Onuma Quasi-National Park

Japanese: 大沼国定公園 - おおぬまこくていこうえん
Onuma Quasi-National Park

This quasi-national park is located in the southwest of Hokkaido, in the southern part of the Oshima Peninsula. It was designated in 1958 (Showa 33). Its area is 90.83 square kilometers. It consists of the active volcano Mount Komagatake (1,131 meters) and the Onuma, Konuma, and Junsainuma swamps at its southern foot. Made of andesite, Mount Komagatake was a stratovolcano similar to Mount Fuji, but repeated eruptions have changed the mountain's shape since about 10,000 years ago. The summit has collapsed, leaving a large U-shaped crater to the east. Near the summit, there are alpine plants such as rock lilies and Polygonum salicina, and on the middle slopes and below, there are many broad-leaved trees such as mountain willow, poplar, white birch, and Mizunara oak. Lake Onuma, Lake Konuma, and Lake Junsai were formed when mudflow from Mt. Komagatake dammed up the Orito River. They are home to smelt and carp, and produce water shield. The lake has a complex shoreline, with 126 small islands scattered throughout. There are walking trails, and the lake is a popular spot for strolling along the lake, boating, hiking, camping, and skating throughout the year.

[Hideyoshi Segawa]

[References] | Konuma | Mt. Komagatake
Mount Komagatake and Lake Onuma
Mount Komagatake, also known as Oshima Fuji, and Lake Onuma, formed by the damming of its ejecta. This area, rich in nature, is designated as the Onuma Quasi-National Park. There are ski resorts and campsites in the surrounding area, and many people visit throughout the year. Hokkaido Kameda-gun Nanae-cho, Kayabe-gun Shikabe-cho, Mori-cho © Hakodate City Yunokawa Onsen Ryokan Association Hakodate International Tourism and Convention Association

Mount Komagatake and Lake Onuma


Source: Shogakukan Encyclopedia Nipponica About Encyclopedia Nipponica Information | Legend

Japanese:

北海道南西部、渡島(おしま)半島南部にある国定公園。1958年(昭和33)の指定。面積90.83平方キロメートル。活火山の駒ヶ岳(こまがたけ)(1131メートル)とその南麓(なんろく)の大沼、小沼、蓴菜沼(じゅんさいぬま)からなる。安山岩からなる駒ヶ岳は富士山型の成層火山であったが、約1万年前から噴火を繰り返して山体を変えた。山頂部は崩壊し、東に開いたU字形の大火口がある。山頂付近にはイワブクロ、ウラジロタデなどの高山植物、中腹以下にはミネヤナギ、ドロノキ、シラカバ、ミズナラなどの広葉樹が多い。大沼、小沼、蓴菜沼は駒ヶ岳の泥流が折戸(おりと)川をせき止めてできた湖沼で、ワカサギやコイが生息し、ジュンサイを産す。湖岸線は複雑で、湖沼中には126の小島が点在する。遊歩道なども整備され、湖畔散策、ボート遊び、登山、キャンプ、スケートなど四季を通じてにぎわう。

[瀬川秀良]

[参照項目] | 小沼 | 駒ヶ岳
駒ヶ岳と大沼
渡島富士ともよばれる駒ヶ岳と、その噴出物によってせき止められてできた大沼。豊かな自然が広がるこの一帯は大沼国定公園に指定されている。周辺にはスキー場やキャンプ場などの施設もあり、一年を通して多くの人が訪れる。北海道亀田郡七飯町・茅部郡鹿部町・森町©函館市 湯の川温泉旅館協同組合 社団法人函館国際観光コンベンション協会">

駒ヶ岳と大沼


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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