Miry Hole Branch Tributary to Trent River | |
---|---|
Location of Miry Hole Branch mouth Miry Hole Branch (the United States) | |
Location | |
Country | United States |
State | North Carolina |
County | Jones |
Physical characteristics | |
Source | Reedy Branch divide |
• location | about 2 miles south of Trent Woods, North Carolina |
• coordinates | 35°03′19″N 077°07′31″W / 35.05528°N 77.12528°W[1] |
• elevation | 15 ft (4.6 m)[2] |
Mouth | Trent River |
• location | about 0.5 miles east of River Bend, North Carolina |
• coordinates | 35°03′43″N 077°08′20″W / 35.06194°N 77.13889°W[1] |
• elevation | 0 ft (0 m)[3] |
Length | 0.91 mi (1.46 km)[4] |
Basin size | 1.44 square miles (3.7 km2)[5] |
Discharge | |
• location | Trent River |
• average | 2.29 cu ft/s (0.065 m3/s) at mouth with Trent River[5] |
Basin features | |
Progression | Trent River → Neuse River → Pamlico Sound → Atlantic Ocean |
River system | Neuse River |
Tributaries | |
• left | unnamed tributaries |
• right | unnamed tributaries |
Bridges | Crump Farm Road |
Miry Hole Branch is a 0.92 mi (1.48 km) long 1st order tributary to the Trent River in Jones County, North Carolina. This is the only stream of this name in the United States.[1]
Course
Miry Hole Branch rises about 2 miles south of Trent Woods, North Carolina and then flows northwest to join the Trent River about 0.5 miles east of River Bend.[3]
Watershed
Miry Hole Branch drains 1.44 square miles (3.7 km2) of area, receives about 54.7 in/year of precipitation, has a wetness index of 528.11, and is about 47% forested.[5]
See also
References
- 1 2 3 "GNIS Detail - Miry Hole Branch". geonames.usgs.gov. US Geological Survey. Retrieved 21 December 2020.
- ↑ "Get Maps". USGS Topoview. US Geological Survey. Retrieved 21 December 2020.
- 1 2 "Get Maps". USGS Topoview. US Geological Survey. Retrieved 20 December 2020.
- ↑ "ArcGIS Web Application". epa.maps.arcgis.com. US EPA. Retrieved 21 December 2020.
- 1 2 3 "Miry Hole Branch Watershed Report". US EPA Geoviewer. US EPA. Retrieved 21 December 2020.
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