World Library  
Flag as Inappropriate
Email this Article

Wiconisco Creek

Article Id: WHEBN0005008827
Reproduction Date:

Title: Wiconisco Creek  
Author: World Heritage Encyclopedia
Language: English
Subject: Wiconisco, Wiconisco Township, Dauphin County, Pennsylvania, Little Conestoga Creek, Clover Creek (Pennsylvania), Shaver Creek
Collection:
Publisher: World Heritage Encyclopedia
Publication
Date:
 

Wiconisco Creek

Wiconisco Creek is a tributary of the Susquehanna River in Schuylkill and Dauphin counties, Pennsylvania, in the United States. It is approximately 45.5 miles (73.2 km) long.[1]

Contents

  • Course 1
    • Tributaries 1.1
  • Hydrology 2
  • Geography, geology, and climate 3
  • Watershed 4
  • History, etymology, and industries 5
  • Biology 6
  • Recreation 7
  • See also 8
  • References 9

Course

Wiconisco Creek begins on a bend on a mountain in Porter Township, Schuylkill County. It flows in the general direction of west-southwest for several miles between two mountains, one of which is north of the creek and the other of which is south of the creek. The creek passes near Tower City, where the southern border of its valley is defined by a different mountain, and shortly afterwards leaves Schuylkill County.[1]

Upon leaving Schuylkill County, Wiconisco Creek enters Williams Township, Dauphin County. In this township, the creek continues in a westward direction, crossing U.S. Route 209 and passing Williamstown. Further on, the creek enters Wiconisco Township, where it passes by the community of Lykens. Here, it receives the tributary Bear Creek and then the tributary Rattling Creek. Wiconisco Creek then leaves Wiconisco Township and enters Washington Township, where it picks up the tributaries Big Run and Canoe Gap Run. The creek then reaches the end of its valley and turns abruptly north, crossing U.S. Route 209 again. It briefly enters Lykens Township before starting to meander southwest back into Washington Township. Here, the creek crosses Pennsylvania Route 225 and continues meandering in the same direction. It crosses U.S. Route 209 again and enters Upper Paxton Township, where it begins to meander parallel to Berry Mountain. After a while, the creek stops meandering, but continues west, receiving the tributary Little Wiconisco Creek. The creek then reaches its confluence with the Susquehanna River between Lenkerville and Millersburg.[1]

Wiconisco Creek reaches its confluence with the Susquehanna River 97.99 miles (157.70 km) upstream of its mouth.[2]

Tributaries

Tributaries of Wiconisco Creek include Little Wiconisco Creek, Keefers Run, Big Run, Rattling Creek, and Bear Creek. Rattling Creek is the largest of these tributaries, with a watershed area of 19.6 square miles (51 km2). Little Wiconisco Creek is the second-largest tributary. Its watershed has an area of 17.1 square miles (44 km2). The smallest tributary of Wiconisco Creek is Big Run, whose watershed has an area of 1.0 square mile (2.6 km2). Additionally, the tributary Rattling Creek has a number of sub-tributaries.[3]

Hydrology

Wiconisco Creek is considered by the Pennsylvania Department of Environmental Protection to be impaired by abandoned mine drainage, wastewater, and agriculture. Approximately half of the main stem and large parts of Little Wiconisco Creek are considered to be impaired. The creek's water quality is degraded by Bear Creek and three tunnels: the Big Lick Tunnel, Keffer's Tunnel, and the Porter Tunnel.[4]

The concentration of iron in the waters of Wiconisco Creek ranges from 0.41 to 1.7 milligrams per liter (where detected), depending on the site. The daily load ranges from 66.14 to 753.73 pounds (30.00 to 341.89 kg). The concentration of manganese in the waters of the creek ranges from 0.23 to 0.94 milligrams per liter (where detected), depending on the site. The daily load ranges from 40.63 to 203.95 pounds (18.43 to 92.51 kg). The concentration of aluminum in the creek ranges from 0.6 to 1.27 milligrams per liter (where detected), depending on the site. The daily load ranges from 54.9 to 86.22 pounds (24.90 to 39.11 kg). The concentration of acidity ranges from 27.47 to 48.3 milligrams per liter, depending on the site. The daily load ranges from 1,852.28 to 21,167.71 pounds (840.18 to 9,601.51 kg). The concentration of alkalinity ranges from 3.2 to 70.17 milligrams per liter, depending on the site. The daily load ranges from 138.33 to 13,796.13 pounds (62.75 to 6,257.82 kg).[4]

Geography, geology, and climate

The elevation near the mouth of Wiconisco Creek is 380 feet (120 m) above sea level.[5] The highest elevation in the watershed is 1,785 feet (544 m) above sea level. This occurs on Big Lick Mountain.[4] From river mile 37.5 to the mouth, the elevation of the creek decreases at a rate of 11.4 feet (3.5 m) per mile.[3]

Some strainers are situated on Wiconisco Creek between Lykens and Loyalton. The creek flows through a

  1. ^ a b c  
  2. ^ a b Pennsylvania Gazetteer of Streams (PDF), November 2, 2001, retrieved September 3, 2014 
  3. ^ a b c d e f Water Supply Commission of Pennsylvania, Water Resources Inventory Report, p. 642, retrieved September 3, 2014 
  4. ^ a b c d e f g h i j k l m  
  5. ^ Topographic Map Stream Features in Dauphin County, Pennsylvania, retrieved September 3, 2014 
  6. ^ a b c d e f Edward Gertler (1984), Keystone Canoeing, Seneca Press, p. 203 

References

See also

It is possible to canoe on 34 miles (55 km) of Wiconisco Creek during snowmelt in late winter and spring or several days after heavy rains. The creek is considered to be suitable for novice canoers. However, there are Class 1 and Class 2 rapids on the creek near the community of Lykens. Edward Gertler describes the scenery as "poor to good" in his book Keystone Canoeing.[6]

Recreation

Wiconisco Creek is designated as a warmwater fishery in Dauphin County.[4]

Groves of hemlock can be found on Wiconisco Creek, as can alder trees.[6]

Biology

In the early 1900s, the Pennsylvania Railroad followed Wiconisco Creek between its mouth and Williamstown. The Philadelphia and Reading Railroad followed the creek from its headwaters as far as Lykens.[3]

Coal mining (both strip mining and deep mining) is done in the upper reaches of the watershed of Wiconisco Creek, and has been since the late 1800s.[6][4] There are six active mining permits in the watershed.[4] The remains of a dam are located in the lower reaches.[6]

The name of Wiconisco Creek comes from a Native American word meaning "wet and dirty camp".[6]

History, etymology, and industries

Almost all of the southern part and northern and northwestern edges of the watershed of Wiconisco Creek is forested land, including Pennsylvania State Game Lands. Nearly all of the western part of the watershed is agricultural land. Abandoned mining land is found in patches in the watershed's eastern half. Most of the watershed's population centers are found in a band running through the central part of the watershed from east to west.[4]

Major roads in the watershed of Wiconisco Creek include U.S. Route 209 and also Pennsylvania Route 225 and Pennsylvania Route 325. A large number of township roads are also found in the watershed.[4]

Numerous boroughs and villages are situated in the watershed of Wiconisco Creek. Boroughs in the western part of the watershed include Berrysburg, Elizabethville, and Millersburg. Boroughs in the central part of the watershed include Lykens, Gratz, and Wiconisco and boroughs in the watershed's eastern portion include Tower City and Williamstown. Villages in the eastern part of the watershed include Muir , Orwin, Reinerton, and Sheridan. Villages in the central part of the watershed include Big Run, Dayton, and Loyalton and villages in the watershed's western section include Cloverly Acres, Pleasant Hills, and Reservoir Heights.[4]

The watershed of Wiconisco Creek has an area of 116 square miles (300 km2).[2] The watershed of the creek is situated in southwestern Schuylkill County and northern Dauphin County.[3] The watershed is on several United States Geological Survey 7.5 minute quadrangles: the Elizabethville quadrangle, the Lykens quadrangle, the Millersburg quadrangle, the Pine Grove quadrangle, and the Tower City quadrangle.[4]

Watershed

The annual rate of precipitation in the watershed of Wiconisco Creek ranges between 40 inches (100 cm) and 50 inches (130 cm).[3]

The Hazleton-Dekalb-Lehew soil association occurs in the southern, northeastern, and northwestern parts of the Wiconisco Creek watershed. A minute area near the mouth of the creek is occupied by soil of the Duncannon-Urban-Land-Chavies association. The rest of the watershed is occupied by the Leck Kill-Minersville-Calvin soil association.[4]

The Pocono Formation occurs in the southern part of the Wiconisco Creek watershed and also on the northwestern edge. The Llewellyn Formation and the Pottsville Group occur in the northeastern part of the watershed. The Pottsville Group is also found in the watershed's southeastern portion. The Spechty Kopf Formation and the Duncannon Member of the Catskill Formation occur in small areas in the its southernmost portion. The rest of the watershed is on the Mauch Chunk Formation.[4]

The channel of Wiconisco Creek is tortuous. The creek flows through rock formations made of sandstone and shale. Deposits of anthracite occur in the watershed.[3] The main rock formation in the watershed is the Mauch Chunk Formation. Other rock formations include the Duncannon Member of the Catskill Formation, the Llewellyn Formation, the Pocono Formation, the Pottsville Formation, and the Spechty Kopf Formation.[4]

[6]

This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and USA.gov, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for USA.gov and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
 
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
 
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.
 


Copyright © World Library Foundation. All rights reserved. eBooks from Project Gutenberg are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.