Mud Creek (Middle Fork Salt River)
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Mud Creek (Middle Fork Salt River)
Mud Creek is a stream in the Randolph and Monroe counties of north central Missouri. It is a tributary of Middle Fork Salt River. The stream headwaters are in Northeast Randolph County just northeast of Cairo and U. S. Route 63. The stream flows northeast then turns southeast as it passes Levicks Mill. The stream turns east as it enters Monroe County just to the northwest of Ash. The stream meanders eastward passing under Missouri Route 151 reaching its confluence with the Middle Fork of the Salt River about three miles northwest of Holiday. The stream source is at and the confluence In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); o ... is at . Mud Creek was so named on account of muddy banks. See also * List of rivers of Missouri References Rivers of Monroe County, Miss ...
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Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes th ...
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