せんじょうち
扇状地
1. alluvial fan or delta
2. Alluvial fanAn alluvial fan is a fan-shaped deposit formed where a fast flowing stream flattens, slows, and spreads typically at the exit of a canyon onto a flatter plain. A convergence of neighboring alluvial fans into a single apron of deposits against a slope is called a bajada, or compound alluvial fan.
Read “Alluvial fan” on English Wikipedia
Read “扇状地” on Japanese Wikipedia
Read “Alluvial fan” on DBpedia
Read “Alluvial fan” on English Wikipedia
Read “扇状地” on Japanese Wikipedia
Read “Alluvial fan” on DBpedia
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