V.—On Changes of Climate during the Glacial Epoch
It has already been sufficiently insisted that no warm or genial climate has intervened since the close of the Glacial epoch. The climate of Britain is milder now than at any other period subsequent to the re-elevation of our country after the last great submergence; our winters have been gradually...
| Published in: | Geological Magazine |
|---|---|
| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1872
|
| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/s0016756800468275 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800468275 |
| Summary: | It has already been sufficiently insisted that no warm or genial climate has intervened since the close of the Glacial epoch. The climate of Britain is milder now than at any other period subsequent to the re-elevation of our country after the last great submergence; our winters have been gradually growing less intense; Britain has slowly passed from an Arctic to a temperate condition of things. Mr. Dawkins accounts for the absence of the mammal-bearing drifts in Scotland and the upland districts of England by supposing that in post-glacial times all these regions were covered with snow and ice. This, however, is a rather exaggerated picture of post-glacial Britain. It is quite true that after the emergence of our country from the last great subsidence, a few local glaciers continued to linger on among our mountain valleys. |
|---|