Skip to main content

Advertisement

Log in

Experimental formation of Pele’s hairs and tears at 1200°C under atmospheric pressure from natural alkali olivine basalt

  • Published:
Journal of Earth System Science Aims and scope Submit manuscript

Abstract

The formation of Pele’s hairs and tears (PH and PT) is generally associated with fluid-charged rapid explosive basaltic volcanism on Earth’s surface. Their formation and relationship with eruption types have led to a sudden increase in theoretical and experimental studies in recent years. Unlike previous experimental setups, the present study successfully formed these volcanic structures using a simple experimental design. The viscosity of basaltic melt was lowered to <100 Pa·s at 1200°C under 1 atmospheric pressure using a novel cylinder-in-cylinder graphite sample chamber for the in-situ fluxing of excess fluids into the melt system. The abundance of vesicles in the basaltic melt observed in mesoscopic to sub-microscopic scales suggests the presence of fluid phase in excess, its decoupling and degassing. The dissolved gas species in the experimentally generated melt are confirmed by the Fourier transform infrared spectroscopic analyses. The PH and PT formed during the present study compare morphologically very well to their known natural and experimental counterparts, and are found to be compositionally similar. They display a small range of chemical variations and exhibit a good chemical homogeneity similar to their natural analogues.

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.

Figure 1
Figure 2
Figure 3
Figure 4
Figure 5
Figure 6

Similar content being viewed by others

References

  • Andronico D, Cristaldi A, Del Carlo P and Taddeucci J 2009 Shifting styles of basaltic explosive activity during the 2002–03 eruption of Mt. Etna, Italy; J. Volcanol. Geotherm. Res. 180(2–4) 110–122.

  • Blank J G and Brooker R A 1994 Experimental studies of carbon dioxide in silicate melts: Solubility, speciation, and stable carbon isotope behavior; In: Volatiles in magmas (eds) Carroll M R and Holloway J R, Rev. Mineral. Geochem. 30(1) 157–186.

  • Brooker R A, Kohn S C, Holloway J R and McMillan P F 2001 Structural controls of the solubility of CO2 in silicate melts. Part I: Bulk solubility data; Chem. Geol. 174(1–3) 225–239.

  • Cannata C B, De Rosa R, Houghton B, Donato P and Nudo A 2011 Pele’s hair: Case studies from Kilauea volcano and Vulcanello (Aeolian Islands); Acta Vulcanol. 23(1–2) 27–34.

  • Cannata C B, De Rosa R, Donato P, Donato S, Lanzafame G, Mancini G and Houghton B F 2019 First 3D imaging characterization of Pele’s hair from Kilauea volcano (Hawaii); Sci. Rep. 9(1) 1–13.

  • Clague D A, Batiza R, Head J W and Davis A S 2003 Pyroclastic and hydroclastic deposits on Loihi Seamount, Hawaii; AGU Geophys. Monogr. Ser. 140 73–95.

  • Comida P P, Ross P S, Zimanowski B and Büttner R 2018 Artificial juvenile pyroclasts from wet and dry “eruptions”: Impact of magma composition on grain sizes and particle shapes; In: Earth and Environmental Sciences Day - JSTE, Quebec, Canada.

  • Crisp J, Cashman K V, Bonini J A, Houghen S B and Pierie D C 1994 Crystallization history of the 1984 Mauna Loa lava flow; J. Geophys. Res. 99(B4) 7177–7198.

  • Cucciniello C, Choudhary A K, Pande K and Sheth H 2019 Mineralogy, geochemistry and 40Ar-39Ar geochronology of the Barda and Alech complexes, Saurashtra, northwestern Deccan Traps: Early silicic magmas derived by flood basalt fractionation; Geol. Mag. 156(10) 1668–1690.

  • Di Genova D, Romano C, Alletti M, Misiti V and Scarlato P 2014 The effect of CO2 and H2O on Etna and Fondo Riccio (Phlegrean Fields) liquid viscosity, glass transition temperature and heat capacity; Chem. Geol. 377 72–86.

  • Duffield W A, Gibson E K and Heiken G 1977 Some characteristics of Pele’s hair; J. Res. US Geol. Surv. 5(1) 93–101.

  • Giordano D, Russell J K and Dingwell D B 2008 Viscosity of magmatic liquids: A model; Earth Planet. Sci. Lett. 271(1–4) 123–134.

  • Hamilton V E, Morris R V, Gruener J E and Mertzman S A 2008 Visible, near-infrared, and middle infrared spectroscopy of altered basaltic tephras: Spectral signatures of phyllosilicates, sulfates, and other aqueous alteration products with application to the mineralogy of the Columbia Hills of Gusev Crater, Mars; J. Geophys. Res. Planets 113(E12).

  • Hazlett R W and Hyndman D W 1996 Roadside Geology of Hawaii; Mountain Press Publishing Company, Montana, USA, 318p.

  • Heiken G 1972 Morphology and petrography of volcanic ashes; Geol. Soc. Am. Bull. 83(7) 1961–1988.

  • Heiken G and Wohletz K 1985 Volcanic ash; University Presses of California, Chicago, Harvard and MIT, USA, 245p.

  • Hess K U and Dingwell D D 1996 Viscosities of hydrous leucogranitic melts: A non-Arrhenian model; Am. Mineral. 81(9–10) 1297–1300.

  • Ho A M and Cashman K V 1997 Temperature constraints on the Ginkgo flow of the Columbia River Basalt Group; Geology 25(5) 403–406.

  • John B, Singh Y, Rao D T, Barman M C, Pradeepkumar A P and Sanjeev K 2021 Observation on rock melt extrusion occurrence in southern part of Tamil Nadu; J. Geol. Soc. India 97(2) 119–124.

  • Katsura T 1967 Pele’s hair as a liquid of Hawaiian tholeiitic basalts; Geochem. J. 1(4) 157–168.

  • Keszthelyi L P and Pieri D C 1993 Emplacement of the 75-km-long Carrizozo lava flow field, south-central New Mexico; J. Volcanol. Geotherm. Res. 59(1–2) 59–75.

  • Keszthelyi S and Self S 1998 Some physical requirements for the emplacement of long basaltic lava flows; J. Geophys. Res. 103(B11) 27,447–27,464.

  • Konschak A and Keppler H 2014 The speciation of carbon dioxide in silicate melts; Contrib. Mineral. Petrol. 167(5) 1–13.

  • Larsen E S 1929 The temperatures of magmas; Am. Mineral. 14(3) 81–94.

  • Lightfoot P C, Hawkesworth C J and Sethna S F 1987 Petrogenesis of rhyolites and trachytes from the Deccan Trap: Sr, Nd and Pb isotope and trace element evidence; Contrib. Mineral. Petrol. 95(1) 44–54.

  • Macdonald G A 1949 Hawaiian petrographic province; Geol. Soc. Am. Bull. 60(10) 1541–1596.

  • Mastin L G, Spieler O and Downey W S 2009 An experimental study of hydromagmatic fragmentation through energetic, non-explosive magma-water mixing; J. Volcanol. Geotherm. Res. 180(2–4) 161–170.

  • McBirney A R 1993 Igneous Petrology; Jones and Bartlett Learning, USA, 508p.

  • McMillan P F 1994 Water solubility and speciation models; In: Volatiles in magmas (eds) Carroll M R and Holloway J R, Berlin, Boston: De Gruyter, pp. 131–156.

  • Michalski J R, Kraft M D, Diedrich T, Sharp T G and Christensen P R 2003 Thermal emission spectroscopy of the silica polymorphs and considerations for remote sensing of Mars; Geophys. Res. Lett. 30(19).

  • Morizet Y, Kohn S C and Brooker R A 2001 Annealing experiments on CO2-bearing jadeite glass: An insight into the true temperature dependence of CO2 speciation in silicate melt; Mineral. Mag. 65(6) 701–707.

  • Morizet Y, Nichols A R L, Kohn S C, Brooker R A and Dingwell D B 2007 The influence of H2O and CO2 on the glass transition temperature: Insights into the effects of volatiles on magma viscosity; Eur. J. Mineral. 19(5) 657–669.

  • Moune S, Faure F, Gauthier P J and Sims K W 2007 Pele’s hairs and tears: Natural probe of volcanic plume; J. Volcanol. Geotherm. Res. 164(4) 244–253.

  • Murase T and McBirney A R 1973 Properties of some common igneous rocks and their melts at high temperatures; Geol. Soc. Am. Bull. 84(11) 3563–3592.

  • Mysen B O 1977 The solubility of H2O and CO2 under predicted magma genesis conditions and some petrological and geophysical implications; Rev. Geophys. 15(3) 351–361.

  • Ni H and Keppler H 2013 Carbon in silicate melts; Rev. Mineral. Geochem. 75(1) 251–287.

  • Niyogi A, Pati J K, Patel S C, Panda D and Patil S K 2011 Anthropogenic and impact spherules: Morphological similarity and chemical distinction – A case study from India and its implications; J. Earth Syst. Sci. 120(6) 1043–1054.

  • Nowak M, Porbatzki D, Spickenbohm K and Diedrich O 2003 Carbon dioxide speciation in silicate melts: A restart; Earth Planet. Sci. Lett. 207(1–4) 131–139.

  • Ochs F A and Lange R A 1999 The density of hydrous magmatic liquids; Science 283(5406) 1314–1317.

  • Pati J K 1985 Surface tension measurements on artificial and natural silicate melts; M.Tech. Dissertation Thesis, University of Roorkee, India, 37p.

  • Pati J K, Arima M and Gupta A K 2000 Experimental study of the system diopside-albite-nepheline at P(H2O) = P(Total) = 2 and 10 kbar and at P(Total) = 28 kbar; Can. Mineral. 38(5) 1177–1191.

  • Porritt L A, Russell J K and Quane S L 2012 Pele’s tears and spheres: Examples from Kilauea Iki; Earth Planet. Sci. Lett. 333 171–180.

  • Ramsey M S and Fink J H 1999 Estimating silicic lava vesicularity with thermal remote sensing: A new technique for volcanic mapping and monitoring; Bull. Volcanol. 61(1) 32–39.

  • Robert G, Knipping J L, Scherbarth S, Robertson T E, Stechern A, Behrens H and Whittington A G 2015 Heat capacity and viscosity of basaltic melts with H2O ± F ± CO2; Chem. Geol. 418 51–65.

  • Seifert R, Malfait W J, Lerch P and Sanchez-Valle C 2013 Partial molar volume and compressibility of dissolved CO2 in glasses with magmatic compositions; Chem. Geol. 358 119–130.

  • Shellnutt J G, Bhat G M, Wang K L, Brookfield M E, Dostal J and Jahn B M 2012 Origin of the silicic volcanic rocks of the Early Permian Panjal Traps, Kashmir, India; Chem. Geol. 334 154–170.

  • Shimozuru D 1994 Physical parameters governing the formation of pele’s hair and tears; Bull. Volcanol. 56(3) 217–219.

  • Shishkina T, Botcharnikov R E, Holtz F, Almeev R R, Jazwa A M and Jakubiak A A 2014 Compositional and pressure effects on the solubility of H2O and CO2 in mafic melts; Chem. Geol. 388 112–129.

  • Spina G L, Arzilli F, Llewellin E W, Burton M R, Clarke A B, Vitturi M M, Polacci M, Hartley M E, Genova D D and Mader H M 2021 Explosivity of basaltic lava fountains is controlled by magma rheology, ascent rate and outgassing; Earth Planet. Sci. Lett. 553(116658) 1–11.

  • Usmani M 2017 A study of spherules and melts from Lonar impact structure, India; PhD Thesis, University of Allahabad, Prayagraj, India, 356p.

  • Villermaux E 2012 The formation of filamentary structures from molten silicates: Pele’s hair, angel hair and blown clinker; C. R. Mecanique 340(8) 555–564.

  • Walker D and Mullins O 1981 Surface tension of natural silicate melts from 1200–1500°C and implications for melt structure; Contrib. Mineral. Petrol. 76(4) 455–462.

  • Wilson L 1999 Explosive volcanic eruptions-X. The influence of pyroclast size distributions and released magma gas contents on the eruption velocities of pyroclasts and gas in Hawaiian and Plinian eruptions; Geophys. J. Int. 136(3) 609–619.

Download references

Acknowledgements

This study is based on an M.Sc. Dissertation project of MZ. AKS expresses his sincere thanks to the Council of Scientific and Industrial Research (CSIR), New Delhi, India, for providing him with financial assistance in the form of Shyama Prasad Mukherjee Fellowship [SPM-09/001(0328)/2020-EMR-I] and also, acknowledges the Department of Science and Technology (DST), Government of India, for the INSPIRE Fellowship (IF170168). Dr Kamlesh Pandey, NCEMP, the University of Allahabad is thanked for the FTIR runs. We are grateful to the Editor Professor Somnath Dasgupta and the two anonymous reviewers for their constructive comments and suggestions, which helped to improve the manuscript.

Author information

Authors and Affiliations

Authors

Contributions

JKP conceived the problem and designed the experiment. The experiments and analyses were carried out by MZ, AKS, AA and MMD. JKP: Conceptualization, sample collection, supervision, writing, interpretation, and validation. MZ and AKS: Experimental investigation, laboratory analysis, data compilation, writing, interpretation, and validation. MMD, SD, and AA: Experimental investigation and laboratory analysis.

Corresponding author

Correspondence to Anuj Kumar Singh.

Additional information

Communicated by Somnath Dasgupta

Corresponding editor: Somnath Dasgupta

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Zahbi, M., Singh, A.K., Pati, J.K. et al. Experimental formation of Pele’s hairs and tears at 1200°C under atmospheric pressure from natural alkali olivine basalt. J Earth Syst Sci 132, 47 (2023). https://doi.org/10.1007/s12040-023-02061-w

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s12040-023-02061-w

Keywords

Navigation