The area of the East Anglia region is an extension of the cuesta, but it is made up of the East Anglia region, which has been eroded by glacial ice and formed into undulating landforms, and the Fenland region, which is an alluvial plain along the Wash and covered with peat and silt. *Some of the terminology used to refer to the "Eastern Plains of England" is listed below. Source | Heibonsha World Encyclopedia 2nd Edition | Information |
…そのうちチルターン丘陵,ウィールド丘陵などの石灰岩や白亜層の部分は急斜面を,ロンドン盆地やテムズ川上流地域などの粘土質の部分は河谷を形成し,典型的なケスタ地形の発達をみる。(10)イングランド東部平野 ケスタ地帯の延長部ではあるが,氷食を受けて波状地となったイースト・アングリア地域と,ウォッシュ湾岸の沖積平野で泥炭(ピート)とシルトでおおわれるフェンランド地域からなる。 ※「イングランド東部平野」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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