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477:. This volcano became active around 200,000 years ago, and through repeated eruptions and pyroclastic flows, especially 55,000 and 36,000 and 15,000 years ago, created an 11-kilometer-diameter (6.8 mi) caldera with the proto-Lake-Towada. From approximately 15,000 to 12,000 years ago, intermittent eruptions formed a small stratovolcano within this caldera (Mount Goshikiiwa). Intermediate eruptive activity continued, and at least eight eruptions of
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occurred from 11,000 years ago to the present. The
Ogurayama Lava Dome was formed approximately 7,600 years ago on the northeastern slope of the Goshikiiwa volcano. The Mikadoishi Lava Dome is estimated to have emerged between 12,000 and 2,800 years ago. The collapse of these secondary lava domes
704:
65:, is a useful starting point for translations, but translators must revise errors as necessary and confirm that the translation is accurate, rather than simply copy-pasting machine-translated text into the English Knowledge.
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approximately 5400 years ago give the lake its distinct shape, and the inlet between its two peninsulas (called the "Nakaumi") is the remnant of a secondary caldera which erupted and collapsed.
430:. With a surface area of 61.1 km (23.6 sq mi), Towada is Japan's 12th largest lake; its bright blue color is due to its great depth. The lake is roughly circular, with two
546:. The mountain continued to erupt well into the historical period, with the last recorded eruption occurring in 915 AD in the Nakaumi caldera, devastating the surrounding area with
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The lake's symbol, the Otome-no-Zo statue, is located in the central area of
Yasumiya. From there excursion boats arrive and depart. In Utarube, visitors can canoe or camp.
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of the lake covers an area of 129 square kilometers (50 sq mi). The lake area is fed by around seventy rivers, half of which are intermittent. The
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which crashed in 1943 was found at the bottom of Lake Towada on 13 August 2010. It was recovered on 5 September 2012 and has been placed on display.
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Do not translate text that appears unreliable or low-quality. If possible, verify the text with references provided in the foreign-language article.
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According to the
National Institute for Environmental Studies of Japan, the water renewal cycle of Lake Towada is approximately 8.5 years. The
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extending from its southern shore approximately one-third into the center of the lake. The lake is a popular tourist destination.
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was dedicated at the lakeshore as part of the park's 15th anniversary celebration. It was the last work by that sculptor.
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Content in this edit is translated from the existing
Japanese Knowledge article at ]; see its history for attribution.
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In 1953, in order to popularize the lake and the park, a sculpture of two women titled "The Maiden Statue" by
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List of
Special Places of Scenic Beauty, Special Historic Sites and Special Natural Monuments
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The area around Lake Towada remained largely wilderness until towards the end of the
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Lake Towada is located approximately 540 kilometers (340 mi) northeast of
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on the eastern shore of the
Nakayama peninsula in 807 AD dedicated to
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visited Lake Towada during one of his expeditions north to conquer the
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to the source of your translation. A model attribution edit summary is
839:. Bouquins (in French). Paris: Éditions Robert Laffont. p. 1215.
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in 1927. In 1936, the lake and surrounding areas became part of
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1015:"Towada: National catalogue of the active volcanoes in Japan"
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Ministry of Land, Infrastructure, Transport and
Tourism.
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for irrigation. In 1903, largely through the efforts of
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were introduced into Lake Towada. The lake now also has
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and is 327 m (1,073 ft) deep, drained by the
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prefectures, it lies 400 meters (1,800 ft) above
962:"About Lake Towada - Aomori Travel Guide | Planetyze"
728:
938:旧陸軍練習機、十和田湖で発見…戦時中に墜落：社会 : YOMIURI ONLINE（読売新聞）
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The name of the lake is believed to derive from the
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784:. National Institute for Environmental Studies.
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83:accompanying your translation by providing an
49:Click for important translation instructions.
36:expand this article with text translated from
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454:. It forms part of the northern section of
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983:Southerland, Mary and Britton, Dorothy.
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583:of water, as being associated with the
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837:Le Japon: dictionnaire et civilisation
526:According to a legendary account, the
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329:4.19 km (3,400,000 acre⋅ft)
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305:61.1 km (23.6 sq mi)
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871:Towada National Park Association.
814:. Chūōkōron Shinsha. p. 154.
731:"Towada-Hachimantai National Park"
523:, literally meaning "rocky lake".
14:
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987:. Kodansha International (1995).
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606:projects at Sanbongihara (modern
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835:Frédéric, Louis (October 1996).
685:Imperial Japanese Army Air Force
667:Towada-Hachimantai National Park
456:Towada-Hachimantai National Park
414:. Located on the border between
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1455:Special Places of Scenic Beauty
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380:Sightseeing boat on Lake Towada
1450:Volcanoes of Aomori Prefecture
1007:- Japan Meteorological Agency
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93:You may also add the template
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1022:- Japan Meteorological Agency
751:Japan Meteorological Agency.
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653:The lake was selected by the
198:Show map of Aomori Prefecture
16:Caldera lake in Aomori, Japan
1028:- Geological Survey of Japan
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985:The National Parks of Japan
906:Ministry of the Environment
729:National Parks Foundation.
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663:Eight Scenic Views of Japan
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352:not a well-defined measure
345:400 metres (1,312 ft)
321:327 m (1,073 ft)
57:Machine translation, like
1435:Lakes of Akita Prefecture
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810:Umehara, Takeshi (1989).
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538:tribes and built a small
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1038:Global Volcanism Program
1043:Smithsonian Institution
928:Retrieved April 2, 2016
573:, including worship of
337:46 km (29 mi)
313:71 m (233 ft)
104:For more guidance, see
659:Osaka Mainichi Shimbun
602:attempted large-scale
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95:{{Translated|ja|十和田湖}}
1445:Volcanic crater lakes
565:During the Heian and
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106:Knowledge:Translation
77:copyright attribution
1460:Pleistocene calderas
532:Sakanoue Tamuramaro
241: /
1440:Calderas of Honshū
948:2010-08-16 at the
776:Takamura, Noriko.
473:still regarded as
382:
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245:40.467°N 140.867°E
85:interlanguage link
1465:Holocene calderas
1417:
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1298:Mikata Five Lakes
926:September 5, 2012
899:"日本八景(昭和2年)の選定内容"
548:pyroclastic flows
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342:Surface elevation
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1046:. Retrieved
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753:"24. Towada"
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736:November 22,
734:. Retrieved
724:
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640:Japanese eel
612:Oirase River
610:) using the
589:
585:azure dragon
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560:volcanic ash
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496:Oirase River
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428:Oirase river
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334:Shore length
326:Water volume
302:Surface area
281:Oirase River
190:Lake Towada
158:Lake Towada
122:Lake Towada
81:edit summary
72:
45:(April 2013)
43:
35:
1244:Kasumigaura
1235: [
888:, p. 1
594:, when the
404:crater lake
385:Lake Towada
372:Lake Towada
267:Crater lake
248: /
223:Coordinates
40:in Japanese
1424:Categories
1189:Inawashiro
1048:2021-06-24
971:2017-08-15
812:日本人の「あの世」観
716:References
691:Activities
679:A wartime
596:Nambu clan
592:Edo period
432:peninsulas
318:Max. depth
1271:Kawaguchi
966:Planetyze
886:NIES 2001
636:Carassius
571:Yamabushi
512:to watara
486:Hydrology
424:sea level
397:Towada-ko
99:talk page
1306:Suigetsu
1287:Yamanaka
1227:Chūzenji
1151:Shikotsu
1126:Kutcharo
1121:Kussharo
1101:Abashiri
1033:"Towada"
946:Archived
942:Japanese
911:17 March
855:36327575
797:"青森・十和田"
782:NIES2001
699:See also
530:general
438:Location
410:island,
236:140°52′E
208:Location
75:provide
1360:Nakaumi
1314:Kugushi
1249:Kitaura
1199:Ogawara
1179:Hachirō
1131:Kuttara
1111:Akkeshi
761:May 20,
502:History
467:caldera
461:Geology
233:40°28′N
97:to the
79:in the
42:.
1365:Shinji
1318:Hiruga
1302:Mikata
1293:Hamana
1275:Motosu
1209:Towada
1204:Tazawa
1184:Hibara
1161:Utonai
1146:Saroma
1141:Notoro
1026:Towada
1005:Towada
991:
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638:, and
608:Towada
577:, the
575:Suijin
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475:active
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