Sherman Landslide, Alaska

Sherman Landslide, Alaska
复制标题

DOI:
10.1126/science.154.3757.1639
复制
发表时间:
1966-12
期刊:
影响因子:
56.9
通讯作者:
R. L. Shreve
R. L. Shreve
中科院分区:
综合性期刊1区
文献类型:
--
作者:
R. L. Shreve

文献摘要

被引文献

相似文献

由1964年3月27日的地震引发,3 × 107立方米的岩石下降了600米,然后在科尔多瓦附近的近水平谢尔曼冰川上高速滑动5公里。除了其他大型滑坡的典型特征外,该滑坡还具有许多重要的新特征,这些特征可能是在一层被困和压缩的空气上滑动的。
Triggered by the earthquake of 27 March 1964, 3 x 107 cubic meters of rock fell 600 meters, then slid at high speed 5 kilometers across the nearly level Sherman glacier near Cordova. The landslide has a number of significant new features in addition to those typical of other large landslides that may have slid on a layer of trapped and compressed air.