntCal09 | doi:10.1016/s0377-0273(99)00037-2 | Charcoal in palaeosol underlying La Pigna 1 tephra gives 14C age of 11,060 ± 60 yr BP (CAMS-38437) which calibrates to 13,113-12,727 cal BP (2 sigma). Mainly pdc interbedded with pumice fall | ||
| Gauro | Sub-Plinian | 0 | doi:10.1016/s0377-0273(99)00037-2 | epoch 1 eruption; mainly pdc | ||||
| Bacoli | Sub-Plinian | -10882 | 1322 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 11,511-14,154 cal. yr BP (Smith et al. 2011); mainly pdc | ||
| Capo Miseno | Sub-Plinian | -2122.5 | 813 | IntCal09 | doi:10.1016/j.quascirev.2011.07.012 | Bayesian (95% confidence) modelled age range of 3259-4886 cal. yr BP (Smith et al. 2011). Stratigraphic position is controversial - the tephra is very poorly dated. | ||
| X-6 Tephra | Plinian | -106449.5 | 2700 | Varve | ref:wulf2007dts | c. 108.40 ± 5.4 ka BP (varve yr with 5% error) in Lago Grande di Monticchio (Wulf et al. 2007) |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Masseria Montemaoro quarry | Italy | 14.42599964 | 40.82099915 | Terrestrial | WP4_ITA_ZS98274 | proximal | fall | pumice | rcioni | distal fall |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| CM92-43 | 14.73239994 | 42.88679886 | -252 | Marine | QUEST588/86 | distal | fall | ash | quest | ||||||
| CM92-41 | 15.09659958 | 42.56790161 | -173 | Marine | QUEST589/86 | distal | fall | ash | quest | ||||||
| IN68-21 | 14.92500019 | 42.18500137 | -252 | Marine | QUEST591/86 | distal | fall | ash | quest | ||||||
| IN88-22 | 15 | 42.38330078 | -129 | Marine | QUEST592/86 | distal | fall | ash | quest | ||||||
| PAL94-66 | 14.93929958 | 42.87390137 | -214 | Marine | QUEST604/86 | distal | fall | ash | quest | ||||||
| PAL94-08 | 14.61830044 | 42.61640167 | -150 | Marine | QUEST603/86 | distal | fall | ash | quest | ||||||
| RF93-77 | 15.11660004 | 42.44350052 | -152 | Marine | QUEST608/86 | distal | fall | ash | quest |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| CM92-43 | 14.73239994 | 42.88679886 | -252 | Marine | QUEST588/23 | distal | fall | ash | quest | ||||||
| CM92-41 | 15.09659958 | 42.56790161 | -173 | Marine | QUEST589/23 | distal | fall | ash | quest | ||||||
| IN68-21 | 14.92500019 | 42.18500137 | -252 | Marine | QUEST591/23 | distal | fall | ash | quest | ||||||
| Langsee LG99 | Austria | 14.41940022 | 46.76250076 | 548 | Terrestrial | QUEST481/23 | distal | fall | ash | quest | |||||
| PAL94-66 | 14.93929958 | 42.87390137 | -214 | Marine | QUEST604/23 | distal | fall | ash | quest | ||||||
| PAL94-08 | 14.61830044 | 42.61640167 | -150 | Marine | QUEST603/23 | distal | fall | ash | quest | ||||||
| Prato Spilla C | Italy | 10.1079998 | 44.36130142 | Terrestrial | QUEST607/23 | distal | fall | ash | quest | ||||||
| RF93-77 | 15.11660004 | 42.44350052 | -152 | Marine | QUEST608/23 | distal | fall | ash | quest | ||||||
| KET 82-18 | 17.61669922 | 41.75 | -1077 | Marine | QUEST597/23 | distal | fall | ash | quest | Layer C-2 | |||||
| KET 80-22 | 13.56669998 | 40.58330154 | -2430 | Marine | QUEST593/23 | distal | fall | ash | quest | Layer C-2 |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| RF93-75 | 14.75 | 42.70000076 | -119 | Marine | QUEST615/21 | distal | fall | ash | quest | ||||||
| KET 80-03 | 14.48330021 | 38.81669998 | -1900 | Marine | QUEST596/21 | distal | fall | ash | quest | Layer C-13 (note: Paterne et al. 1988 correlates layer C-10, 3 m depth, with the Y5) | |||||
| KET 80-11 | 15.06669998 | 39.15000153 | -2111 | Marine | QUEST595/21 | distal | fall | ash | quest | Layer C-13 (note: Paterne et al. 1988 correlates layer C-10, 2.58 m depth, with the Y5) | |||||
| Rostov on Don | Russia | 39.5 | 47.09999847 | Terrestrial | QUEST648/21 | distal | fall | ash | quest | ||||||
| Tambov | Russia | 41.5 | 52.5 | Terrestrial | QUEST649/21 | distal | fall | ash | quest | ||||||
| KET 82-18 | 17.61669922 | 41.75 | -1077 | Marine | QUEST597/21 | distal | fall | ash | quest | Layer C-13 (note: Paterne et al. 1988 correlates layer C-10, 3.6 m depth, with the Y5) | |||||
| MAR03-2 | 26.37170029 | 38.06620026 | -398 | Marine | N1: 391/428 cm | distal | fall | ash | aeasku | visible tephra | |||||
| MAR03-28 | 25.02470016 | 39.01699829 | -453 | Marine | A2: 230/330 cm | distal | fall | ash | aeasku | visible tephra | |||||
| MAR03-3 | 25.81949997 | 37.86199951 | -720 | Marine | G5: 120/144 cm | distal | fall | ash | aeasku | visible tephra | |||||
| M72/5-24-GC3 | 37.19469833 | 41.47769928 | -208 | Marine | 24-GC3, 882 cm | distal | fall | ash | 2007-06-01 | quest | averaged EPMA data only presented | ||||
| M72/5-25-GC1 | 36.62379837 | 42.10350037 | -418 | Marine | 25-GC1, 721 cm | distal | fall | ash | 2007-06-01 | quest | averaged EPMA data only presented |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| KET 80-11 | 15.06669998 | 39.15000153 | -2111 | Marine | QUEST595/24 | distal | fall | ash | quest | Layer C-7 (?). See discussion in Zanchetta et al. (2008). |
| site | country | longitude | latitude | elevation | site_type | sample | tephra_type | tephra_deposit | material | z_range | collected | collected_by | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| PAL94-66 | 14.93929958 | 42.87390137 | -214 | Marine | QUEST604/18 | distal | fall | ash | quest |
| z | z_range | sample | t | t_sigma | context | sector | tephra_type | tephra_deposit | material | tephra_shards | tephra_shards_abs | volc_region | volcano | eruption | notes | ||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 3.075 | 0.05 | QUEST602/18 | -10086.5 | 122 | Pomici Principali | distal | fall | ash | 9999 | 0 | Campania | Campania_volcanic_field | Pomici Principali |
| z | z_range | t | t_sigma | sample | volc_region | volcano | eruption | ref | ||
|---|---|---|---|---|---|---|---|---|---|---|
| -6629.5 | 173 | QUEST602/114 | Aeolian Is | Aeolian_volcanoes | Gabellotto-Fiumebianco | |||||
| -19864.5 | 405 | QUEST602/13 | Campania | Somma-Vesuvius | Pomici di Base | |||||
| -17194.5 | 260 | QUEST602/14 | Campania | Somma-Vesuvius | Verdoline | |||||
| 3.075 | 0.05 | -10086.5 | 122 | QUEST602/18 | Campania | Campania_volcanic_field | Pomici Principali | |||
| -12239.5 | 680 | QUEST602/23 | Campania | Campania_volcanic_field | Neapolitan Yellow Tuff | |||||
| -12649.5 | 300 | QUEST602/84 | Campania | Campania_volcanic_field | Tufi Biancastri (GM1) | |||||
| -2603.5 | 72 | QUEST602/86 | Campania | Campania_volcanic_field | Agnano Monte Spina | |||||
| -12513.5 | 189 | QUEST602/87 | Campania | Campania_volcanic_field | Lagno Amendolare | |||||
| -14489.5 | 410 | QUEST602/89 | Sicily | Etna | Biancavilla-Montalto Ign. (Y1) | |||||
| -9639.5 | 362 | QUEST602/94 | Tyrrhensian Sea | Palinuro_Seamount | Capo Palinuro |