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Some of you will recall Burberry's The Art of the Trench site, which shows images of people in their trench coats.
Therefore, secondary deposits by post-tsunami surface processes are easily deposited at the trench site, resulting in the contamination of old carbon just above the tsunami deposits.
HFF Himalayan Frontal Fault, PT Patu Thrust, BT Bardibas Thrust, Red lines are the active faults, Location marked in yellow are the trench site location by previous workers.
The average recurrence interval of tsunami deposits is calculated to be 350 390 years using the modeled date of the E11 deposits in Model B and the number of identified events at the trench site.
Fig. 3 a Distribution of surface ruptures (red lines), previously mapped active fault traces (blue lines), and locations of photographs (solid circles) and the trench site (yellow box) along the Takano-Shirahata segment of the Hinagu fault zone (Fig. 1c).
However, the right-lateral strike-slip around this trench site was only ~0.5 m in 2016 (Kumahara et al. 2016), as compared to the maximum right-lateral strike-slip of ~2 m to the northeast.
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Fig. 5 Photographs around the trench sites.
Although both tsunamis inundated up to the trench sites, only single-event deposits were identified from AD 2011 to 1660.
According to interviews with landowners, no storm deposits have settled in the trench sites during the past 40 50 years.
Furthermore, the KYD-trench is located 300 m inland from the beach, and landowners reported no storm deposits in the trench sites during the past 40 50 years.
From these data, we consider that the present depositional setting (beach ridge and behind marsh) around the trench sites was already established by 6 ka.
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