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. 2018 Jul 17;9:2768. doi: 10.1038/s41467-018-05180-x

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© The Author(s) 2018

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, 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 license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license 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 license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 3 — Glacier geometry along the cross section of GPR and seismic transects. a Cross section of Midgardsormen ridge, as revealed by the seismic measurements in 1998 (location: red dot in Fig. 1). b Glacier geometry along the first 3.2 km of the light blue profile in Fig. 4, according to the airborne radar measurements in 1997. The x-axis coordinates are identical in a and b. The y-axis in a represents the true scale, while the vertical axis is exaggerated three-fold in b