09391774-n 'a type of glaciation characteristic of Alaska';
Definitions
- English
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a type of glaciation characteristic of Alaska
large valley glaciers meet to form an almost stagnant sheet of ice
- Japanese
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アラスカの一種の氷河作用の特性
ほとんど淀んだ層の氷を形成するために大きな谷氷河が出会う
Relations
External Links
SUMO:
⊂ Glacier
TempoWN:
◁
▲
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(Past: 0.001;
Present: 0.344;
Future: 0.000)
SentiWN:
△
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(+0.00
-0.00)
MLSentiCon:
▲
▽
(+0.12
-0.00)
More detail about the Extended Open Multilingual Wordnet (1.3)
Maintainer:
Francis Bond
<bond@ieee.org>