Knife River Flint

Abstract

Twenty-four Knife River F I int quarries have been newly discovered in Dunn County, North Dakota. Five were previously known in Mercer County. The flint occurs as pebbles, cobbles, and boulders in alluvial, slope-wash, and colluvial lag deposits of Pleistocene age. The flint in these deposits was originally derived from a silicified lignite bed in the Golden Valley Formation of Eocene age and possibly also from other lignite-bearing formations. The flint has a characteristic petrography and can be readily distinguished from all other commonly used rock types in North Dakota and adjacent areas.

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