Alps, | portions |a t Green River |Anoplotherium,
Carpathians| of the |m s _Zeuglodon group |and other
N. Africa | Himalaya,|a cetoides_ |forms
Asia Minor| and | |presenting a
Western | frontiers|p |resemblance to
Thibet. | of China.|e |the fauna of
| |r |that period in
| |i |Europe.
| |o |
| |d |
| | |
| | |
| | |
| | |
| | Wahsatch |
| | |
| | |
| | |
| | _Coryphodon_ |
| | _Eohippus_ |
| | |
| | |
| | |
| | |
| | |
| | |
| | |
| | Laramic or Lignitic Period.|
------------------------------------------------------------------------
We learn, both from the nature of these deposits and from their organic
contents, that climatic oscillations have been passing during the whole
period of their deposition over the surface of the globe, and inducing
corresponding fluctuations in the character of the vegetable and animal
life abounding on it. A complete collation of these varying conditions at
synchronous periods remains to be achieved, but the study of our own
country, and those adjacent to it, shows that alternations of tropical,
boreal, and temperate climate have occurred in it; a remarkable series of
conditions which has only lately been thoroughly and satisfactorily
accounted for.
Public-domain text, read in full here on John Shaqi.
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