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Dames & Moore, 1999 - USDA Forest Service

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- Soil<br />

Surficial materials at the Site south of Railroad Creek, except for the tailings and waste rock piles, are<br />

primarily either soil or a mixture of soil and man-made fill material. Soil is composed of relatively<br />

loose/sofi fine-grained material originating from weathered local bedrock and organic material. Fill is<br />

composed of local soil plus rock, branches, stumps, and manmade artifacts which have been placed in<br />

..;:conjunction with historic earthworks. Based on the results of borings (Appendix B) and test pit excavations<br />

(Appendices C and E), the thickness of the soil unit varies from less than one foot to approximately 10 feet.<br />

Colluvium<br />

Colluvium is material deposited by gravity. Grain-sizes present in colluvium range from silt and sand<br />

through cobbles and boulders. Colluvial deposits comprise the majority of surficial material in Holden<br />

Village and much of the north bank of Railroad Creek opposite the tailings piles. Based on the borings<br />

(Appendix B) and test pit excavations (Appendices C and E), colluvial deposits appear to underlie the<br />

southern portion of tailings pile 3, as well as beneath Holden Village and the Winston home sites area. The<br />

soil is noted as a mixture of low to moderate density, fine-grained soil with angular rock. The thickness of<br />

the colluvium may be in excess of 20 to 30 feet in isolated locations.<br />

Alluvium<br />

Alluvium is material moved and deposited by the action of moving water. Material size ranges from silt- to<br />

cobble- and boulder-size, and grains are usually rounded to subrounded. The density of the material<br />

normally ranges from loose to moderately dense. Alluvium (as differentiated from alluvium/reworked till<br />

described later) is limited in extent to areas beneath and adjacent to the current and recent channels of<br />

Railroad Creek.<br />

ail inns Materials<br />

Tailings are fine-grained materials and are the by-product of the milling/processing operation. The tailings<br />

are distributed along the south side of Railroad Creek in tailings piles 1, 2, and 3. The thickness of tailings<br />

pile 1 appears to range from less than 10 feet near the southern edge of the pile to about 60 feet at the TPI-2<br />

location. Tailings materials within the three piles are relatively loose to moderately dense mixtures of silt to<br />

fine sand. The thickness of tailings pile 2 appears to range from 15 feet near the southern edge of the pile to<br />

about 120 feet at the northern edge. The thickness of tailings pile 3 appears to range from 10 feet or less near<br />

the southern boundary of the pile to approximately 70 feet along the northern edge. Tailings thicknesses are<br />

based on boring logs (Appendices C and E) and interpretation of geophysical survey data (Appendix A).<br />

The engineering properties of the materials were investigated by Hart Crowser in 1975, and by <strong>Dames</strong> &<br />

<strong>Moore</strong> for the RI. The grain size of the material ranged from a silt (90 percent passing the No. 200 sieve;<br />

0.075 mm) to a silty fine sand (approximately 40 percent passing the No. 200 sieve). The dry unit density is<br />

approximately 11 0 to 11 5 pounds per cubic foot. The relative density based on the Standard Penetration<br />

Test (SPT) conducted during the drilling and sampling completed by Hart Crowser was "medium dense."<br />

The densities noted in test pits completed by <strong>Dames</strong> & <strong>Moore</strong> were qualitatively determined to range<br />

between "loose" to "moderately compact." The moisture contents ranged from 15 to 30 percent. The shear<br />

G:\WPDATA\OOJ\REPORTSWOLDM-ZW-O.M)(:<br />

17693-005-019Uuly 19.<strong>1999</strong>;4:51 Ph4;DRAFT FINAL RI REPORT<br />

'

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