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SITE INFORMATION PACKAGE FOR NATIONAL REMEDY REVIEW BOARD<br />

PART B, SECTION 1: SITE NAME, LOCATION, AND BRIEF HISTORY<br />

<strong>In<strong>for</strong>mation</strong> <strong>Package</strong>, the FFS Report, and the <strong>for</strong>thcoming ROD Amendment extends<br />

approximately 1 mile to the west beyond the confluence of the SFCDR and the North Fork<br />

of the Coeur d’Alene River. Figure A-2 provides a map of the Upper Basin. The topographic<br />

relief in the Upper Basin ranges from approximately 2,000 to 7,000 feet above mean sea<br />

level.<br />

1.2 Mining History<br />

The Bunker Hill Superfund <strong>Site</strong> has a long history of mining and related metals-processing<br />

activities. Mining and smelting within the Coeur d’Alene Basin began more than 100 years<br />

ago, and the region became one of the leading silver-, lead-, and zinc-producing areas in the<br />

world. The area surrounding the SFCDR produced over 97 percent of the ore mined in the<br />

entire Basin (Science Applications International Corporation [SAIC], 1993). Approximately<br />

1.2 billion ounces (34,000 tons) of silver, 8 million tons of lead, and 3.2 million tons of zinc<br />

were produced (Long, 1998).<br />

The Bureau of Land Management (BLM) of the U.S. Department of the Interior identified<br />

more than 1,000 mining or milling-related features in the region surrounding the SFCDR<br />

(BLM, 1999). Several of the features were metals-processing facilities that were constructed<br />

at various times, including an electrolytic zinc plant, a lead smelter plant, three sulfuric acid<br />

plants , a phosphoric acid plant , and a fertilizer plant.<br />

As a result of past mining, milling, and smelting practices, substantial portions of the Coeur<br />

d’Alene Basin contain elevated concentrations of lead, zinc, cadmium, and other metals.<br />

Within the Upper Basin, elevated concentrations of metals resulted primarily from the<br />

discharge or erosion of mill tailings and other mine-generated waste into rivers and streams.<br />

These water bodies, in turn, deposited millions of tons of mine tailings into streambeds,<br />

floodplains, and shorelines throughout the Upper and Lower Basins. The history of milling<br />

and tailings disposal practices in the Basin is summarized in Table B1-1; some significant<br />

details are summarized below.<br />

• Approximately 62 million tons of tailings were discharged to the Coeur d’Alene Basin<br />

after mining began.<br />

• Tailings were frequently used as fill material <strong>for</strong> residential and commercial<br />

construction projects.<br />

• Until 1968, tailings tended to be discharged directly into the SFCDR or its tributaries.<br />

Most of the tailings were transported downstream, particularly during high-flow events,<br />

and deposited as solid tailings or as tailings/sediment mixtures in beds, banks, and<br />

floodplain areas. Since 1968, all mill tailings have been placed in impoundments or<br />

returned as fill to provide structural support to active mines.<br />

• Mining activities generated large volumes of waste rock and discharged water from<br />

mine openings (adits) that contained high concentrations of metals.<br />

• Particulates released to the air from smelting operations contained high concentrations<br />

of metals. The particulates were transported by the wind and were deposited<br />

throughout the Bunker Hill Box area. (The Bunker Hill “Box” is a 21-square-mile area<br />

surrounding the <strong>for</strong>mer smelter complex.)<br />

B1-2

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