A river that flows through eastern Aomori Prefecture. It is 67 kilometers long. It flows out from Nenokuchi on the eastern shore of Lake Towada, flows north and east, and empties into the Pacific Ocean in Oirase Town, Kamikita District. The 14 kilometers from Nenokuchi to Yakeyama, where it joins the Tsuta River, are called the Oirase Stream, and are an important part of Towada-Hachimantai National Park. In the valley, you can see riverside forests of horse chestnut, Japanese walnut, and katsura trees, and as you move away from the stream, you will see a mixture of beech forest species such as beech, magnolia, and Japanese chromosome. On the sandbanks of the riverside that are strongly influenced by the flowing water and at the confluence, keyama alder forests, dow forests, and Onoe willow forests have developed. The stream has a variety of flows, including waterfalls along the way, and is particularly spectacular in the seasons of new greenery and autumn leaves. Tourist buses run along the route, and there is also a walking trail. From Yakeyama, the river flows eastward, carving out the Sanbongi Plateau. In 1855 (Ansei 2), a samurai of the Nanbu clan, Nitobe Tsuto (Inazo's grandfather), began developing the barren land of Sanbongihara. After difficult construction, he succeeded in drawing water from the Oirase River into the river in 1859, which marked the start of rice paddy development on the plateau. [Hiroshi Yokoyama] [References] |It stretches from Nenokuchi on the eastern end of Lake Towada to Yakeyama. The continuous flow of waterfalls and strangely shaped rocks, combined with the surrounding trees that change with the seasons, create a magnificent valley of beauty. Nationally designated special scenic spot Nationally designated natural monument Towada City, Aomori Prefecture © Aomori Prefecture "> Oirase Gorge Source: Shogakukan Encyclopedia Nipponica About Encyclopedia Nipponica Information | Legend |
青森県東部を流れる川。延長67キロメートル。十和田湖の東岸子ノ口(ねのくち)から流出し、北流、東流して上北(かみきた)郡おいらせ町で太平洋に注ぐ。子ノ口から蔦(つた)川との合流点の焼山(やけやま)までの14キロメートルを奥入瀬渓流とよび、十和田八幡平(はちまんたい)国立公園の重要な要素の一つとなっている。渓谷にはトチノキ、サワグルミ、カツラなどの河畔林がみられ、渓流から離れるにつれブナ、ホオノキ、オオバクロモジなどブナ林の構成種が混生する。流水による影響を強く受ける河畔の中州や合流地点にはケヤマハンノキ林、ドウノキ林、オノエヤナギ林が発達している。渓流は途中に滝をつくるなど流れも変化に富み、とくに新緑、紅葉の季節は圧巻である。観光バスが通じるほか、遊歩道も完備している。焼山からは三本木台地を刻みながら東流するが、1855年(安政2)南部藩士新渡戸伝(にとべつとう)(稲造の祖父)は、不毛の地である三本木原開拓に着手した。難工事のすえ、1859年に奥入瀬川の水を引き入れることに成功し、これが台地の水田化の契機となった。 [横山 弘] [参照項目] |十和田湖東端の子ノ口から焼山まで続く。滝や奇岩が連続する流れは、季節により変化を見せる周囲の木々と相まって、みごとな渓谷美をつくり出す。国指定特別名勝 国指定天然記念物 青森県十和田市©青森県"> 奥入瀬渓流 出典 小学館 日本大百科全書(ニッポニカ)日本大百科全書(ニッポニカ)について 情報 | 凡例 |
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