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and mine waste dumps have been further identified in the area. <br /> Surface geologic mapping, supported by an evaluation of aerial <br /> photographs available for the site, was performed so that individual <br /> geotechnical units could be delineated and characterized for the purpose <br /> of this study. The geotechnical mapping performed within this study was <br /> also used to provide data on the general stability of the area. <br /> The results of geotechnical mapping are shown on Plate 2, Geo- <br /> technical Map. In this map, the area of interest was divided into several <br /> geotechnical units that are important for the scope of work. Following <br /> is a brief description of these geotechnical units: <br /> Man-made fills cover a considerable area on the southern part <br /> of the property where most of the mine surface facilities are located. <br /> They appear to be spread over most of the alluvial valley of Ralston <br /> Creek; minor fills have been constructed along the road on the northern <br /> end of the property. Fills consist predominantly of cobbles and gravels. <br /> Waste piles are located in the northern part of the property, <br /> on both sides of Ralston Creek. For the purpose of this report, they <br /> are called East and West piles. <br /> Alluvial sediments of Ralston Creek occur along the creek <br /> within the entire area covered by this study. The width of alluvial <br /> deoosits is limited on the northern end of the property and increases <br /> toward the south. The maximum width of the alluvial sediments is ap- <br /> parently at the location of the mine and other surface facilities, <br /> although the alluvium is obstructed by the cover of the man-made fills. <br /> Alluvial sediments are also covered by both waste piles; an attempt <br /> was made to indicate the original alluvial boundaries on the geotechni- <br /> cal map. The alluvial deposits consist predominantly of cobbles and <br /> gravels with some sand. The color of the sediments is medium brown. <br /> Alluvial soils are frequently well-sorted , forming lenses of similar <br /> - 7 - <br />