庐山东南麓第六阶地基座上，发现了早更新世冰川作用表皮构造。
The glaciated surface structures of the early pleistocene were discovered in the autumn of 1984, on the sixth terrace base which is located at the southeastern piedmont of Lushan.
最后一次冰川作用的漂浮物沉积在最近的其中一个地质时期——更新世，这段时期从180万年前持续到1万年前。
The drift of the last glaciation was deposited during one of the most recent epochs of geologic time, the Pleistocene, which lasted from 1.8 million to 10,000 years ago.
到二十世纪初，科学家们认为，在更新世期间，有四次不同的冰川作用对北美和欧洲产生了影响。
By the early part of the twentieth century, scientists believed that four distinct glaciations had affected North America and Europe during the Pleistocene epoch.
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