| Muddy Run | |
| Source1 Location: | near the base of Buffalo Mountain in West Buffalo Township, Union County, Pennsylvania |
| Mouth Location: | Spruce Run in Buffalo Township, Union County, Pennsylvania |
| Mouth Coordinates: | 40.9797°N -76.9838°W |
| Progression: | Spruce Run → Buffalo Creek → West Branch Susquehanna River → Susquehanna River → Chesapeake Bay |
| Length: | 4.8miles |
| Source1 Elevation: | between 780and |
| Mouth Elevation: | 486feet |
| Basin Size: | 4.57sqmi |
Muddy Run is a tributary of Spruce Run in Union County, Pennsylvania, in the United States. It is approximately 4.8miles long and flows through West Buffalo Township and Buffalo Township. The watershed of the stream has an area of 4.57sqmi. Part of the stream is designated as an impaired waterbody due to sedimentation and siltation from grazing-related agriculture. The majority of the watershed is forested, but there is also a considerable amount of agricultural land. A bridge has been constructed over the stream in the community of Mazeppa.
Muddy Run begins near the base of Buffalo Mountain in West Buffalo Township. It flows east-southeast for several tenths of a mile before turning east-northeast and then east-southeast. Several tenths of a mile further downstream, the stream turns south-southeast for a few tenths of a mile before entering Buffalo Township and turning east for a few miles. It then turns southeast for several tenths of a mile before turning northeast. Several hundred feet further downstream, it reaches its confluence with Spruce Run.
Muddy Run joins Spruce Run 0.34miles upstream of its mouth.
A total of 2.6miles of streams in the watershed of Muddy Run are designated as impaired waterbodies. The cause of the impairment is sedimentation/siltation and the source of the impairment is grazing-related agriculture. The total maximum daily load date is 2015. In addition to sediment, Muddy Run is also affected by E. coli, nutrient pollution, and thermal radiation.
In 2000, the load of sediment in Muddy Run was 526669lb, while in 2008 it was 494901lb. This equates to somewhere between 150lb/acre200lb/acre. In the future, the load could be reduced by 50.30 percent to 245956lb per year. In 2000, the nitrogen load in the stream was 37176lb and in 2008, it was 36879lb. This equates to somewhere between 10lb/acre15lb/acre. In the future, the nitrogen load could be reduced by 20.26 percent to 29406lb per year. In 2000 and 2008, the phosphorus load was 1372lb1343lb, respectively. This equates to more than 0.4lb/acre. In the future, the phosphorus load could be reduced by 37.53 percent to 839lb per year.
Of the 526669lb of sediment in Muddy Run in 2000, 247195lb came from row crops and 144298lb came from streambank erosion. Another 32677lb came from hay and pastures, while 11133lb came from unpaved roads. A total of 8838lb came from low-density urban development, while 82528lb came from other sources.
In 2000, the total load of nitrogen in Muddy Run from groundwater was 14221lb. The load from row crops was 1588lb and the load from hay and pastures was 983lb. The nitrogen load from low-density urban development was 85lb, the load from unpaved roads was 45lb, and the load from septic systems was 44lb. A total of 7lb came from streambank erosion and 431lb came from other sources.
In 2000, the total load of phosphorus in Muddy Run from row crops was 250lb and the load from groundwater was 229lb. The load from hay and pastures was 99lb, the load from low-density urban land was 14lb, 7lb came from unpaved roads, and 6lb came from septic systems. Other sources contributed 3lb.
The elevation near the mouth of Muddy Run is 486feet above sea level. The elevation of the stream's source is between 780and above sea level.
A total of 0.2miles of streams in the watershed of Muddy Run are flanked by fences, though this could eventually increase to 4.3miles. Stabilization occurs on only 0.1miles of streams, though this could increase to 9.7miles in the future.
The watershed of Muddy Run has an area of 4.57sqmi. The mouth of the stream is in the United States Geological Survey quadrangle of Lewisburg. However, the source is in the quadrangle of Mifflinburg. The watershed makes up 3 percent of the watershed of Buffalo Creek. There are 9.7miles of streams in the watershed of Muddy Run, of which 4.3miles are in agricultural land.
A total of 57 percent of the watershed of Muddy Run is on forested land. Another 35 percent is on agricultural land, while 3 percent is on impervious surfaces. The amount of land on impervious surfaces could be as high as 26 percent in the future. There is a field lane improvement project on 1625feet of Muddy Run. A total of 227acres of agricultural land in the watershed is on slopes of more than 3 percent. There are 1.2miles of unpaved roads in the stream's watershed.
A total of 2.4miles of streams in the watershed of Muddy Run have riparian buffering, but this could increase to as much as 4.3miles in the future.
Muddy Run was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1182059. While some deeds reference Muddy Run as the name, the original name was Armstrong Run, as depicted on an official survey map of Union County dated 1874. Armstrong Run is also the name referenced in the landowners and residents map published in 1868 by Pomeroy and Beers of Philadelphia.
A concrete stringer/multi-beam or girder bridge carrying State Route 1001 was constructed over Muddy Run in Mazeppa in 1932. It is 24feet long.