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Dames & Moore, 1999 - USDA Forest Service

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4.2.8 Potential Borrow Source Areas<br />

Remedial strategies may require methods to improve protection From wind and stream erosion processes,<br />

and mass inovement hazards. For example, riprap may need to be placed in specific areas due to river<br />

rerouting, places where it is now absent but required (e.g., slope reach 1-A), or supplemented in river<br />

reaches with present low quality riprap (see Section 4.2.7, Existing Railroad Creek Riprap). In addition,<br />

remedial work (e.g., revegetation, recontouring, etc.) of tailings may require a local soil cover source. A<br />

preliminary assessment of potential borrow source areas was conducted to achieve the following objectives:<br />

4.2.8.1 Sand and Gravel<br />

Identify potential accessible sources of riprap within the Railroad Creek drainage basin<br />

Identify potential accessible sources of soil cover within the Railroad Creek drainage basin<br />

Summary of Historical Findings<br />

The gravel currently covering the tailings piles was placed during the 1991 site reclamation efforts. The<br />

gravel reportedly originated from a gravel pit developed at "Dan's Camp" (Figure 4.2-23). Other than the<br />

"Dan's Camp" pit utilized by the USFS previously, no onsite sources of granular borrow material were<br />

identified during the review of historical information,<br />

RI Findings<br />

A borrow source evaluation to identify potential sources of sand and gravel was conducted as part of the RI.<br />

The scope of work included the initial review of geologic maps and aerial photographs for the Railroad<br />

Creek watershed from the Glacier Peak Wilderness boundary down to Lucerne. The objective of the<br />

assessment was to identify a source or sources of granular borrow material as close to the Site as possible.<br />

The gravel pit area at Dan's Camp was assessed visually and appears to be a good source of sand and gravel.<br />

The material exposed in the gravel pit was estimated to be a gravelly sand to sandy gravel, with relatively<br />

low percentages of silt. However, this source is approximately seven miles from the Site.<br />

Referring to Figure 4.2-25, on September 30, 1997, six test pits were excavated in two potential source<br />

areas: (1) three pits east of tailings pile 3 (DMTP3E-4 through DMTP3E-6), and (2) three pits along the<br />

slopes south of the' three tailings piles (DMTP I S- I, DMTP2S- 1, AND DMTP3S- 1). A second objective of<br />

the test pits completed south of the tailings piles was to characterize the near-surface groundwater<br />

conditions in the native soil. The test pit logs are presented in Appendix C. Soils in the test pits were<br />

described generally following USCS standards and were evaluated with respect to approximate grain size<br />

distribution (i.e., percent boulders, cobbles, sands, and fines), maximum boulder size, and range of boulder<br />

sizes.<br />

The onsite potential borrow areas may be adequate sources for soil cover, particularly for elements of the<br />

Site which may require siltier soils. For general tailings pile slope cover, some sorting would be necessary<br />

to sifi out the coarse fraction (which may be suitable as a riprap supplement) and the fine fraction (to<br />

prevent wind transport).<br />

G:\WPDATA\OOS\REPORTS\HOLDEN-2W-O.DOC<br />

17693-00Sd19Wuly 19. <strong>1999</strong>;4:51 PM;DRAFr FINAL RI REPORT

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