The Lower Gasconade watershed is located in central Missouri and covers an area of approximately 2,154 square miles. The area is predominantly rural, with agriculture being the primary land use. The watershed is characterized by a dendritic drainage pattern, with numerous small tributaries feeding into the mainstem of the Gasconade River. The hydrology of the watershed is influenced by the Ozark Plateau, which is characterized by steep terrain and shallow soils. The area typically receives moderate to high rainfall, with occasional snowfall events in the winter months. Surface water in the watershed is primarily composed of the Gasconade River and its tributaries. The river is an important recreational resource, supporting fishing, boating, and swimming activities. There are several small dams and reservoirs located in the watershed, which are used for flood control and water supply purposes. The reservoirs typically contain high levels of sediment and nutrients, which can contribute to water quality issues downstream. Interesting climatic facts and trends in the area include the occurrence of severe thunderstorms and flash flooding events during the summer months. Additionally, the area has experienced periods of drought in recent years, which has impacted agricultural production and water availability.