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179:(river terraces) are found on the plateau. One is formed by the flow of the Tama River on the south side. The lowest terrace (low surface) is the Tachikawa terrace, and the terrace one step higher than that (high surface) is the Musashino terrace. The other is in the north and is thought to be a remnant of the former Tama River channel.
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thick. The loam is primarily andesite or basaltic sandy mud formed from volcanic ash that the wind carried west from
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202:[Exhibit explanation "Three-dimensional topographic model of Musashino Plateau" (Earth Room)].
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The Tama River carved the
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formed by the ancient Tama River, covered by a layer of
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This article about a regional geological feature is a
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41:Musashino Plateau and riverbank lowlands of the
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16:Large tableland in Kantō region, Japan
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295:Landforms of Saitama Prefecture
208:(in Japanese). November 5, 2020
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243:. You can help Knowledge by
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136:The plateau is part of the
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205:Tamarokuto Science Center
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92:that sits between the
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82:Musashino Platform
305:Tables (landform)
300:Plateaus of Japan
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210:. Retrieved
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284:Categories
183:References
170:Mount Fuji
148:. Much of
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132:Location
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94:Arakawa
43:Arakawa
212:May 8,
166:meters
156:Origin
112:. The
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150:Tokyo
110:Japan
67:武蔵野台地
29:武蔵野台地
19:Place
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98:Tama
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