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Deep Run (North Branch Patapsco River tributary) facts for kids

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Deep Run
Deep Run is located in the United States
Deep Run
Deep Run
Location in the United States
Deep Run is located in Maryland
Deep Run
Deep Run
Location in Maryland
Country United States
State Maryland
County Carroll County
Physical characteristics
Main source Carroll County, Maryland, United States
39°36′4″N 76°50′59″W / 39.60111°N 76.84972°W / 39.60111; -76.84972
River mouth Carroll County, Maryland, United States
453 ft (138 m)
39°31′33″N 76°52′41″W / 39.52583°N 76.87806°W / 39.52583; -76.87806
Basin features
Tributaries
  • Left:
    Aspen Run

Deep Run is a small stream located in Carroll County, Maryland, in the United States. It is a natural waterway that plays a part in the local environment. This stream is known as a tributary, which means it's a smaller river or stream that flows into a larger one.

What is Deep Run?

Deep Run is a natural stream. It is an important part of the local water system. It helps carry water from the land into bigger rivers. Think of it like a small road connecting to a main highway.

Deep Run's Role as a Tributary

A tributary is like a helper stream. Deep Run flows into the North Branch Patapsco River. This means Deep Run adds its water to the Patapsco River. The Patapsco River then continues its journey.

Where is Deep Run Located?

Deep Run is found entirely within Carroll County, Maryland. Carroll County is a part of the state of Maryland. Maryland is located on the east coast of the United States.

Starting Point and End Point

Deep Run begins its journey in Carroll County, Maryland. Its source is where the stream starts. It then flows until it reaches its mouth. The mouth is where it joins the North Branch Patapsco River. This meeting point is also in Carroll County. The elevation at its mouth is about 453 feet (138 meters) above sea level.

Other Streams Joining Deep Run

Deep Run also has its own smaller streams that flow into it. One of these is called Aspen Run. Aspen Run joins Deep Run on its left side. This shows how many streams connect to form larger waterways.

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