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190:(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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213:[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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27:Large tableland in Kantō region, Japan
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306:Landforms of Saitama Prefecture
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254:. You can help Knowledge by
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147:The plateau is part of the
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157:Saitama Prefecture
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316:Tables (landform)
311:Plateaus of Japan
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16:(Redirected from
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295:Categories
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181:Mount Fuji
159:. Much of
153:Tokyo Bay
101:tableland
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143:Location
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105:Arakawa
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223:May 8,
177:meters
167:Origin
123:. The
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161:Tokyo
121:Japan
78:武蔵野台地
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225:2024
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