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Wallace Run (Bald Eagle Creek tributary)

Coordinates:40°55′51″N77°49′01″W / 40.9307°N 77.8169°W /40.9307; -77.8169
From Wikipedia, the free encyclopedia
(Redirected fromWallace Run (Bald Eagle Creek))
Not to be confused withWallis Run.

Wallace Run is a tributary ofBald Eagle Creek inCentre County,Pennsylvania, in the United States. It is 12.1 miles (19.5 km) long and is a low-alkalinity stream.[1] The stream flows throughUnion Township andBoggs Township in Centre County. Most of the watershed is in Boggs Township. The North Branch of Wallace Run is one tributary of the stream. The watershed has an area of 24 square miles (62 km2). Oaks, maples, ash trees, birches, hemlocks, and rhododendrons all exist in the upper reaches of the stream, which is mostly forested. The lower reaches of the stream are mostly developed.

Course

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Wallace Run begins in a valley in thePennsylvania State Game Lands Number 163 in western Union Township.[2] The headwaters are situated on the southern side of theAllegheny Plateau.[1] Foxy Hollow is to the south of the headwaters and Bear Knob is to the east. The stream flows northeast past Dry Hollow and picks up Rock Cabin Run on the left. The stream continues northeast, passing Grindstone Gap on the right and picking up Birch Lick Run on the left. After this, the creek flows around Ganderstep Knob, picking up its north branch. It turns southeast and exits the township.[2] Wallace Run then enters Boggs Township and its valley becomes shallower. The stream passesGum Stump and begins to parallelPennsylvania Route 144 for several miles to its mouth, passing the community ofRunville along the way. Wallace Run enters Bald Eagle Creek at the community of Wingate, a short distance upstream ofMilesburg.[3]

Tributaries

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Wallace Run's North Branch begins near the edge of Boggs Township, just south of Pennsylvania Route 144. It flows southwest a short distance into Union Township, where it joins the main stem.[3]

Hydrology

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The concentration ofalkalinity in Wallace Run near its source is 10 parts per million. Near its mouth, the concentration is 28 parts per million.[1]

At an unnamed tributary of Wallace Run downstream of Gum Stump, thepH was measured in 2008 to be 7.9 and 8.0 and the conductivity was 387 and 390 micro-siemens. In August 2008, the water temperature was 68 feet (21 m) in the lower reaches of the creek and 63 feet (19 m) two miles (three kilometers) upstream.[1]

In 2009, before a storm, the size of particles in Wallace Run was measured. 10% had a diameter of less than one millimeter, about one third had a diameter of less than one centimeter, and over 90% had a diameter of less than ten centimeters. After a storm, a very small percentage of particles had a diameter of less than one millimeter. Slightly under 10% of the particles had a diameter of less than one centimeter. 80% to 90% of the particles had a diameter of less than ten centimeters.[4]

TheManning formula values on Wallace Run were 0.039 on July 31 and August 1, 2009 and 0.046 on October 24, 2009.[4]

Geology and geography

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Wallace Run is a coldwaterfreestone stream. In the upper eight miles, the main rock types aresandstone, red and brownshale, and grayconglomerate. The elevation of the creek at its headwaters is 2,240 feet (680 m). For the first 6.1 miles (9.8 km), the stream's elevation decreases at a rate of 184 feet (56 m) per mile, reaching an elevation of 1,112 feet (339 m). For the next 2.1 miles (3.4 km), the elevation falls at a rate of 73 feet (22 m) per mile, to 958 feet (292 m). From this point to the mouth, the elevation decreases at a rate of 58 feet (18 m) per mile. The mouth is at an elevation of 726 feet (221 m).[1] The elevation of the entire Wallace Run watershed ranges from 211 metres (692 ft) to 758 metres (2,487 ft).[4]

Ice caves and other ice formations have been observed to form on Wallace Run in the wintertime.[5]

Wallace Run has experienced damagingfloods in the past. Past attempts to remedy this mainly focused on straightening the stream and lining it with rocks, increasing the velocity of the water. Landowners, as well as the area's governments, have attempted to addriprap andlevees to the stream to improve its quality. Although initially these attempts were unsuccessful, the stream quality has improved.[6]

3.2 kilometres (2.0 mi) upstream of Wallace Run's mouth, the stream is 12 metres (39 ft) in bankfull width and 0.55 metres (1.8 ft) in bankfull depth. The actual depth, as measured in 2009, was 0.37 metres (1.2 ft). Thedischarge of the stream was measured to be 5.3 cubic meters per second on July 31 and August 1, 2009 and 4.5 cubic meters per second on October 24, 2009. The velocity of the stream on these dates was 1.28 meters per second and 1.09 meters per second, respectively.[4]

The Bear Rocks are a geological formation located on a hill northeast of Wallace Run. They are square blocks of sandstone that are "nearly as big as houses". The Wallace Run valley is 900 feet (270 m) high in the upper reaches of the stream.[7]

Watershed

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The area of the Wallace Run watershed is 24 square miles (62 km2). The upper part of the watershed is mostly forested with some cabins, while the lower part is mostly suburban, with some agricultural land.[1] The watershed is mostly located within Boggs Township.[6]

History

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In the 1800s, there was asabbath school on Wallace Run.[8] Anarrow-gauge railroad once went through the creek's valley, but only traces of thegrade remain in the 21st century.[1][5] ThePennsylvania Fish and Boat Commission has done measurements of the fish andmacroinvertebrate populations in Wallace Run since the 1930s.[1] In the 1930s, theCivilian Conservation Corps constructed afire road on Ganderstep Knob and stairs leading from it down to the stream, where there was aswimming hole. The swimming hole no longer existed as of January 2008.[5] Threegas wells are located in the watershed, but only one is unplugged.[1] A 1,000-foot (300 m) stretch of the stream was restored by theWildlife for Everyone Foundation in 2010.[9]

Biology

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Near the headwaters, the main plants forming thecanopy arehemlock andrhododendron. Further downstream, but still in the first half of its course, the main trees areash (particularlywhite ash andgreen ash[7]),chestnut oaks,red oaks,red maples,tulips,yellow birches, and hemlocks. There are noriparian buffers in the lower reaches of the stream; there are oftenlawns instead.[1] Wallace Run is an approvedtrout stream (Class A Wild Trout Waters) by thePennsylvania Fish and Boat Commission.[10] Bothbrook trout andbrown trout live in the stream.[11]

Recreation

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Opportunities for recreation on Wallace Run includecanoeing,kayaking,birdwatching, andfishing.[6]

See also

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References

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  1. ^abcdefghijBald Eagle Watershed Association, Centre County Conservation District (October 2008),Wallace Run Assessment: October 2008(PDF), retrievedJanuary 27, 2014
  2. ^abUSGS (1953–1970),union.jpg, retrievedJanuary 27, 2014
  3. ^abUSGS (1953–1970),boggs.jpg, retrievedJanuary 27, 2014
  4. ^abcdMichael D. McKay (2010),A Thesis in Agricultural and Biological Engineering, retrievedJanuary 28, 2014
  5. ^abcGary Thornbloom (January 2008),No Snow, No Problem, retrievedJanuary 28, 2014
  6. ^abcCentre County Office of Planning & Community Development (August 2009),Centre County Recreation and Greenway Plan(PDF), archived fromthe original(PDF) on September 23, 2015, retrievedJanuary 28, 2014
  7. ^abWestern Pennsylvania Conservancy (December 31, 2002),Centre County Natural Heritage Inventory(PDF), retrievedJanuary 28, 2014
  8. ^Commemorative Biographical Record of Central Pennsylvania, 1898, retrievedJanuary 28, 2014
  9. ^Restoration of Wallace Run, Centre County, Underway, January 4, 2010, retrievedJanuary 28, 2014
  10. ^Pennsylvania Fish and Boat Commission (2014),NORTHCENTRAL REGION - Regulated Trout Waters, retrievedJanuary 28, 2014
  11. ^Pennsylvania Fish and Boat Commission (December 16, 2013),Class A Wild Trout Waters(PDF), retrievedJanuary 28, 2014
Lower Susquehanna River
Juniata River
West Branch Susquehanna River
Middle Susquehanna River
Chemung River
Upper Susquehanna River
  • Streams shown as: Tributaries
  • subtributaries
  • (subsubtributaries)

40°55′51″N77°49′01″W / 40.9307°N 77.8169°W /40.9307; -77.8169

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