Iron Mine Branch
Tributary to Marshyhope Creek
Map of Iron Mine Branch mouth location
Map of Iron Mine Branch mouth location
Location of Iron Mine Branch mouth
Map of Iron Mine Branch mouth location
Map of Iron Mine Branch mouth location
Iron Mine Branch (Marshyhope Creek tributary) (the United States)
Location
CountryUnited States
StateDelaware
CountySussex
Physical characteristics
SourceBridgeville Branch divide
  locationDublin Hill, Delaware
  coordinates38°46′12.00″N 075°38′33.00″W / 38.7700000°N 75.6425000°W / 38.7700000; -75.6425000[1]
  elevation58 ft (18 m)[1]
MouthMarshyhope Creek
  location
about 1-mile south-southwest of Woodenhawk, Delaware
  coordinates
38°46′57.41″N 075°38′33.00″W / 38.7826139°N 75.6425000°W / 38.7826139; -75.6425000[1]
  elevation
23 ft (7.0 m)[1]
Length3.96 mi (6.37 km)[2]
Basin size2.82 square miles (7.3 km2)[3]
Discharge 
  locationMarshyhope Creek
  average3.40 cu ft/s (0.096 m3/s) at mouth with Marshyhope Creek[3]
Basin features
ProgressionMarshyhope CreekNanticoke RiverChesapeake Bay → Atlantic Ocean[2]
River systemNanticoke River
Tributaries 
  leftunnamed tributaries
  rightunnamed tributaries
BridgesEpworth Church Road, PA 404, Smith Road, Sand Hill Road

Iron Mine Branch is a 3.82 mi (6.15 km) long second-order tributary to Marshyhope Creek in Sussex County, Delaware.

Course

Iron Mine Branch rises on the Bridgeville Branch divide at Dublin Hill, Delaware, and then flows generally northwest to join Marshyhope Creek about 1.5 miles south-southwest of Woodenhawk, Delaware.[1]

Watershed

Iron Mine Branch drains 2.82 square miles (7.3 km2) of area, receives about 44.8 in/year of precipitation, and is about 3.04% forested.[3]

See also

References

  1. 1 2 3 4 5 "Geographic Names Information System". edits.nationalmap.gov. US Geological Survey. Retrieved January 27, 2023.
  2. 1 2 "ArcGIS Web Application". epa.maps.arcgis.com. US EPA. Retrieved January 27, 2023.
  3. 1 2 3 "Watershed Report | Office of Water | US EPA". watersgeo.epa.gov. US EPA. Retrieved January 27, 2023.
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