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Management of Commercially Generated Radioactive Waste - U.S. ...

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3-3 3-4<br />

Comment Comment<br />

Number Number<br />

that this represents a single sample from Pikes Peak (Pirsson, pg. 169) 2. The Keweenawan Series is misplotted as is the Triassic <strong>of</strong> N.J. and<br />

It would have been better to use Tschirwinsky's average <strong>of</strong> 90 analyses Connecticut. This is not surprising as the map <strong>of</strong> the Keweenawan<br />

(Pirsson, pg. 169) which results in a significantly different chemical which was supposedly used in compiling this map (Y/OWI/TM 36/7,<br />

composition for an "average" granite. An alternate source <strong>of</strong> information Figure 3-1) is illegible.<br />

is Clark, S.P., 1966, "Handbook <strong>of</strong> Physical Constants," Geol. Soc. <strong>of</strong><br />

Amer. 3. Reference Y/OWI/TM 36/7 is cited as a source <strong>of</strong> information for the<br />

location <strong>of</strong> the Triassic "Lavas." There is no information on the<br />

3.a.7 p. 3.1.13 Triassic in this publication.<br />

p. 7.2.10, DOE/ET-0028<br />

Figure 3.1.3 does not appear in Reference 10 as indicated in GEIS. Appar- 4. The expression Keweenawan and Triassic "Lavas" is misleading, as many<br />

ently it was adopted from a similar but slightly different diagram in <strong>of</strong> these basalts are not extrusive igneous rocks, e.g., Palisades<br />

Y/OWI/TM 36/3 which was adapted from OWI-76-26 and Tourtelot 1962. The Sill.<br />

orginal references should have been used. The figure's caption implies<br />

that it shows all the shale formations (sic) in the U.S.. However, there 5. Figure 7.2.4 could not have been developed from information found in<br />

are a number <strong>of</strong> significant omissions such as the thick shales found in Y/OWI/TM-44.<br />

the Appalachian foldbelt, the Ouachita Mts., Anadarko Basin, and the<br />

Midland, Marfa, and Delaware Basins <strong>of</strong> West Texas. 3.a.10 p. 3.1.32<br />

The first paragraph does not reflect fissure and joint permeability differ-<br />

3.a.8 p. 3.1.14 ences, and induced characteristics due to construction. The final paragraph<br />

The table is very important since it is a direct numerical comparison <strong>of</strong> makes an assertion that is not supported; i.e., no bases have been provided<br />

major host rock types. Therefore, the selection <strong>of</strong> numerical ratings for to support the conclusion that groundwater inflow can always "...be controlled<br />

each characteristic <strong>of</strong> each rock type should be discussed, by state-<strong>of</strong>-the-art engineering technology."<br />

3.a.9 p. 3.1.14 3.a.11 p. 3.1.67<br />

p. 7.2.13, DOE/ET-0028 The age <strong>of</strong> the earth is given as 10 billion years. The current geologic<br />

Figures 3.1.4 and 7.2.4 are incorrectly referenced, are incorrect and estimate <strong>of</strong> the age is 5 billion years.<br />

misleading:<br />

3.a.12 p. 7.2.2, DOE/ET-0028<br />

1. They fail to show some <strong>of</strong> the other basalt areas which should be The statement that: "The repository should not be sited in or near an<br />

assessed as candidates for deep geological burial <strong>of</strong> HLW, e.g., area in whch igneous or volcanic activity has occurred during the post-<br />

Colorado Plateau, Rio Grande Valley, San Juan Mts. <strong>of</strong> Colorado, Snake Pleistocene" should be assessed and actively discussed by DOE. An assess-<br />

River Plains, Triassic Basins <strong>of</strong> the Carolinas, Virginia and ment should be made <strong>of</strong> the potential for volcanic activity and its impact<br />

Pennsylvania.

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