
Craig serves as the primary hub in this northwestern Missouri landscape, where the flat alluvial plains of the Missouri River valley meet the dissecting bluffs to the east. The drainage patterns are defined by the winding course of Little Tarkio Creek and the remnants of former waterways, including the Old Channel Little Tarkio Creek and Old Channel Tarkio River. These abandoned channels suggest a history of significant hydrological engineering or natural shifting within the floodplain.
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