The Toreva-Block: A Distinctive Landslide Type
The Toreva-Block: A Distinctive Landslide Type
复制标题
托雷瓦区块：一种独特的滑坡类型
DOI：
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发表时间：
1937
期刊：
影响因子：
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通讯作者：
P. Reiche
中科院分区：
文献类型：
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作者：
P. Reiche
根据亚利桑那州东北部霍皮印第安人保留地的一个指定类型地点，描述并命名了“岩石滑坡”组的一个末端成员。Toreva区块基本上是由一团连续倾斜的层状物质组成，在许多情况下，这些层状物质沿走向的长度超过1000英尺。试图将滑梯与类型所在地的山墙残留物联系起来。简要讨论了科罗拉多高原省其他地区Toreva-blpks的分布和特征。现有的数据表明，更大的滑坡体形成于更新世晚期。
An end member of the "rock-slide" group is described and named from an assigned type locality in the Hopi Indian Reservation of northeastern Arizona. A Toreva-block consists essentially of an unbroken tilted mass of stratified material which in numerous instances measures over 1,000 feet along the strike. Attempt is made to relate the slides to pediment remnants at the type locality. Distribution and character of Toreva-blpcks elsewhere in the Colorado Plateau Province are briefly discussed. Available data suggest the late Pleistocene formation of the larger slides.