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Arahama Japan

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Journal Article
Published: 01 June 1989
Clays and Clay Minerals (1989) 37 (3): 219–226.
Image
A: Map showing elevation around <span class="search-highlight">Arahama</span> transect, Sendai Plain, <span class="search-highlight">Japan</span> (base...
Published: 01 October 2012
Figure 1. A: Map showing elevation around Arahama transect, Sendai Plain, Japan (based on 5 m digital elevation model data before tsunami) and Google Earth images of beach at southern end of transect. B: On 4 April 2010. C: On 14 March 2011. D: On 24 March 2011. Beach width was not changed
Image
Beach profiles before and after 2011 Tohoku-oki tsunami (<span class="search-highlight">Japan</span>) at <span class="search-highlight">Arahama</span> ...
Published: 01 October 2012
Figure 3. Beach profiles before and after 2011 Tohoku-oki tsunami (Japan) at Arahama (A) transect. April–July 2011 data are our own measurements, while January–March 2006 and March 2011 (post-tsunami) data are digital elevation model (DEM) data. March (DEM), April, June, and July data include
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2011 Tohoku-oki tsunami (<span class="search-highlight">Japan</span>) deposits. A: At <span class="search-highlight">Arahama</span> transect point A3 (...
Published: 01 October 2012
Figure 4. 2011 Tohoku-oki tsunami (Japan) deposits. A: At Arahama transect point A3 (∼0.25 km from shoreline). Sand deposit is 12 cm in thickness. B: At A29 (∼2.85 km from shoreline). Note thin sand laminae below mud layer in B. Units in cm. C: Liquefaction feature (sand boiling) at rice paddy. D
Journal Article
Journal: Geology
Published: 01 October 2012
Geology (2012) 40 (10): 887–890.
...Figure 1. A: Map showing elevation around Arahama transect, Sendai Plain, Japan (based on 5 m digital elevation model data before tsunami) and Google Earth images of beach at southern end of transect. B: On 4 April 2010. C: On 14 March 2011. D: On 24 March 2011. Beach width was not changed...
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Journal Article
Published: 01 April 2010
Bulletin of the Seismological Society of America (2010) 100 (2): 762–775.
... the mainshock. The parameter k in equation  (3) was set to 0.0001 for all the NIOM analyses conducted in this study. This value does not strongly affect the lag time of the prominent peak shown in Figure  2 . The KSH vertical array is located on the Arahama sand dune, and the surface layer...
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