Bulletin No. 5

Cover Bulletin No. 5
Bulletin No. 5
Washington Geological Survey
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1, 1909, pp. 24-25.
Digitized by Google 72 BtMetin No. 5, Washmgion Geological Survey desitic tuff and both are followed by andesite flows. Further- more, beds of Miocene age have been reported from many of the larger valleys of British Columbia (a) while beds of Eocene age are absent and Pliocene lakes if reported are unknown to the present writer.
Since Miocene lake deposits are known at various places in the boundary country, while beds assigned to other divisions of the Tertiary are not com
...mon, if occurring at all, and since the analogy with the Republic deposits is so close, it would seem reasonable, even in the absence of fossils, to consider the lake beds at Oroville as Miocene.
ANDBSITB.
Distribution.
Three areas of andesite occur in the Oroville-Nighthawk dis- trict. The largest comprises about one and one-half square miles and is plastered against the steep slope west of Oroville.
The next in importance forms the capping of Kruger mountain, while the third appears in the valley wall west of Lake Osoyoos.


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