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In summer, rainfall is heavy due to the rainy season front caused by monsoon, and typhoons are often seen. Thunderclouds that form in the northern to western mountains areas before noon reach the plains in the early afternoon, often resulting in evening showers (thunderstorms). In years when
Okhotsk
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due to clear skies and north winds, so the minimum temperature before sunrise can drop to about 5 degrees below zero in winter. Even on days when the temperature drops at dawn, the daytime temperature rises to about 7 to 10 degrees
Celsius on sunny days, and on days with strong dry north winds, the
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The climate of the Kanto Plain is temperate, with a
Pacific Ocean side climate. Winters are cold and summers are hot. The further inland, the greater the temperature difference between summer and winter, and within a day. There are relatively many hours of sunshine, especially in the northern part.
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makes it difficult to find active faults that can cause earthquakes (faults exist in the base 3000m below the sedimentary layers). In addition, natural sediments such as sediment carried by rivers have been used to create land, and the terrain was almost the same as it is today in the
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tends to get hotter because of being inland, foehn phenomenon, which occurs when the wind in the sky above blows down after crossing the mountains on the north and west sides of the Kanto Plain, and the sea breeze that warms up while passing through central Tokyo.
352:. Of these, the Tone River encompasses a large area of floodplain, for its drainage area of 16,840 km (6,500 sq mi) is the largest in Japan. The drainage areas covered by these rivers account for the alluvial lowland of the Kantō Plain.
425:, typically, undulating between 100 and 200 m above sea level. Hills located at the western edge of the Kantō Plain, the Hiki Hills, Koma Hills, Kusahana Hills, and Kaji Hills, also reach approximately 200 m (660 ft) above sea level.
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is blocked by the Mikuni
Mountains, and the moisture falls as snow along the mountains to the north, and the monsoon that has lost its moisture blows through the Kanto Plain as a strong gale carrying dry air (such as Akagi Orosi in
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The overall tilt of the plateaus and hills is noteworthy. In general, the whole area is slightly bent and forming a basin centered in the Tone River and Tokyo Bay. The ongoing process of
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anticyclone prevails, the winds from this anticyclone become northeasterly winds, and temperatures do not rise due to the cool air brought in by the Yamase, resulting in a cold summer.
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Plateaus. These large plateaus are divided into smaller ones by shallow river valleys. A common feature of the plateaus is that their surfaces are covered with a thick layer of
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sensory temperature is lower than the actual temperature. The lowest temperatures in central Tokyo are higher than those in surrounding areas due to the heat island effect.
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and
Futaara Orosi). Snowfall has been decreasing year by year, but snow accumulation of around 10–20 cm is recorded several times during the winter.
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define the eastern end of the plain. Most of its rivers originate in the northern or western mountain ranges and flow east or southeast into the
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Among the plateaus, the
Musashino Plateau has the largest stretch of land, extending from the western edge of
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Rivers. Its elevation gradually declines from west to east, measuring 190 m at Ōme and 20 m at
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Throughout the year, the entire Kanto Plain, especially the inland areas, are easily affected by
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are thought to exist in the central part of the plain, but this thick accumulation of soft
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Kanto Plain was formed by the Kanto basin-forming movement, which has continued since the
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A collection of plateaus constitute a large part of the plain. Among them are the Ōmiya,
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strata and rise higher than surrounding plateaus, exemplified by the Sayama Hills and
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to the southwest, are thought to have been deposited on these plateaus.
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of volcanic origin. Volcanic ash from surrounding volcanoes, Mounts
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extension continues as the plain's central region gradually sinks.
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The Kantō Plain witnessed its greatest devastation from an
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549:Encyclopedia of Japan Tokyo, Kōdansha
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97:adding citations to reliable sources
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579:. The Jim Pattison Group. pp.
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417:Hills in the Kantō Plain stand on
276:The northern limit borders on the
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626:Landforms of Kanagawa Prefecture
561:Nihon Daihyakka Jiten, Shōgakkan
492:In winter, the monsoon from the
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27:Plain in the Kantō region, Japan
646:Landforms of Ibaraki Prefecture
641:Landforms of Tochigi Prefecture
621:Landforms of Saitama Prefecture
537:Encyclopedia of Japan, Kōdansha
340:; and in the southern part the
84:needs additional citations for
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437:earthquake on 1 September 1923
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636:Landforms of Gunma Prefecture
631:Landforms of Chiba Prefecture
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472:(more than 3,000 years ago).
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575:Guinness World Records 2014
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183:Aerial view of Kantō Plain
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387:to the north and Mounts
191:Map of the Kantō Plain.
175:Geofeatures map of Kantō
30:Not to be confused with
571:Glenday, Craig (2013).
402:to the eastern edge of
304:. The Kashima Sea and
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282:Yamizo Mountain Range
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457:Median Tectonic Line
286:Kantō Mountain Range
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93:improve this article
503:Ibaraki Prefecuture
501:, Tsukuba Orosi in
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616:Landforms of Tokyo
461:sedimentary layers
266:Ibaraki Prefecture
262:Tochigi Prefecture
246:Saitama Prefecture
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55:36.000°N 140.000°E
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108:"Kantō Plain"
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91:Please help
86:verification
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453:Fossa Magna
294:Miura Hills
228:of central
218:Kantō heiya
201:Kantō Plain
58: /
18:Kantō plain
605:Categories
522:References
466:Late Jomon
423:Tama Hills
346:Tama River
338:Kuji River
334:Naka River
330:Kinu River
322:Tone River
318:Sagami Bay
302:Sagami Bay
149:March 2022
119:newspapers
468:to Early
357:Musashino
314:Tokyo Bay
298:Tokyo Bay
272:Geography
224:, in the
193:Tokyo Bay
515:Kumagaya
455:and the
430:tectonic
419:Tertiary
404:Yamanote
361:Sagamino
205:Japanese
46:140°00′E
476:Climate
443:Geology
408:Arakawa
369:Shimōsa
213:Hepburn
133:scholar
43:36°00′N
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412:Sumida
389:Hakone
383:, and
381:Haruna
367:, and
348:, and
336:, and
300:, and
292:, the
264:, and
230:Honshu
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385:Akagi
377:Asama
316:, or
242:Tokyo
238:Japan
234:plain
140:JSTOR
126:books
585:ISBN
410:and
393:Fuji
391:and
373:loam
365:Jōsō
209:関東平野
199:The
112:news
581:015
400:Ōme
236:in
95:by
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