…The topography that forms the backbone of the country is the old and new sedimentary topography of the Rhine and Meuse rivers that run through the Netherlands from east to west and north, and the broad central part is the Rhine delta, which is made up of fluvial clay. As the Rhine flows into the Netherlands, it splits into the Waal and the Nederrijn, the latter of which branches off into the IJssel to the east of Arnhem, and further downstream it is called the Lek. The IJssel flows north and empties into Lake IJssel. … *Some of the terminology that mentions the "Eysel River" is listed below. Source | Heibonsha World Encyclopedia 2nd Edition | Information |
…国土の骨格を形づくる地形は,オランダを東から西,北へ貫流するライン川,マース(ムーズ)川の新旧の堆積地形であり,その広い中央部はライン川の三角州で河成粘土からなる。ライン川はオランダに流入するとワールWaal川とネーデルライン川に分かれ,後者はアルンヘムの東方でエイセルIJssel川を分流し,さらに下流はレックLek川と呼ばれる。エイセル川は北流してアイセル(エイセル)湖に注ぐ。… ※「エイセル[川]」について言及している用語解説の一部を掲載しています。 出典|株式会社平凡社世界大百科事典 第2版について | 情報 |
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