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. 2021 Aug 3;11:15703. doi: 10.1038/s41598-021-94866-2

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© The Author(s) 2021

Open AccessThis 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 licence, and indicate if changes were made. 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/4.0/.

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(A) Graph of dune waveheight vs wavelength for subaerial dry and moist pyroclastic flows, eolian, fluvial and aqueous sediment-gravity (epiclastic) flows. Modified from Moorehouse and White (2016) (B) Thickness of surge deposits in the upper, middle, and lower slopes of the southeast sector of TVI. Profiles also show dunes with stoss and lee sides at different gradients of underlying slope.