著者
中田 正夫 奥野 淳一
出版者
日本地形学連合
雑誌
地形 = Transactions, Japanese Geomorphological Union (ISSN:03891755)
巻号頁・発行日
vol.32, no.3, pp.327-331, 2011-07-25
参考文献数
4
被引用文献数
1

During the growth of an ice sheet the continental crust beneath and near the ice sheet subsides, while in the decay period of glacier ice the crust is unloaded and rebounds. The process is called glacio-isostasy. The volume of sea water decreases during ice growth, while it increases during ice decay. The changing water load causes the vertical movement of the oceanic crust. The process is referred to as hydro-isostasy. These two processes combined are involved in glacio-hydro isostasy, i.e., the Earth's response to changes in ice and water loading during glacial cycle. The outline of a model for glacio-hydro isostasy is described and an application of the model to the northwestern Kyushu area is briefly introduced.

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地球表面は意外とぐにゃぐにゃなのよね。なので海水面が変化すると列島各地の標高もぐにゃぐにゃ曲がるよ。いわゆる「縄文海進」のときも日本列島で均一に海水面が上がったわけじゃなくて。>RT|CiNii 論文 -  グレイシオハイドロアイ… https://t.co/2GInC2IHHg
こんな論文どうですか? グレイシオハイドロアイソスタシー(用語解説)(中田 正夫ほか),2011 http://t.co/tZoVhPmFZP
おもしろいでしょ。九州、特に長崎あたりの図はここ(pdf http://t.co/WbnZiA4T3a) RT @rukiakagoshima: ハイドロアイソスタシー 図解はこれがわかりやすいかな。 http://t.co/U4kJ4xUZ2O

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