陆架冰崩解向海洋输送的冰山对全球海平面升高有一定的影响。
Iceberg transferred from shelf ice collapse to ocean gives a certain impact on global sea level raising.
东海陆架冰后期潮流沙脊以不对称横剖面为特征，陡坡倾向SW。
The cross-section of tidal sand ridges is asymmetric with a steep slope inclining to the SW.
现在的研究表明，在最后一次冰河时期的尾声阶段，阿拉斯加东南部沿岸的内大陆架的相当大的区域并未被冰覆盖。
Research now indicates that sizable areas of southeastern Alaska along the inner continental shelf were not covered by ice toward the end of the last Ice Age.
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