Translating bumblebee dialect…
The general conclusions set forth in this paper are based on about five days' underground study and mapping of the Twin Lakes Diversion‐Tunnel, which was recently completed to divert water from Lincoln Gulch, on the west slope of the Sawatch Range, to the North Fork of Lake Creek, a tributary of the Arkansas River, on the east slope. The surface geology of the region was studied before the driving of the tunnel by J. W. Vanderwilt and A. H. Koschmann (Geology of the Independence Pass District, Colorado, U.S. Geol. Surv., preliminary report, mimeographed form No. 67484, 1932), and the general correlation of the tunnel‐section with the surface geology is based on the results of this work and consultation with the authors. More details regarding the general geology of the region are given in the report cited and in a report by J. V. Howell (Twin Lakes District of Colorado, Colo. Geol. Surv., Bull. 17, 1919) covering the region east of the Continental Divide.
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