Nine unusually large tsunami deposits from the past 4000 years at Kiritappu marsh along the southern Kuril Trench

• Published in: Sedimentary geology 2007-08, Vol.200 (3), p.275-294
• Main Authors: Nanayama, Futoshi, Furukawa, Ryuta, Shigeno, Kiyoyuki, Makino, Akito, Soeda, Yuji, Igarashi, Yaeko
• Format: Article
• Language: English
• Subjects: AMS 14C age dating; Diatom and pollen analysis; Eastern Hokkaido; Grain size analysis; Kuril subduction zone; Large earthquake; Recurrence interval; Sedimentary structure; Tephrochronology; Tsunami deposit
• ISSN: 0037-0738
• DOI: 10.1016/j.sedgeo.2007.01.008

Large earthquakes along the Kuril subduction zone in northern Japan are known to have caused damaging tsunami, although there is a little information on historical earthquakes and tsunami in this area because no documents exist before the 19th century that might refer to tsunami events. To determine the likely timing and size of future events we need information on their recurrence intervals and to do this for the prehistoric past we have investigated sediments located in the Kiritappu marsh in eastern Hokaido that we interpret as laid down by tsunami. Using reliable multiple lines of evidence from sedimentological, geomorphological, micropaleontological, and chronological results, we identify 13 tsunami sands. Two of these lie within a peat bed above a historical tephra, Ta-a (AD 1739); the upper one probably corresponds to the AD 1843 Tempo Tokachi-oki earthquake ( M 8.2) tsunami, and the lower to either the AD 1952 Tokachi-oki earthquake ( M 8.2) tsunami or the AD 1960 Chilean earthquake ( M 9.5) tsunami. Underlying are 11 prehistoric tsunami sand beds (nine large sand beds and two smaller sand beds) deposited during the past 4000 years. Because of the wide spatial distribution of the large sand beds, and inundation distances inland of between 1200 to 3000 m, we suggest that they record unusually large tsunamis along the Kuril subduction zone. According to our analyses, these tsunami sands were derived from the coastal area and, although they do not show clear graded bedding, they commonly have gradational upper boundaries and erosional bases and include internal sedimentary structures such as plane beds, dunes, and current ripples, reflecting bedload transportation. Based on our results we calculate the recurrence interval of unusually large earthquakes (probably M 8.6) along the Kuril subduction zone as about 365–553 years and estimate the youngest large event to have occurred in the 17th century.