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Dames & Moore, 1999 - USDA Forest Service

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were transferred to AutoCAD maps of the Site. Polygons of erosion potential were mapped in the field<br />

based on the observations. The field findings and results of office analyses are presented in Section<br />

4.2.4.3.<br />

3.1.5.4 Mine Subsidence Potential Assessment<br />

Based on a review of underground mine maps for the Holden Mine, the ore body was noted to have been<br />

present within metamorphic bedrock, was nearly vertical in orientation, had a strike in a northwest-<br />

southeast direction, and a width of approximately 80 feet. The ore body was mined by developing a<br />

number of underground openings, or stopes, which are noted on mine maps. The upper limit of the<br />

underground openings are indicated on the mine maps to approach within approximately 50 feet of the<br />

ground surface. The potential for subsidence exists in these areas. The zone of mapped shallow mine<br />

workings is noted to exist in the area noted as Honeymoon Heights (Figure 3.1-7).<br />

The mine subsidence potential assessment evaluat,ion included mapping of the field conditions along the .<br />

mapped strike of the exposed ore body, including the documentation of the following:<br />

Frequency and orientation of bedding, fractures, and joints<br />

Rock type and consistency<br />

Slope angles<br />

Vegetative cover<br />

Presence or absence of surface water drainages<br />

Indications of potential subsidence features<br />

The data were analyzed as described in Section 3.1 1.2. The field findings and results of office analyses<br />

are presented in Section 4.2.5.<br />

3.1.5.5 Existing Riprap Investigation<br />

A visual assessment of the existing riprap was conducted for the sections of Railroad Creek and Copper<br />

Creeks adjacent to the three tailings piles (Figure 3.1-7). During the reconnaissance, the riprap condition<br />

was characterized for each section (as defined in the Erosion Potential subsection above). The<br />

characterization included a reach by reach assessment of the predominant and maximum boulder size,<br />

boulder lithologic color and composition, and weathering characteristics. Boulder types were classified<br />

into six different types on the basis of lithologic composition and weathering condition. In addition,<br />

Schmidt-hammer tests were performed on representative boulder types to assess the relative hardness and<br />

competency of each riprap type. This information was used by <strong>Dames</strong> & <strong>Moore</strong> in estimating the quality<br />

of the riprap for each slope reach. The data collected in the field were utilized to complete an office<br />

analysis of whether the riprap is sufficient to protect the toes of the tailings pile slopes from erosion by<br />

Railroad Creek and Copper Creek. The field findings and results of the office analyses are presented in<br />

Section 4.2.7. .<br />

3.2 TASK 2 - HYDROLOGIC IIWESTIGATION<br />

Referring to Figures 3.2-1 and 3.2-2, the RI hydrologic investigation was designed to provide a<br />

comprehensive database in support of the feasibility study and ecological risk assessment, as well as<br />

G:\wpdru\OO5\rcpon~Uloldcn-2LiU-O~d0~<br />

17693-005-019Uuly 19. <strong>1999</strong>:2:07 PM;DRAFT FINAL RI REPORT

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