Abstract
Growing evidence indicates that glacial cycles influence volcanic activity, yet the physical mechanisms linking glaciation to magmatic processes in continental arcs remain unclear. We integrate realistic ice and topographic loads with a dike model to evaluate how glaciation modulated magma ascent beneath Mocho-Choshuenco, Chile, during the Last Glacial Maximum (LGM). Ice loading generates a crustal stress “pinch point” that causes dikes rising from lower-crustal reservoirs to stall deeper than under ice-free conditions, effectively shutting off recharge to shallow magma reservoirs. This mechanism explains the ~2-3 km increase in magma storage depth and reduced eruption rates during the LGM without invoking changes in mantle melt supply or reservoir strength. Shutting off recharge also favors magma differentiation, setting the stage for more explosive silicic eruptions during deglaciation once recharge resumes. We identify a parsimonious explanation for glacially-driven shifts in magma composition, storage depth, and eruption rate at Mocho-Choshuenco and arc volcanoes worldwide.
Similar content being viewed by others
Data availability
No new data aside from model outputs were generated. The numerical data generated in this study have been deposited in the Zenodo database under accession code: https://doi.org/10.5281/zenodo.18320729.
Code availability
The Matlab codes used to perform dike model simulations and all output files used to produce manuscript figures are publicly available on Zenodo: https://doi.org/10.5281/zenodo.18320729.
References
Sigvaldason, G. E., Annertz, K. & Nilsson, M. Effect of glacier loading/deloading on volcanism: postglacial volcanic production rate of the Dyngjufjöll area, central Iceland. Bull. Volcanol. 54, 385–392 (1992).
Maclennan, J., Jull, M., McKenzie, D., Slater, L. & Grönvold, K. The link between volcanism and deglaciation in Iceland. Geochem. Geophys. Geosyst. 3, 1–25 (2002).
Huybers, P. & Langmuir, C. Feedback between deglaciation, volcanism, and atmospheric CO2. Earth Planet. Sci. Lett. 286, 479–491 (2009).
Kutterolf, S. et al. A detection of Milankovitch frequencies in global volcanic activity. Geology 41, 227–230 (2013).
Kutterolf, S., Schindlbeck, J. C., Jegen, M., Freundt, A. & Straub, S. M. Milankovitch frequencies in tephra records at volcanic arcs: the relation of kyr-scale cyclic variations in volcanism to global climate changes. Quat. Sci. Rev. 204, 1–16 (2019).
Nyland, R. E. et al. Volcanic activity and its link to glaciation cycles: single-grain age and geochemistry of Early to Middle Miocene volcanic glass from ANDRILL AND-2A core, Antarctica. J. Volcanol. Geotherm. Res. 250, 106–128 (2013).
Wanket, S., Jellinek, A. M. & Johnson, C. L. Potential ice sheet modulation of volcanism in West Antarctica: constraints on the cadence and magnitude of melt delivery into the crust. J. Geophys. Res. Solid Earth 130, e2024JB029730 (2025).
Schindlbeck, J. C. et al. 100- kyr cyclicity in volcanic ash emplacement: evidence from a 1.1 Myr tephra record from the NW Pacific. Sci. Rep. 8, 4440 (2018).
Coonin, A. N. et al. Magma chamber response to ice unloading: applications to volcanism in the West Antarctic Rift System. Geochem. Geophys. Geosyst. 25, e2024GC011743 (2024).
Jull, M. & McKenzie, D. The effect of deglaciation on mantle melting beneath Iceland. J. Geophys. Res. Solid Earth 101, 21815–21828 (1996).
Licciardi, J. M., Kurz, M. D. & Curtice, J. M. Glacial and volcanic history of Icelandic table mountains from cosmogenic 3He exposure ages. Quat. Sci. Rev. 26, 1529–1546 (2007).
Huybers, P. & Langmuir, C. H. Delayed CO2 emissions from mid-ocean ridge volcanism as a possible cause of late-Pleistocene glacial cycles. Earth Planet. Sci. Lett. 457, 238–249 (2017).
Satow, C. et al. Eruptive activity of the Santorini Volcano controlled by sea-level rise and fall. Nat. Geosci. 14, 586–592 (2021).
Watt, S. F. L., Pyle, D. M. & Mather, T. A. The volcanic response to deglaciation: Evidence from glaciated arcs and a reassessment of global eruption records. Earth-Sci. Rev. 122, 77–102 (2013).
Conway, C. E., Pure, L. R. & Ishizuka, O. An assessment of potential causal links between deglaciation and eruption rates at arc volcanoes. Front. Earth Sci. 11, 1082342 (2023).
Rawson, H. et al. The magmatic and eruptive response of arc volcanoes to deglaciation: Insights from southern Chile. Geology 44, 251–254 (2016).
Singer, B. S. et al. New perspectives on ice forcing in continental arc magma plumbing systems. J. Volcanol. Geotherm. Res. 455, 108187 (2024).
Moreno-Yaeger, P. et al. Pleistocene to recent evolution of Mocho-Choshuenco volcano during growth and retreat of the Patagonian Ice Sheet. Geol. Soc. Am. Bull. 136, 5262–5282 (2024).
Moreno et al. Expansion and contraction of the Patagonian Ice Sheet and its influence on magma storage beneath Mocho-Choshuenco Volcano, Chile. J. Geophys. Res. Solid Earth 130, e2025JB031528 (2025).
Geyer, A. & Bindeman, I. Glacial influence on caldera-forming eruptions. J. Volcanol. Geotherm. Res. 202, 127–142 (2011).
Mora, D. & Tassara, A. Upper crustal decompression due to deglaciation-induced flexural unbending and its role on post-glacial volcanism at the Southern Andes. Geophys. J. Int. 216, 1549–1559 (2019).
Wilson, A. M. & Russell, J. K. Glacial pumping of a magma-charged lithosphere: A model for glaciovolcanic causality in magmatic arcs. Earth Planet. Sci. Lett. 548, 116500 (2020).
Jellinek, A. M., Manga, M. & Saar, M. O. Did melting glaciers cause volcanic eruptions in eastern California? Probing the mechanics of dike formation. J. Geophys. Res. Solid Earth 109, https://doi.org/10.1029/2004JB002978 (2004).
Rivalta, E., Taisne, B., Bunger, A. P. & Katz, R. F. A review of mechanical models of dike propagation: schools of thought, results and future directions. Tectonophysics 638, 1–42 (2015).
Rawson, H. et al. The frequency and magnitude of post-glacial explosive eruptions at Volcán Mocho-Choshuenco, southern Chile. J. Volcanol. Geotherm. Res. 299, 103–129 (2015).
Cuzzone, J., Romero, M. & Marcott, S. A. Modeling the timing of Patagonian Ice Sheet retreat in the Chilean Lake District from 22–10 ka. Cryosphere 18, 1381–1398 (2024).
Hickey-Vargas, R., Holbik, S., Tormey, D., Frey, F. A. & Moreno Roa, H. Basaltic rocks from the Andean Southern Volcanic Zone: insights from the comparison of along-strike and small-scale geochemical variations and their sources. Lithos 258–259, 115–132 (2016).
Moreno, P. I. et al. Radiocarbon chronology of the Last Glacial Maximum and its termination in northwestern Patagonia. Quat. Sci. Rev. 122, 233–249 (2015).
Alloway, B. V. et al. Refinement of the tephrostratigraphy straddling the northern Patagonian Andes (40–41°S): new tephra markers, reconciling different archives and ascertaining the timing of piedmont deglaciation. J. Quat. Sci. 37, 441–477 (2022).
Lister, J. R. & Kerr, R. C. Fluid-mechanical models of crack propagation and their application to magma transport in dykes. J. Geophys. Res. Solid Earth 96, 10049–10077 (1991).
Rubin, A. M. Getting granite dikes out of the source region. J. Geophys. Res. Solid Earth 100, 5911–5929 (1995).
Maccaferri, F., Bonafede, M. & Rivalta, E. A quantitative study of the mechanisms governing dike propagation, dike arrest and sill formation. J. Volcanol. Geotherm. Res. 208, 39–50 (2011).
Muller, J. R., Ito, G. & Martel, S. J. Effects of volcano loading on dike propagation in an elastic half-space. J. Geophys. Res. Solid Earth 106, 11101–11113 (2001).
Urbani, S., Acocella, V., Rivalta, E. & Corbi, F. Propagation and arrest of dikes under topography: models applied to the 2014 Bardarbunga (Iceland) rifting event. Geophys. Res. Lett. 44, 6692–6701 (2017).
Urbani, S., Acocella, V. & Rivalta, E. What drives the lateral versus vertical propagation of dikes? Insights from analogue models. J. Geophys. Res. Solid Earth 123, 3680–3697 (2018).
Furst, S., Maccaferri, F. & Pinel, V. Modeling the shape and velocity of magmatic intrusions, a new numerical approach. J. Geophys. Res. Solid Earth 128, e2022JB025697 (2023).
Townsend, M. & Huber, C. A critical magma chamber size for volcanic eruptions. Geology 48, 431–435 (2020).
Tassara, A., Götze, H.-J., Schmidt, S. & Hackney, R. Three-dimensional density model of the Nazca plate and the Andean continental margin. J. Geophys. Res. Solid Earth 111, https://doi.org/10.1029/2005JB003976 (2006).
Jaeger, J. C., Cook, N. G. W. & Zimmerman, R. Fundamentals of Rock Mechanics (John Wiley & Sons, 2009).
Pinel, V. & Jaupart, C. The effect of edifice load on magma ascent beneath a volcano. Philos. Trans. R. Soc. Lond. Ser. Math. Phys. Eng. Sci. 358, 1515–1532 (2000).
Mantiloni, L., Rivalta, E. & Davis, T. Mechanical modeling of pre-eruptive magma propagation scenarios at calderas. J. Geophys. Res. Solid Earth 128, e2022JB025956 (2023).
Moon, S., Perron, J. T., Martel, S. J., Holbrook, W. S. & St. Clair, J. A model of three-dimensional topographic stresses with implications for bedrock fractures, surface processes, and landscape evolution. J. Geophys. Res. Earth Surf. 122, 823–846 (2017).
Turcotte, D. L. & Schubert, G. Geodynamics (Cambridge University Press, 2002).
Sigmundsson, F. et al. Climate effects on volcanism: influence on magmatic systems of loading and unloading from ice mass variations, with examples from Iceland. Philos. Trans. R. Soc. Math. Phys. Eng. Sci. 368, 2519–2534 (2010).
Segall, P., Cervelli, P., Owen, S., Lisowski, M. & Miklius, A. Constraints on dike propagation from continuous GPS measurements. J. Geophys. Res. Solid Earth 106, 19301–19317 (2001).
Patrick, M. R. et al. Cyclic lava effusion during the 2018 eruption of Kīlauea Volcano. Science 366, eaay9070 (2019).
Wang, T., Zheng, Y., Pulvirenti, F. & Segall, P. Post-2018 caldera collapse re-inflation uniquely constrains Kīlauea’s magmatic system. J. Geophys. Res. Solid Earth 126, e2021JB021803 (2021).
Townsend, M. & Huang, M. Timescales of dike growth and chamber deflation constrain magma storage and transport pathways during Kīlauea’s 2018 lower east rift zone intrusion. J. Geophys. Res. Solid Earth 127, e2022JB025636 (2022).
Iacovino, K. & Till, C. B. DensityX: a program for calculating the densities of magmatic liquids up to 1,627 °C and 30 kbar. Volcanica 2, 1–10 (2019).
Spence, D. A. & Turcotte, D. L. Buoyancy-driven magma fracture: a mechanism for ascent through the lithosphere and the emplacement of diamonds. J. Geophys. Res. Solid Earth 95, 5133–5139 (1990).
Rubin, A. M. Propagation of magma-filled cracks. Annu. Rev. Earth Planet. Sci. 23, 287–336 (1995).
Pollard, D. D. & Segall, P. Theoretical displacements and stresses near fractures in rock: with applications to faults, joints, veins, dikes, and solution surfaces. in Fracture Mechanics of Rock (ed. Atkinson, B. K.) 277–347 (Academic Press Inc., London, 1987).
Jellinek, A. M. & DePaolo, D. J. A model for the origin of large silicic magma chambers: precursors of caldera-forming eruptions. Bull. Volcanol. 65, 363–381 (2003).
Degruyter, W. & Huber, C. A model for eruption frequency of upper crustal silicic magma chambers. Earth Planet. Sci. Lett. 403, 117–130 (2014).
Richter, D. H. Chronological Narrative of the 1959-60 Eruption of Kilauea Volcano, Hawaii: A Detailed and Pictorial Account of an Eruptive Sequence Consisting of a Summit Eruption, a Flank Eruption, and a Summit Collapse (U.S. Government Printing Office, 1970).
Pinel, V. & Jaupart, C. Magma storage and horizontal dyke injection beneath a volcanic edifice. Earth Planet. Sci. Lett. 221, 245–262 (2004).
Acknowledgements
The authors would like to acknowledge the following funding sources: NSF EAR-2444709 and NSF EAR-2123211 to M.T., NSF EAR-2123216 to A.H., NSF EAR-2121655 to C.H., and NSF EAR-2121570 to B.S. In addition, the authors thank Joshua Cuzzone for sharing Patagonian Ice Sheet thickness data files.
Author information
Authors and Affiliations
Contributions
Meredith Townsend: writing—original draft, conceptualization, methodology, validation, investigation, visualization. Pablo Moreno-Yaeger: data curation, writing—review and editing. Andrew Harp: methodology, writing—review and editing. Christian Huber: writing—review and editing. Brad S. Singer: writing—review and editing.
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing interests.
Peer review
Peer review information
Nature Communications thanks Lorenzo Mantiloni, and the other, anonymous, reviewer for their contribution to the peer review of this work. A peer review file is available.
Additional information
Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary information
Rights and permissions
Open Access This article is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License, which permits any non-commercial use, sharing, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if you modified the licensed material. You do not have permission under this licence to share adapted material derived from this article or parts of it. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by-nc-nd/4.0/.
About this article
Cite this article
Townsend, M., Moreno-Yaeger, P., Harp, A. et al. Stress pinch points from glacial loading modulate magma ascent and storage in continental arcs. Nat Commun (2026). https://doi.org/10.1038/s41467-026-69485-y
Received:
Accepted:
Published:
DOI: https://doi.org/10.1038/s41467-026-69485-y


