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Interpretation of the results from extensive regional reconnaissance studies of the geology, stratigraphy, and geochemistry of the Chandler Lake quadrangle, northern Brooks Range, Alaska, and site-specific evaluations of mineralized areas conducted by the U.S. Bureau of Mines indicate that the mineral potential of the Chandler Lake quadrangle is low. There is no surface or geophysical expression indicating the presence of plutons and there is no indication that any of the mineral deposit types associated with plutons are present in the study area. The geologic characteristics and the structural evolution of the sedimentary basins suggests that rocks in the quadrangle are permissive for several mineral deposit types; however, detailed geochemieal sampling and lead-isotopic evaluation of permissive areas where geochemieal anomalies were found indicate that the probability of the presence of undiscovered mineral resources in the Chandler Lake quadrangle is low.

Maps showing mineral resource assessment of the Chandler Lake Quadrangle, Alaska