Geology volume 3

Cover Geology volume 3
Geology volume 3
Thomas C Thomas Chrowder Chamberlin
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214-218, Vol. I), and more considerable deposits of the latter material antedate the present by some considerable interval of time. Many of these deposits probably fall within the limits of the Pleistocene period. Their distribution seems to indicate that the sites of deposition have become successively lower and lower, as the valleys have been deepened, the springs taking advantage of suc- cessively lower avenues of escape. Tufaceous deposits of the same type are known at various other points ...in the western mountains. 1 Salisbury, Jour, of Geol. , Vol. IX, p. 730.
476 GEOLOGY.
Marine deposits. Along the western coast of the United States there are marine deposits reaching inland some distance from the FIG. 558. A sink-hole of recent development near Meade, Kan. (Johnson, U. S. Geol. Surv. ) coast. They are known to extend up to altitudes of 200 or 300 feet in California 1 and Oregon, and perhaps even higher. The Pleistocene submergence indicated by the disposition of these beds must have ' >-'u - ' " ' - ''" '"' Tt V i i, ^ erIL ";'?T i " -eioCne But FIG.


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