Fisher Run facts for kids
Quick facts for kids Fisher Run |
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Fisher Run looking upstream in its lower reaches
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| Physical characteristics | |
| Main source | Catawissa Mountain in Main Township, Columbia County, Pennsylvania 1,340 ft (410 m) |
| River mouth | Catawissa Creek in Beaver Township, Columbia County, Pennsylvania 574 ft (175 m) 40°57′24″N 76°21′20″W / 40.95666°N 76.35545°W |
| Length | 2.9 mi (4.7 km) |
| Basin features | |
| Progression | Catawissa Creek → Susquehanna River → Chesapeake Bay |
| Basin size | 3.03 sq mi (7.8 km2) |
| Tributaries |
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Fisher Run is a small stream, also called a tributary, that flows into Catawissa Creek in Columbia County, Pennsylvania. It's about 2.9 miles (4.7 km) long. This stream flows through two areas: Main Township and Beaver Township. Even though it has some pollution from old mines, Fisher Run is known for its very cold, clean water. It's a great place for certain fish, especially wild trout! The land area that drains into Fisher Run is about 3.03 square miles (7.85 km2).
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Where Does Fisher Run Flow?
Fisher Run starts high up on Catawissa Mountain. This mountain is in the southwestern part of Main Township.
The stream first flows east through a valley. It crosses a road not long after it begins. Then, it turns and flows northeast for more than a mile. Along its path, it crosses Fisher Run Road and then Iron Bridge Road. Right after Iron Bridge Road, the stream turns southeast. It then enters Beaver Township. In Beaver Township, Fisher Run quickly meets up with Catawissa Creek.
Fisher Run joins Catawissa Creek about 8.78 miles (14.13 km) before Catawissa Creek reaches its own end.
Smaller Streams Joining Fisher Run
Fisher Run has one smaller stream that flows into it. This stream doesn't have a common name. It is simply called "Trib 27549 To Fisher Run."
Water Quality of Fisher Run
Fisher Run's water quality is affected by something called acid mine drainage. This means that water from old mines can flow into the stream. This mine water can carry metals and make the stream less healthy. Fisher Run is one of several streams in the Catawissa Creek area that has this issue.
The pH level of the stream's water is usually between 6.0 and 6.9. This means it's slightly acidic. The water also has a small amount of alkalinity, which helps to balance the acidity.
Land and Rocks Around the Stream
The land around the mouth of Fisher Run is about 574 feet (175 meters) above sea level. Where the stream begins, its source is much higher, around 1340 feet (408 meters) above sea level.
Most of the land that drains into Fisher Run is made of certain types of rock. The upper parts of the stream's area are mostly on rock from the Pocono Formation. The lower parts are on rock from the Mauch Chunk Formation. However, the southern part of the area has rock from the Spechty Kopf Formation and the Buddys Run Member of the Catskill Formation.
The main soil types found in the Fisher Run area are called Leck Kill soil, Hazleton soil, and Watson soil.
History and Name of Fisher Run
The entire area that drains water into Fisher Run is about 3.03 square miles (7.85 km2). Most of this area is in Main Township. But some parts are also in Catawissa Township and Roaring Creek Township. A very small part of the area is in Beaver Township.
The upper parts of the Fisher Run area are located within Pennsylvania State Game Lands Number 58. This is a protected area. However, as the stream flows lower, it goes through agricultural land, which is used for farming.
Fisher Run was most likely named after a person named Isaac Fisher.
Animals and Fish in Fisher Run
The Pennsylvania Department of Environmental Protection says that Fisher Run is a very good place for coldwater fish. It's also called "Class A Wild Trout Waters" by the Pennsylvania Fish and Boat Commission. This means it's an excellent habitat for wild trout.
The stream is home to brook trout. These fish are special because they reproduce naturally throughout the stream. This shows that the stream provides a good environment for them to live and have their young.
