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The 2011 Tohoku-oki Earthquake Tsunami: Similarities and Differences to the 869 Jogan Tsunami on the Sendai Plain

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TLDR
A post-tsunami field survey following the 2011 Tohoku-oki Earthquake Tsunami was carried out to asses inundated area in Sendai Plain, Northeast Japan as mentioned in this paper.
Abstract
A post-tsunami field survey following the 2011 Tohoku-oki Earthquake Tsunami was carried out to asses inundated area in Sendai Plain, Northeast Japan. The type of inundation was classified into two categories (major and minor) according to the amount of accumulated debris, garbage and sediment. Major and minor inundations were identified up to 4 and 5 km from the coastline, respectively. Many artificial geomorphological features, such as roadway embankments and canals, were believed to have affected the run-up process of the tsunami. The inundation area of the 2011 tsunami on the Sendai Plain is compared with that of the 869 Jogan tsunami, which was reconstructed using numerical modeling based on available historical and geological records. The inundation area of the 2011 Tohoku-oki tsunami is comparable to that of the 869 Jogan tsunami, although a direct comparison is difficult due to differences in geomorphological contexts between the paleo period and the present.

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Citations
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Challenges of anticipating the 2011 Tohoku earthquake and tsunami using coastal geology

TL;DR: In this article, the authors used radiocarbon ages just below/above sand deposits left by the pre-Jogan tsunamis suggested recurrence intervals in the range of 500 to 800 years.
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Sediment sources and sedimentation processes of 2011 Tohoku-oki tsunami deposits on the Sendai Plain, Japan — Insights from diatoms, nannoliths and grain size distribution

TL;DR: The authors in this article showed that even very large tsunamis may not transport marine sediments onland and thus many commonly applied indicators of tsunami deposits based on the assumption of their offshore origin (marine diatoms, foraminifera, nannoliths, marine sediment) may be of limited use.
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Geochemical signatures up to the maximum inundation of the 2011 Tohoku-oki tsunami — Implications for the 869 AD Jogan and other palaeotsunamis

TL;DR: In this paper, the authors assessed the geochemical signature of the Tohoku-oki tsunami deposit and underlying soil two months, five months and seven months after the 11 March 2011 tsunami inundated the Sendai Plain.
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Tohoku earthquake: a surprise?

TL;DR: This paper showed that historical magnitudes systematically underestimate this maximum size of future events, but the discrepancy shrinks with time, and the moment conservation principle yields consistent estimates: for all the subduction zones the corner magnitude is of the order 9.0-9.7.
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Relationship between the maximum extent of tsunami sand and the inundation limit of the 2011 Tohoku-oki tsunami on the Sendai Plain, Japan

TL;DR: In this article, the authors focused on the relationship between the maximum extent of sandy tsunami deposits and inundation distance of the 2011 Tohoku-oki tsunami and assessed over seven shore-normal transects along the Sendai Coastal Plain Inundation distances were found to range from 6 to 40 km.
References
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Journal ArticleDOI

Surface deformation due to shear and tensile faults in a half-space

TL;DR: In this paper, a suite of closed analytical expressions for the surface displacements, strains, and tilts due to inclined shear and tensile faults in a half-space for both point and finite rectangular sources are presented.
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Coseismic and postseismic slip of the 2011 magnitude-9 Tohoku-Oki earthquake

TL;DR: The Tohoku-Oki earthquake reminds us of the potential for Mw ≈ 9 earthquakes to occur along other trench systems, even if no past evidence of such events exists, and it is imperative that strain accumulation be monitored using a space geodetic technique to assess earthquake potential.
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Survey of 2011 Tohoku earthquake tsunami inundation and run‐up

TL;DR: In this paper, the authors conducted a tsunami survey along a 2000 km stretch of the Japanese coast from about 50 to 200 km north of Sendai, the narrow bays focused the tsunami waves, generating the largest inundation heights and run-ups.
Journal Article

The 869 Jogan tsunami deposit and recurrence interval of large-scale tsunami on the Pacific coast of northeast Japan

TL;DR: Sediment analysis and hydrodynamic simulation indicate that the tsunami inferred to be triggered by a magnitude 8.3 earthquake spread more than 4 km inland from the Japanese coast as discussed by the authors.
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