[en] The St. Cloud 1:250,000 scale quadrangle of central Minnesota is entirely covered by variable thicknesses of Late Wisconsin age glacial deposits (drift). Precambrian bedrock is primarily exposed within the Mississippi River Valley, but only in very small, scattered outcrops. Approximately 25% of the bedrock is composed of Cretaceous sediments in the southern half of the quadrangle. There are no known uranium deposits (or occurrences) within the quadrangle. One hundred twenty-four (124) groups of uranium samples were defined as anomalies and are discussed. None were considered significant