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Stress pinch points from glacial loading modulate magma ascent and storage in continental arcs
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  • Published: 20 February 2026

Stress pinch points from glacial loading modulate magma ascent and storage in continental arcs

  • Meredith Townsend  ORCID: orcid.org/0000-0001-8846-14661,
  • Pablo Moreno-Yaeger  ORCID: orcid.org/0000-0001-5219-45462,
  • Andrew Harp3,
  • Christian Huber  ORCID: orcid.org/0000-0001-6518-710X4 &
  • …
  • Brad S. Singer  ORCID: orcid.org/0000-0003-3595-51682 

Nature Communications , Article number:  (2026) Cite this article

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We are providing an unedited version of this manuscript to give early access to its findings. Before final publication, the manuscript will undergo further editing. Please note there may be errors present which affect the content, and all legal disclaimers apply.

Subjects

  • Climate change
  • Palaeoclimate
  • Tectonics
  • Volcanology

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.

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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.

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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

  1. Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, PA, USA

    Meredith Townsend

  2. Department of Geoscience, University of Wisconsin-Madison, Madison, WI, USA

    Pablo Moreno-Yaeger & Brad S. Singer

  3. Department of Earth and Environmental Sciences, California State University, Chico, Chico, CA, USA

    Andrew Harp

  4. Department of Earth, Environmental and Planetary Sciences, Brown University, Providence, RI, USA

    Christian Huber

Authors
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  2. Pablo Moreno-Yaeger
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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

Correspondence to Meredith Townsend.

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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

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  • Received: 26 November 2025

  • Accepted: 03 February 2026

  • Published: 20 February 2026

  • DOI: https://doi.org/10.1038/s41467-026-69485-y

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