著者
橋本関雪著
出版者
中央美術社
巻号頁・発行日
1924
著者
野村 英明
雑誌
日本プランクトン学会報 (ISSN:03878961)
巻号頁・発行日
vol.44, no.1, pp.40-42, 1997-08-31
参考文献数
27
著者
田中 圭 中田 高 松浦 律子 田力 正好 松田 時彦
出版者
公益社団法人 東京地学協会
雑誌
地學雜誌 (ISSN:0022135X)
巻号頁・発行日
vol.127, no.3, pp.305-323, 2018
被引用文献数
1

<p> <i>Kambara Jishinyama</i> (earthquake-mound) located on the west bank of lower reach of the Fujikawa river, is widely believed to be a mound that was tectonically formed at the time of the 1854 Ansei Tokai earthquake. Using old maps and aerial photogtaphs, geomorphological changes around <i>Kambara Jishinyama</i> before and after the earthquake are examined. The Fujikawa river frequently flooded and the course on its west bank changed especially after construction of the <i>Karigane-zutsumi</i> (big bank) in order to protect farmland on its east bank. The area around the lower reach of the river was surveyed in 1803 for the <i>Dai Nihon Enkai Yochizu</i> large-scale map, which is the so-called <i>Ino-Daizu</i>. On that map, the river was at almost the same location as its present course. The historical road map (<i>Kaido-Ezu</i>) of <i>Tokaido</i>, which was the trunk road connecting Edo and Kyoto, illustrated in the same period as <i>Ino-Daizu</i>, shows that the Fujikawa river shifted its course close to the foot of river terraces at the west bank. Due to lateral erosion of the river, part of the <i>Tokaido</i> between the towns of Iwabuchi and Kambara collapsed several times. Subsequently, the road was diverted to the new route via Shinzaka as shown on the 1:20,000 scale topographic map published in 1890. A micro-landform classification map of the alluvial lowland of the west bank of the Fujikawa river based on interpretations of aerial photographs taken in 1952 and 1953 reveals that <i>Kambara Jishinyama</i> was located on one of the former mid-channel bars in the braided channels of the river before the 1854 Ansei Tokai earthquake. The earthquake caused a large landslide that dammed the Fujikawa river for a short period at the foot of Shiratori-yama to the north of Iwabuchi. The discharged flood water changed the river course close to the present stream. Geomorphic evidence for tectonic uplift does not exist around <i>Kambara Jishinyama</i>. The Koike river, a small stream flowing in the former main stream of the Fujikawa river, abandoned at the time of the Ansei Tokai earthquake, concordantly flows into the present main stream of the Fujikawa river showing that co-seismic uplift did not take place at the west bank. We conclude that <i>Kambara Jishinyama</i> was not tectonically formed by the earthquake, but is a product of the river course change.</p>
著者
高橋 正樹
出版者
東京大学社会科学研究所
雑誌
社会科学研究 (ISSN:03873307)
巻号頁・発行日
vol.54, no.4, pp.59-74, 2003
被引用文献数
2

人の意識や行動様式を規定するのは,属性や置かれた環境だけではなく,個々人の出来事の経験とその積み重ねとしての人生経験である.しかし,量的な調査において,ライフヒストリーに代表される質的調査が主導してきたこうした視点を欠きがちであった.本論文では,量的な手法を活かしつつ,この人生経験をとらえる手法としてライフイベント研究をとりあげた.個々の出来事経験はモノのように記憶の中で出し入れされたりするような固定されたものではなく,記憶化される中で変容していく動的な特徴をもつ.自伝的記憶のこうした特徴を,その形成過程にまで視野を広げて実際の調査データを基に考察した.分析において,より影響力の強い出来事経験と出来事経験への感度という視点を提起し,自伝的記憶形成モデルとして,職業・仕事を軸としたモデルと(男性に多い),家族の出来事への配慮を軸としたモデル(女性に多い)をとらえた.

1 0 0 0 OA 図印集

著者
北沢米吉 著
出版者
葉盛堂
巻号頁・発行日
vol.下, 1883

1 0 0 0 OA 図印集

著者
北沢米吉 著
出版者
葉盛堂
巻号頁・発行日
vol.上, 1883