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Auger with tungsten carbide teeth hydraulic-rotary milltooth or tungsten carbide tricone hydraulic-rotary winch or hydraulics hydraulic hydraulic poor poor to moderate excellent original texture original texture original texture (dry) to slurry (wet) slurry (disturbed sample) nil nil (tungsten) nil to high (tungsten) nil, fines lost (tungsten) excellent, cores bedrock original texture (core can be shortened. lengthened and/or contorted nil (tungsten) From Plouffe (1995). Drilling costs based on 1985 data (Canadian $).

G. Brereton et al. 1988; Saarnisto et al. 1991; Hartikainen & Nurmi 1993; Sibbick & Kerr 1995). In analysis of Au, a minimum of 30 to 50 g of the fine fraction is required because of the particulate nature in which Au occurs coupled with sample inhomogeneity (the 'nugget' effect). Unusually high or low levels of major elements in till also may act as pathfinders because variations can indicate bedrock alteration related to Au mineralization (Hartikainen & Damsten 1991). g. Campbell et al. 1999).

HICOCK, S. R. 1988. Calcareous till facies north of Lake Superior, Ontario: implications for Laurentide ice streaming. Geographie Physique et Quaternaire, 42, 120-135. HIRVAS, H. & NENONEN, K. 1990. Field methods for glacial indicator tracing. In: KUJANSUU, R. & SAARNISTO, M. (eds) Glacial Indicator Tracing. A. Balkema, Rotterdam, 217-248. HOFFMAN, S. J. 1986. Soil sampling. Exploration geochemistry: design and interpretation of soil surveys. Society of Economic Geologists, Reviews in Economic Geology, 3, 39-77.

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