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<br />fll\ ,1 ;) <br />We have also reviewed the routing provided us of a Probable Maximum Flood <br />through the proposed reservoir. This flood had an estimated peak inflow of 497,000 <br />cfs and a 10 day volume of slightly over 2,000,000 af. Using both spillways during <br />passage-of the Probable Mmdmum Flood volume of over 2,000,000 ai, the reservoir <br />operation would result in a reservoir level above Elev. 4428.5 for only slightly over 7 <br />days. Analogously, for a Once in 1000 Years Flood of about 1,000,000 af, reservoir <br />levels would not be above Elev. 4428.5 for more than about 3 days. This condition is <br />considered to be of basic importance because it determines Elev. 4428.5 as the reason- <br />able ma.'l:imwn design elevation of reservoir water surface for steady seepage conditions, <br />inasmuch as it is our judgment that the rare and very brief incursions of surface flood- <br />ing above that elevation could not possibly saturate the foundation of the long, right abut- <br />ment, non-cutoff reach of the dam, as presently designed with a slurry trench cutoff to <br />Sta. 231, suffiCiently to create steady state seepage conditions exiting at the downstream <br />toe, except possibly at those locations to the right of the slurry trench where the grolID.d <br />surface is below about Elev. 4400. Such locations are limited and would require special <br />study and determination whether seepage exit control is justified. <br />3. Foundation Conditions <br /> <br />a. <br /> <br />Left Abutment and Riverbed. <br /> <br />It is our understanding that this <br /> <br />reach of the dam is underlain at shallow depth by the Pierre Formation (siltstone). <br />Overburden consists of weathered siltstone, aeolian sand, and, in the riverbed, recent <br />sandy alluvium. The feasibility design calls for an excavated cutoff to siltstone under <br />the core zone, and minimal surface stripping elsewhere. It is our impression that the <br />latter requirement should be reviewed, insofar as it seems probable that the river allu- <br />vium should be expected to be at a low relative density, and the weathered Pierre may <br />be thick and appreciably less strong than the compacted embankment fill to be placed <br />on it. Stripping should, in our judgment, be done sufficiently to expose foundation of <br />eqUivalent or superior strength when compared to the embankment fill strength. <br />We concur that the Pierre Formation is low in permeability and would provide a <br />suitable base for the seepage cutoff. We do have some concern about the Pierre as a <br />foundation for the Service Spillway and its Chute and Bucket, and for the River Outlet <br /> <br />10. <br />