Evidence of a Further Glacial Episode within the Valley of the Lower Thames
Evidence of a Further Glacial Episode within the Valley of the Lower Thames
复制标题
泰晤士河下游河谷内进一步冰川事件的证据
DOI：
10.1017/s0016756800092463
复制
发表时间：
1935
影响因子：
2.3
通讯作者：
J. Burchell
中科院分区：
文献类型：
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作者：
J. Burchell
在过去的一年中，继续在位于诺斯弗利特和斯旺斯科姆之间的、填充穿过后早期穆斯特（勒瓦利斯期）库姆岩的通道的矿床中进行挖掘。在继承的基础上，“地板”继续产生一系列当代中Mousterian（Levalloisian）工具，以及来自Coombe Rock和早期沉积物的文物。与这些工具相关的还有大象、古犀牛、田鼠、M. anglicus和M.尼瓦利斯
During the past year excavations have been continued in the deposits filling the channel cut through the Coombe Rock of post-Early Mousterian (Levalloisian) age and situated between Northfleet and Swanscombe. “The floor” at the base of the succession has continued to yield a fine series of contemporary Middle Mousterian (Levalloisian) implements, together with artifacts derived from the Coombe Rock and earlier deposits. Associated with the implements are the remains of Elephas primigenius, Rhinoceros antiquitatis, Microtus arvalis, M. anglicus, and M. nivalis.