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Detailing the Impact of the Storegga Tsunami at Montrose, Scotland This is a repository copy of Detailing the impact of the Storegga Tsunami at Montrose, Scotland. White Rose Research Online URL for this paper: https://eprints.whiterose.ac.uk/174960/ Version: Published Version Article: Bateman, Mark D, Kinnaird, Tim C, Hill, Jon orcid.org/0000-0003-1340-4373 et al. (4 more authors) (2021) Detailing the impact of the Storegga Tsunami at Montrose, Scotland. Boreas. 12532. ISSN 0300-9483 https://doi.org/10.1111/bor.12532 Reuse This article is distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs (CC BY-NC-ND) licence. This licence only allows you to download this work and share it with others as long as you credit the authors, but you can’t change the article in any way or use it commercially. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ bs_bs_banner Detailing the impact of the Storegga Tsunami at Montrose, Scotland MARK D. BATEMAN , TIM C. KINNAIRD , JON HILL, ROBERT A. ASHURST, JENNA MOHAN, REBECCA B. I. BATEMAN AND RUTH ROBINSON Bateman, M. D., Kinnaird, T. C., Hill, J., Ashurst, R. A., Mohan, J., Bateman, R. B. I. & Robinson, R.: Detailing the impact of the Storegga Tsunami at Montrose, Scotland. Boreas, https://doi.org/10.1111/bor.12532. ISSN 0300-9483. The Storegga tsunami, dated in Norway to 8150Æ30 cal. years BP,hit many countries bordering the North Sea. Run- upsof>30 m occurredand1000sof kilometres ofcoastwereimpacted.Whilstrecentmodellingsuccessfullygenerated a tsunami wave train, the wave heights and velocities, it under-estimated wave run-ups. Work presented here used luminescence to directly date the Storegga tsunami deposits at the type site of Maryton, Aberdeenshire in Scotland. It also undertook sedimentological characterization to establish provenance, and number and relative power of the tsunami waves. Tsunami model refinement used this to better understand coastal inundation. Luminescence ages successfully date Scottish Storegga tsunami deposits to 8100Æ250 years. Sedimentology showed that at Montrose, three tsunami waves came from the northeast or east, over-ran pre-existing marine sands and weathered igneous bedrock on the coastal plain. Incorporation of an inundation model predicts well a tsunami impacting on the Montrose Basin in terms of replicate direction and sediment size. However, under-estimation of run-up persisted requiring further consideration of palaeotopography and palaeo-near-shore bathymetry for it to agree with sedimentary evidence. Future model evolution incorporating this will be better able to inform on the hazard risk and potential impacts for future high-magnitude submarine generated tsunami events. Mark D. Bateman ([email protected]) and Robert A. Ashurst, Department of Geography, University of Sheffield, Winter St., Sheffield S10 2TN, UK; Tim Kinnaird, Rebecca B. I. Bateman and Ruth Robinson, School of Earth and Environmental Science, St Andrews University, St Andrews KY16 9AL, UK; Jon Hill and Jenna Mohan, Department of Environment and Geography, University of York, Heslington, York YO10 5NG, UK; received 8th December 2020, accepted 7th April 2021. The Storegga tsunami event might be considered the The best age estimate for the Storegga tsunami event is largest natural disaster to hit countries around the North based on AMS radiocarbon dating of mosses ripped up Sea during the last 10 000 years. It was caused by a by thetsunami, whichdirectlydatedthetsunamideposits submarine slide off of the continental slope of south- to 8150Æ30 cal. a BP (Bondevik et al. 2012). As reviewed western Norway (Fig. 1; Haflidason et al. 2005) which by Weninger et al. (2008) and Dawson et al. (2011), many displacedwatergenerating atsunami event(Harbitzet al. other radiocarbon ages bracketing Storegga deposits 2006). Deposits associated with the Storegga tsunami potentially suffer from erosion of the underlying strata have been reported from sites as far apart as Norway, and redeposition of organic material within the tsunami Scotland, and eastern Greenland (Fig. 1A; e.g. Dawson deposit or following the event. This combined with most et al. 1988, 2020; Svendsen & Mangerud 1990; Bondevik radiocarbon ages being measured from bulk samples and et al. 1997, 2005a; Smith et al. 2004, 2007; Wagner et al. the potential for young root penetration led Dawson 2010; Fruergaard et al. 2015; Long et al. 2016). The et al. (2011) to suggest they should be disregarded. As Storegga tsunami has even been connected with the final reviewed by Ishizawa et al. (2020), optically stimulated demise of Mesolithic occupation of Doggerland in the luminescence (OSL) dating offers an alternative North Sea (e.g. Weninger et al. 2008). Proximal sites approachtoradiocarbonandhasthepotentialtodirectly experienced tsunami wave run-up of up to 13 m and date sediment moved in the tsunami event providing that distal sites 3–5 m (Fig. 1A; Smith et al. 2004; Bondevik during the event the sediment eroded and deposited is et al. 2005a; Fruergaard et al. 2015; Rasmussen et al. exposed to sunlight (referred to as bleaching). Brill et al. 2018). Where localized coastal configuration caused (2012) showed for a recent (2004) tsunami deposit in diffraction, refraction, reflection and interference, e.g. in Thailand unbleached residuals were low (~40 years), but island archipelagos like the Shetland Islands, minimum this may be specific to the event and sediments involved. run-ups of >30 m have been reported (Dawson et al. Whilst Gaffney et al. (2020) successfully directly OSL 2020). Reconstructions have calculated that some dated Storegga deposits from Dogger Bank to 8140 13 600 km2 of coastal plain in the southern North Sea, Æ290 years, Shtienberg et al. (2020) applied OSL to from Denmark round to Scotland (but excluding Nor- poorly sorted palaeo-tsunami deposits, which resulted in way), would have been vulnerable to flooding from the age reversals. Careful sediment characterization and Storegga tsunami (Weninger et al. 2008). In Scotland provenance of easily accessible Storegga sediments alone, at least 600 km of coastline was thought to have would allow a better evaluation of whether appropriate been impacted with inundation extending several kilo- bleaching of the luminescence signal happened. If this is metres inland in places (Smith et al. 2004). the case, whilst not able to achieve the age precision DOI 10.1111/bor.12532 © 2021 The Authors. Boreas published by JohnWiley & Sons Ltd on behalf of The Boreas Collegium This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made. 2 Mark D. Bateman et al. BOREAS AB C D Fig. 1. The Storegga tsunami. A. Location of slide causing tsunami (based on Haflidason et al. 2005), location of coastal sites where tsunami deposits reported and estimated wave heights (based on Bondevik et al. 2005a,b; Long et al. 2016; Dawson et al. 2020). Montrose Basin in eastern Scotland shown as red circle. B. Modelled tsunami wave gauge using modern bathymetry for eastern Scotland (Hill et al. 2014). C and D. Modelled tsunami wave map showing distribution of first and second major waves to hit Scotland (Hill et al. 2014). obtained in Norway using the AMS on moss (Bondevik any coastal inundation. Coasts were treated in the model et al. 2012), OSL would allow dating of tsunami as vertical cliffs. Thus, when model outputs of run-up sediments where no organic material has been preserved. were compared to run-up heights from reported inland OSL dating could also help to distinguish Storegga deposits, the model tended to under-estimate. The other tsunami sediments from other less well-documented significant finding was that numerical resolution of near- tsunami (e.g. Bondevik et al. 2005b). shore bathymetry and coastline is important to minimize Hill et al. (2014) presented a multiscale 3D finite the difference between the modelled and geological element, non-hydrostatic numerical model of the tsu- record of run-up. Higher resolutions were not under- nami generated by the Storegga slide. This assumed a taken for such a large spatial area as they were compu- simplified block sliding to trigger the event and used tationally prohibitive. palaeo-bathymetry based on that of the present day The Storegga tsunami event is perhaps the best adjusted for isostatic rebound using data from Bradley examined and mapped out palaeo-tsunami. As such, it et al. (2011). Palaeo-coastlineswere derived from the 0-m holds the potential to inform present-day coastal man- contour. Results were able to successfully generate a agers to help them assess the hazard risk and potential tsunami wavetrain (Fig. 1B), wave heights and velocities impact for future high-magnitude submarine generated as well as plot wave movement for the equivalent of 15 h tsunami events (e.g. Jaffe et al. 2012; Sugawara et al. (Fig. 1C, D). At least two major waves were modelled to 2014). Future slides from the Storegga region could have impacted on Scotland (Fig. 1B, D) and a wave with happen but more likely is a similar event happening from an estimated 5 m run-up predicted to have over-washed Greenland or from volcano flank collapse e.g. in the most of Doggerland. Whilst very powerful, one of the Canaries (Harbitz et al. 2014). The aims of this paper are acknowledged limitations of the Hill et al. (2014) model to (i) establish the provenance of the tsunami sediment was it only modelled the wave up to the coastline and not deposited at the type site of Maryton and in doing so BOREAS Impact of the Storegga Tsunami at Montrose, Scotland 3 evaluate the likelihood of the OSL signal being bleached, water run-up was estimated at 11.1 m (Smith et al.2007).
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