Revised Text book of Geology

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The great lakes of the Eocene were in what is now the summit region of the Rocky Mountains. One of them (U, on the map) lies south of the Uinta Moun- 388 HISTORICAL GEOLOGY.
tains, between the Wasatch and the Front Ranges of Colo- rado ; another, still larger (W, on the map), lies north of the Uinta Mountains. In the later Tertiary, the lakes of the summit region were drained, and great lakes were formed west, and especially- east, of that region. The situation of these lakes indicates that the
... Rocky Mountain region in general was much less elevated at the beginning of the Tertiary than at present.
ROCKS: KINDS AND DISTRIBUTION.
The marine and lacustrine formations are independent in their fossils, and are nowhere interstratified. More- over, as geographical diversity of faunas has increased through all geological time, the fossils of the Atlantic and Pacific Borders are almost wholly of different species. It is therefore impossible to make any exact correlation of the formations of the different regions.


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