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from the three rivers forms the eastern edge of the plain, which easily shows the declination of the area. The declination is called the Nōbi Tilt (濃尾傾動運動
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The Yōrō Fault is located on the edge of the Nōbi Plains and is the cause of the Yōrō Mountain Range.
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The downstream areas of the three areas are located in Aichi
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running through the central part of the Nōbi Plain was the cause of the
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rivers) and has very fertile soil. It is bordered on the west by the
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Geophysical Data Center / World Data Service (NGDC/WDS),
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to ward off water damage and flourished as a result.
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364:National Geophysical Data Center
359:Significant Earthquake Database
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346:). Accessed November 23, 2007.
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546:Landforms of Aichi Prefecture
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541:Landforms of Gifu Prefecture
489:. You can help Knowledge by
436:. You can help Knowledge by
217:View of the Nōbi Plain from
137:View of the Nōbi Plain from
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208:1586 Tenshō earthquake
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66:area of northwest
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403:35.25°N 136.833°E
344:Rissho University
342:. Soki Yamamoto (
298:Kiso Three Rivers
127:Kiso Three Rivers
109:and the south by
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225:Major cities
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394:136°49′59″E
219:Gifu Castle
139:Mount Ikeda
103:Owari Hills
46:is a large
530:Categories
391:35°15′00″N
327:References
302:Kiso River
238:Ichinomiya
41:Nōbi Heiya
29:Nōbi Plain
23:Relief map
310:Ibi River
162:sea level
117:Geography
292:See also
266:Tsushima
182:plateaus
170:Tsushima
166:Wanouchi
316:Ise Bay
286:Hashima
262:Inazawa
258:Iwakura
250:Inuyama
242:Kasugai
158:wetland
111:Ise Bay
62:to the
321:Nagoya
246:Komaki
234:Nagoya
174:Nagoya
88:Nagara
278:Ōgaki
254:Kōnan
92:Ibuki
78:(the
64:Owari
52:Japan
48:plain
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434:stub
368:NOAA
274:Gifu
198:The
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96:Yōrō
94:and
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56:Mino
35:濃尾平野
27:The
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