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单词 Lateral moraine
释义

Lateral moraine

原声例句
Geologic | 地理地质类科普

And where two glaciers join, their lateral moraines merge to form a medial moraine.

在两条冰川汇合处,它们的外侧 冰碛合并形成内侧冰碛。

优山美地

The right lateral moraine was disturbed by a large tributary glacier that occupied the basin of Cascade Creek, causing considerable complication in its structure.

右侧冰碛被占据喀斯喀特溪盆地的大型支流冰川扰动, 导致其结构相当复杂。

加州的群山(上)

A beautiful variety of the bench-top lakes occurs just where the great lateral moraines of the main glaciers have been shoved forward in outswelling concentric rings by small residual tributary glaciers.

就在主要冰川的巨大侧冰碛被小的残留支流冰川向前推成膨胀的同心环的地方,出现了各种各样的台顶湖泊。

加州的群山(上)

Moraine Lake furnishes an equally interesting example of a basin formed wholly, or in part, by a terminal moraine dam curved across the path of a stream between two lateral moraines.

冰碛湖提供了一个同样有趣的例子,一个盆地完全或部分由一个终端冰碛坝形成,该坝弯曲穿过两个侧冰碛之间的溪流路径。

加州的群山(上)

The main lateral moraines that bounded the view on either hand are from 100 to nearly 200 feet high, and about as regular as artificial embankments, and covered with a superb growth of Silver Fir and Pine.

左右两侧的主要侧冰碛高度从 100 英尺到近 200 英尺不等, 与人工堤坝一样规则, 上面覆盖着茂密生长的银杉和松树。

中文百科

冰碛 Moraine

(重定向自Lateral moraine)

冰碛,又称冰碛丘陵,是指任何一种冰川消融之后,在表碛内碛中的碛几乎都沉流到冰川的谷底,和底碛、中碛合称为基碛,这些冰碛沉积物随着时间流逝,跟着谷底的地形和强风,逐渐变成高低起伏的大小丘陵,因此称为冰碛丘陵。冰川越大,丘陵就越大,例如:大陆冰川。

英语百科

Moraine 冰碛

(重定向自Lateral moraine)
The red line at the North Sea marks the Dogger Bank, which is most likely a moraine formed in the Pleistocene[1]
Moraine in Rocky Mountain National Park, taken by Ansel Adams in 1941
Lateral moraines of a retreating glacier in Engadin
Lateral moraines above Lake Louise, Alberta, Canada.

A moraine is any glacially formed accumulation of unconsolidated glacial debris (soil and rock) that occurs in currently glaciated and formerly glaciated regions on Earth (i.e. a past glacial maximum), through geomorphological processes. Moraines are formed from debris previously carried along by a glacier and normally consist of somewhat rounded particles ranging in size from large boulders to minute glacial flour. Lateral moraines are formed at the side of the ice flow and terminal moraines at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines, till-covered areas with irregular topography, and medial moraines which are formed where two glaciers meet.

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更新时间:2025/6/22 21:21:00