Skip to main content
Log in

Estimation of tephra volumes from sparse and incompletely observed deposit thicknesses

  • Research Article
  • Published:
Bulletin of Volcanology Aims and scope Submit manuscript

Abstract

We present a Bayesian statistical approach to estimate volumes for a series of eruptions from an assemblage of sparse proximal and distal tephra (volcanic ash) deposits. Most volume estimates are of widespread tephra deposits from large events using isopach maps constructed from observations at exposed locations. Instead, we incorporate raw thickness measurements, focussing on tephra thickness data from cores extracted from lake sediments and through swamp deposits. This facilitates investigation into the dispersal pattern and volume of tephra from much smaller eruption events. Given the general scarcity of data and the physical phenomena governing tephra thickness attenuation, a hybrid Bayesian-empirical tephra attenuation model is required. Point thickness observations are modeled as a function of the distance and angular direction of each location. The dispersal of tephra from larger well-estimated eruptions are used as leverage for understanding the smaller unknown events, and uncertainty in thickness measurements can be properly accounted for. The model estimates the wind and site-specific effects on the tephra deposits in addition to volumes. Our technique is exemplified on a series of tephra deposits from Mt Taranaki (New Zealand). The resulting estimates provide a comprehensive record suitable for supporting hazard models. Posterior mean volume estimates range from 0.02 to 0.26 km 3. Preliminary examination of the results suggests a size-predictable relationship.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12

Similar content being viewed by others

References

  • Akaike H (1977) On entropy maximization principle. In: Krishnaiah P R (ed) Applications of statistics. North-Holland, pp 27–41

  • Alfano F, Bonadonna C, Volentik ACM, Connor CB, Watt SFL, Pyle DM, Connor LJ (2010) Tephra stratigraphy and eruption volume of the May, 2008, Chaitén eruption, Chile. Bull Volcanol 73:613–630

    Article  Google Scholar 

  • Alloway BV (1989) The late quaternary cover bed stratigraphy and tephrochronology of north-eastern and central Taranaki. PhD thesis, Massey University, New Zealand

    Google Scholar 

  • Alloway BV, Neall VE, Vucetich CG (1995) Late Quaternary (post 28,000 year B.P.) tephrostratigraphy of northeast and central Taranaki, New Zealand. J R Soc NZ 25:385–458

    Article  Google Scholar 

  • Alloway BV, Lowe DJ, Barrell DJA, Newnham RM, Almond PC, Bertler NAN, Litchfield NJ, McGlone MS, Shulmeister J, Vandergoes MJ, Williams PW, members NZ-INTIMATE (2007) Towards a climate event stratigraphy for New Zealand over the past 30 000 years (NZ-INTIMATE project). J Quat Sci 22:9–35

    Article  Google Scholar 

  • Bebbington MS (2014) Long-term forecasting of volcanic explosivity. Geophys J Int 197:1500–1515

    Article  Google Scholar 

  • Bebbington MS, Cronin SJ (2011) Spatio-temporal hazard estimation in the Auckland Volcanic Field, New Zealand, with a new event-order model. Bull Volcanol 73:55–72

    Article  Google Scholar 

  • Bebbington MS, Cronin SJ, Chapman I, Turner MB (2008) Quantifying volcanic ash fall hazard to electricity infrastructure. J Volcanol Geotherm Res 177:1055–1062

    Article  Google Scholar 

  • Bertrand S, Daga R, Bedert R, Fontijn (2014) Deposition of the 2011-2012 Cordón Caulle tephra (Chile, 40 S) in lake sediments: implications for tephrochronology and volcanology. J Geophys Res: Earth Surf 119:2555–2573

    Article  Google Scholar 

  • Biass S, Bonadonna C (2011) A quantitative uncertainty assessment of eruptive parameters derived from tephra deposits: the example of two large eruptions of Cotopaxi volcano, Ecuador. Bull Volcanol 73:73–90

    Article  Google Scholar 

  • Biass S, Bagheri G, Aeberhard WH, Bonadonna C (2014) TError: towards a better quantification of the uncertainty propagated during the characterization of tephra deposits. Stat Volcanol 1.2:1–27

    Google Scholar 

  • Bonadonna C, Costa A (2012) Estimating the volume of tephra deposits: a new simple strategy. Geology 48:415–418

    Article  Google Scholar 

  • Bonadonna C, Houghton BF (2005) Total grain-size distribution and volume of tephra-fall deposits. Bull Volcanol 67:441–456

    Article  Google Scholar 

  • Burden RE, Chen L, Phillips JC (2013) A statistical method for determining the volume of volcanic fall deposits. Bull Volcanol 75(6):1–10

    Google Scholar 

  • Carey S, Sparks RSJ (1986) Quantitative models of the fallout and dispersal of tephra from volcanic eruption columns. Bull Volcanol 48:109–125

    Article  Google Scholar 

  • Christensen R, Johnson W, Branscum A, Hanson TE (2011) Bayesian ideas and data analysis. CRC Press

  • Daggitt ML, Mather TA, Pyle DM, Page SP (2014) AshCalc—a new tool for the comparison of the exponential, power-law and Weibull models of tephra deposition. J Appl Volcan 3(7):1–8

  • Engwell SL, Sparks RSJ, Aspinall WP (2013) Quantifying uncertainties in the measurement of tephra fall thicknesses. J Appl Volcan 2:1–12

    Article  Google Scholar 

  • Engwell SL, Aspinall WP, Sparks RSJ (2015) An objective method for the production of isopach maps and implications for the estimation of tephra deposit volumes and their uncertainties. Bull Volcanol 77(7):1–18

    Google Scholar 

  • Fierstein J, Nathenson M (1992) Another look at the calculation of fallout tephra volumes. Bull Volcanol 54:156–167

    Article  Google Scholar 

  • Fontijn K, Costa F, Sutawidjaja I, Newhall CG, Herrin JS (2015) A 5000-year record of multiple highly explosive mafic eruptions from Gunung Agung (Bali, Indonesia): implications for eruption frequency and volcanic hazards. Bull Volcanol 77:59–74

    Article  Google Scholar 

  • Franks AM (1984) Soils of Eltham County and the tephrochronology of Central Taranaki. PhD thesis, Massey University

  • Gelman A, Carlin JB, Stern HS, Rubin DB (2000) Bayesian data analysis, 1st edn. Chapman & Hall/CRC, Boca Raton-Florida

    Google Scholar 

  • Gonzalez-Mellado AO, De la Cruz-Reyna S (2010) A simple semi-empirical approach to model thickness of ash-deposits for different eruption scenarios. Nat Haz Earth Syst Sci 10:2241– 2257

    Article  Google Scholar 

  • Good IJ, Gaskins RA (1971) Nonparametric roughness penalties for probability densities. Biometrika 58:255–277

    Article  Google Scholar 

  • Green RM, Bebbington MS, Cronin SJ, Jones G (2013) Geochemical precursors for eruption repose length. Geophys J Int 193:855– 873

    Article  Google Scholar 

  • Green RM, Bebbington MS, Cronin SJ, Jones G (2014) Automated statistical matching of multiple tephra records exemplified using five long maar sequences younger than 75 ka, Auckland, New Zealand. Quat Res 82:405–419

    Article  Google Scholar 

  • Johnston EN, Phillips JC, Bonadonna C, Watson IM (2012) Reconstructing the tephra dispersal pattern from the Bronze Age eruption of Santorini using an advection-diffusion model. Bull Volcanol 74:1485–1507

    Article  Google Scholar 

  • Kawabata E, Bebbington MS, Cronin SJ, Wang T (2013) Modeling thickness variability in tephra deposition. Bull Volcanol 75:738–751

    Article  Google Scholar 

  • Kawabata E, Cronin SJ, Bebbington MS, Moufti MR, El-Masry N, Wang T (2015) The AD1256 Al-Madinah eruption, Saudi Arabia: identifying multiple eruption phases from a compound tephra blanket. Bull Volcanol 77:6

    Article  Google Scholar 

  • Klawonn M, Houghton BF, Swanson DA, Fagents SA, Wessel P, Wolfe CJ (2014a) Constraining explosive volcanism: subjective choices during estimates of eruption magnitude. Bull Volcanol 76:793–798

  • Klawonn M, Houghton BF, Swanson DA, Fagents SA, Wessel P, Wolfe CJ (2014b) From field data to volumes: constraining uncertainties in pyroclastic eruption parameters 76:839–854

  • Latter JH (1990) Some real and imaginary examples of volcanic hazard and risk assessment. Proceedings of Pacific Rim Congress 90, Gold Coast, Australia 3:699–711

    Google Scholar 

  • Legros F (2000) Minimum volume of a tephra fallout deposit estimated from a single isopach. J Volcanol Geotherm Res 96:25–32

    Article  Google Scholar 

  • Lunn DJ, Thomas A, Best NG, Spiegelhalter DJ (2000) WinBUGS – a Bayesian modelling framework: concepts, structure, and extensibility. Stat Comput 10:325–337

    Article  Google Scholar 

  • Maeno FD, Nagai M, Nakada S, Burden RE, Engwell S, Suzuki Y, Kaneko T (2014) Constrainting tephra dispersion and deposition from three subplinian explosions in 2011 at Shinmoedake volcano, Kyushu, Japan. Bull Volcanol 76:1–16

    Google Scholar 

  • Marzocchi W, Bebbington MS (2012) Probabilistic eruption forecasting at short and long time scales. Bull Volcanol 74:1777–1805

    Article  Google Scholar 

  • Marzocchi W, Zaccarelli L (2006) A quantitative model for the time-size distribution of eruptions. J Geophys Res 111:B04204

    Google Scholar 

  • Mendoza-Rosas AT, De la Cruz-Reyna S (2008) A statistical method linking geological and historical eruption time series for volcanic hazard estimations: applications to active polygenetic volcanoes. J Volcanol Geotherm Res 176:277–290

    Article  Google Scholar 

  • Moebis A (2010) Understanding the Holocene explosive eruption record of the Tongariro Volcanic Centre. PhD thesis, Massey University, New Zealand

    Google Scholar 

  • Molloy C, Shane P, Augustinus P (2009) Eruption recurrence rates in a basaltic volcanic field based on tephra layers in maar sediments: implications for hazards in the Auckland Volcanic Field. Geol Soc Am Bull 121:1666–1677

    Article  Google Scholar 

  • Neall VE (1972) Tephrochronology and tephrostratigraphy of western Taranaki (N108-109), New Zealand. NZ J Geol Geophys 15:507–557

    Article  Google Scholar 

  • Pollard AM, Blockley SPE, Ward KR (2003) Chemical alteration of tephra in the depositional environment: theoretical stability modelling. J Quat Sci 18:385–394

    Article  Google Scholar 

  • Pyle DM (1989) The thickness, volume and grainsize of tephra fall deposits. Bull Volcanol 51:1–15

    Article  Google Scholar 

  • Rawson H, Naranjo JA, Smith VC, Fontijn K, Pyle DM, Mather TA, Moreno H (2015) The frequency and magnitude of post-glacial explosive eruptions at Volcán Mocho-Choshuenco, southern Chile. J Volcanol Geotherm Res 299:103–129

    Article  Google Scholar 

  • Rhoades DA, Dowrick DJ, Wilson CJN (2002) Volcanic hazard in New Zealand: scaling and attenuation relations for tephra fall deposits from Taupo Volcano. Nat Hazards 26:147–174

    Article  Google Scholar 

  • Sandiford A, Alloway B, Shane P (2001) A 28000-6600 cal yr record of local and distal volcanism preserved in a paleolake, Auckland, New Zealand. NZ J Geol Geophys 42:323–336

    Article  Google Scholar 

  • Sandri L, Marzocchi W, Gasperini P (2005) Some insights on the occurrence of recent volcanic eruptions of Mount Etna volcano (Sicily, Italy). Geophys J Int 163:1203–1218

    Article  Google Scholar 

  • Shane P (2005) Towards a comprehensive distal andesitic tephrostratigraphic framework for New Zealand based on eruptions from Egmont volcano. J Quat Sci 20:45–57

    Article  Google Scholar 

  • Shane P, Hoverd J (2002) Distal record of multi-sourced tephra in Onepoto Basin, Auckland, New Zealand: implications for volcanic chronology, frequency and hazards. Bull Volcanol 64:441–454

    Article  Google Scholar 

  • Spiegelhalter DJ, Best NG, Carlin BP, van der Linde A (2002) Bayesian measures of model complexity and fit (with discussion). J Roy Stat Soc B 64:583–639

    Article  Google Scholar 

  • Tinkler RJ (2013) A high resolution record of late Quaternary climatic and environmental change in Taranaki. PhD thesis, Massey University, New Zealand

    Google Scholar 

  • Turner MB, Cronin SJ, Bebbington MS, Platz T (2008) Developing a probabilistic eruption forecast for dormant volcanoes; a case study from Mt Taranaki, New Zealand. Bull Volcanol 70:507–515

    Article  Google Scholar 

  • Turner MB, Cronin SJ, Bebbington MS, Smith IEM, Stewart RB (2011) Relating magma composition to eruption variability at andesitic volcanoes: a case study from Mount Taranaki, New Zealand. Bull Geol Soc Am 123:2005–2015

    Article  Google Scholar 

  • Turner MB, Cronin SJ, Bebbington MS, Stewart RB (2009) Merging eruption datasets: building an integrated Holocene eruptive record for Mt Taranaki, New Zealand. Bull Volcanol 71:903– 918

    Article  Google Scholar 

  • Volentik ACM, Bonadonna C, Connor CB, Connor LJ, Rosi M (2010) Modeling tephra dispersal in absence of wind: insights from the climactic phase of the 2450 BP Plinian eruption of Pululagua volcano (Ecuador). J Volcanol Geotherm Res 193:117–136

    Article  Google Scholar 

  • Wadge GPL, Guest JE (1981) Steady-state magma discharge and Etna 1971-81. Nature 294:548–550

    Article  Google Scholar 

  • Walker GPL (1980) The Taupo pumice: product of the most powerful known (ultraplinian) eruption? J Volcanol Geotherm Res 8:69–94

    Article  Google Scholar 

  • Watt SFL, Pyle DM, Naranjo JA, Rosqvist G, Mella M, Mather TA, Moreno H (2011) Holocene tephrochronology of the Hualaihue region (Andean southern volcanic zone ∼42 S) southern Chile. Quat Int 246:324–343

    Article  Google Scholar 

Download references

Acknowledgments

R.G. was supported by a Massey University doctoral scholarship. M.B. and S.J.C. are supported by the New Zealand Natural Hazards Research Platform. We would like to thank Mark Woodhouse and an anonymous reviewer for their very valuable suggestions which helped improve the paper.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Rebecca M. Green.

Additional information

Editorial responsibility: L. Sandri

Electronic supplementary material

Below is the link to the electronic supplementary material.

(PDF 267 KB)

(XLSX 56.3 KB)

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Green, R.M., Bebbington, M.S., Jones, G. et al. Estimation of tephra volumes from sparse and incompletely observed deposit thicknesses. Bull Volcanol 78, 25 (2016). https://doi.org/10.1007/s00445-016-1016-5

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s00445-016-1016-5

Keywords

Navigation