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Distinguishing tsunami and storm deposits: An example from Martinhal, SW Portugal

S. Kortekaas, +1 more
- 15 Aug 2007 - 
- Vol. 200, Iss: 3, pp 208-221
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TLDR
In this paper, the authors used a collection of different data and extensive stratigraphical information from cores as well as trenches to distinguish between tsunami and storm deposits in the same site within a single stratigraphic sequence.
About
This article is published in Sedimentary Geology.The article was published on 2007-08-15. It has received 356 citations till now. The article focuses on the topics: Coastal flood & Storm surge.

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Progress in palaeotsunami research

TL;DR: In this article, the authors review progress with the development of these criteria and identify opportunities for refinements and for extending their application to new settings, with the emphasis on promoting the use of multiple proxies, selected to best match the context of the site or region of interest.
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Expanding the proxy toolkit to help identify past events — Lessons from the 2004 Indian Ocean Tsunami and the 2009 South Pacific Tsunami

TL;DR: In this paper, the authors reviewed some of the proxies used to identify palaeotsunamis, and provided a revised toolkit for the analysis of tsunami data using anisotropy of magnetic susceptibility (AMS).
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Boulder and fine sediment transport and deposition by the 2004 tsunami in Lhok Nga (western Banda Aceh, Sumatra, Indonesia): A coupled offshore–onshore model

TL;DR: In this paper, the authors investigate sediment transport and deposition during the December 26, 2004 tsunami inflow and outflow in the Lhok Nga Bay, located 10 km west of the city of Banda Aceh (northwest Sumatra, Indonesia).
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Large-scale washover sedimentation in a freshwater lagoon from the southeast Australian coast: sea-level change, tsunami or exceptionally large storm?

TL;DR: In this article, a lens of marine sand, up to 90 cm thick, confined vertically by peat, is found in the upper fill of a closed freshwater back-barrier lagoon on the southeast Australian coast.
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Boulder accumulations related to storms on the south coast of the Reykjanes Peninsula (Iceland)

TL;DR: In this article, the authors describe boulder accumulations along the volcanic rock coast of Reykjanes (southwest Iceland) consisting of cliff-top boulders, clusters and ridges, beaches, and boulder fields.
References
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Ecology and palaeoecology of benthic foraminifera

TL;DR: In this article, the authors studied population dynamics relationship between living and dead assemblages in the Atlantic seaboard of North America gulf of Mexico and Caribbean Atlantic SEABoard of South America Atlantic SEBoard of Europe and Africa Atlantic ocean Mediterranean Indian ocean western margin of the Pacific ocean eastern margin of Pacific ocean Pacific ocean Southern ocean Arctic ocean summary of modern distribution patterns and characteristics of assemblage palaeoecology.
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Sedimentary differences between the 1993 Hokkaido-nansei-oki tsunami and the 1959 Miyakojima typhoon at Taisei, southwestern Hokkaido, northern Japan

TL;DR: Tsunami deposits differ distinctly from storm deposits as seen in a trench in the southwestern Hokkaido town of Taisei, which was struck by a typhoon in 1959 and a tsunami in 1993 as discussed by the authors.
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Erosion and Sedimentation from the 17 July, 1998 Papua New Guinea Tsunami

TL;DR: In this paper, the authors describe the erosion and sedimentation associated with the 17 July 1998 Papua New Guinea tsunami, and describe the sedimentation of a layer averaging 8 cm thick of gray sand on a brown muddy soil.
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Sedimentary differences between the 2002 Easter storm and the 15th-century Okoropunga tsunami, southeastern North Island, New Zealand

TL;DR: The sedimentological characteristics of a tsunami and a storm deposit laid down on the same stretch of coastline on the southeast coast of the North Island, New Zealand, are distinctly different as discussed by the authors.
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Geomorphological effects of tsunami run-up and backwash

TL;DR: In this paper, the sedimentology of palaeo-tsunamis has been studied and it has been shown that coastal landscapes may be greatly altered not only by direct tsunami run-up orthogonal to the shoreline, but also by episodes of vigorous backwash and by water flow sub-parallel to the coastline.
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