| Mill Branch Tributary to Tussocky Branch  | |
|---|---|
![]() Location of Mill Branch mouth ![]() Mill Branch (Tussocky Branch tributary) (the United States)  | |
| Location | |
| Country | United States | 
| State | Delaware | 
| County | Sussex | 
| Physical characteristics | |
| Source | Tussocky Branch divide | 
| • location | Ralphs, Delaware[1] | 
| • coordinates | 38°30′03″N 075°38′40″W / 38.50083°N 75.64444°W[2] | 
| • elevation | 48 ft (15 m)[1] | 
| Mouth | Tussocky Branch | 
 • location  | about 0.5 miles north of Ralphs, Delaware[3] | 
 • coordinates  | 38°31′14″N 075°38′00″W / 38.52056°N 75.63333°W[2] | 
 • elevation  | 33 ft (10 m)[3] | 
| Length | 1.70 mi (2.74 km)[4] | 
| Basin size | 1.73 square miles (4.5 km2)[5] | 
| Discharge | |
| • location | Tussocky Branch | 
| • average | 2.01 cu ft/s (0.057 m3/s) at mouth with Tussocky Branch[5] | 
| Basin features | |
| Progression | Tussocky Branch → Broad Creek → Nanticoke River → Chesapeake Bay → Atlantic Ocean[4] | 
| River system | Nanticoke River | 
| Tributaries | |
| • left | unnamed tributaries | 
| • right | unnamed tributaries | 
| Bridges | DE 24 | 
Mill Branch is a 1.70 mi (2.74 km) long 1st order tributary to Tussocky Branch in Sussex County, Delaware.
Course
Mill Branch rises in Ralphs, Delaware[1] and then flows northerly into Tussocky Branch about 0.5 miles north of Ralphs, Delaware.[3]
Watershed
Mill Branch drains 1.73 square miles (4.5 km2) of area, receives about 44.6 in/year of precipitation, has a topographic wetness index of 816.27 and is about 20% forested.[5]
See also
References
- 1 2 3 "Get Maps". USGS Topoview. US Geological Survey. Retrieved 16 December 2020.
 - 1 2 "GNIS Detail - Mill Branch". geonames.usgs.gov. US Geological Survey. Retrieved 16 December 2020.
 - 1 2 3 "Get Maps". USGS Topoview. US Geological Survey. Retrieved 16 December 2020.
 - 1 2 "ArcGIS Web Application". epa.maps.arcgis.com. US EPA. Retrieved 16 December 2020.
 - 1 2 3 "Mill Branch Watershed Report". US EPA Geoviewer. US EPA. Retrieved 16 December 2020.
 
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