Nescopeck Mountain

Nescopeck Mountain
Nescopec Mountain

Nescopeck Mountain in Main Township, Columbia County, Pennsylvania
Elevation 1,604 ft (489 m)
Prominence up to 850 feet (260 m) or 900 feet (270 m)
Location
Range chain of mountains from Moosic to the Susquehanna River
Coordinates 40.986ºN, 76.312ºW[1]
Topo map Shumans (for official coordinates; others for the rest of the ridge)
Geology
Type Ridge

Nescopeck Mountain (also known as Nescopec Mountain[2]) is a ridge in Columbia County and Luzerne County, in Pennsylvania, in the United States.[1][3] Its peak elevation is 1,604 feet (489 m) above sea level. The ridge is a forested ridge, with at least two types of forest and two systems of vernal pools. It is a very long and unbroken ridge with two water gaps: one carved by Catawissa Creek and one carved by Nescopeck Creek. Rock formations in the ridge include the Lower Helderberg Formation, the Onondaga Formation, the Spechty Kopf Formation, the Trimmers Rock Formation, and the Mauch Chunk Formation. In the most recent ice age, it was affected by glaciation.

Native Americans historically settled in the vicinity of Nescopeck Mountain. It was visited by Europeans as early as 1755. The ridge's name most likely means "dirty waters" or "black waters". Two Pennsylvania State Game Lands and one state park are situated partially on it. The ridge spans numerous townships in Columbia County and Luzerne County.

Geography

Nescopeck Mountain and Pennsylvania Route 339 from the north in Mifflin Township, Columbia County, Pennsylvania

The elevation of Nescopeck Mountain is 1,604 feet (489 m) above sea level, making it the highest ridge in Columbia County.[1] Townships that Nescopeck Mountain occupies include Beaver Township, Mifflin Township, and Main Township in Columbia County.[3] The ridge extends into Luzerne County, at least as far east as Nescopeck State Park.[2][4] Nescopeck Township is one township that Nescopeck Mountain goes through in Luzerne County.[5]

Nescopeck Mountain is an unbroken ridge, being described as "regular and almost unbroken" in an 1832 book.[6][7] John Gosse Freeze's 1888 book A History of Columbia County, Pennsylvania: From the Earliest Times described the ridge as "beautiful and regular in its formation".[8] It stretches from near the Susquehanna River almost to the Lehigh River and has a length of nearly 20 miles (32 km).[6][7] It is considerably steeper and higher on its northern side, at least in the United States Geological Survey quadrangle of Berwick.[9] The ridge is too rocky for agriculture, with large boulders being abundant on it.[10]

Nescopeck Mountain is part of a long chain of continuously forested mountains and ridges that stretches from Moosic Mountain to the Susquehanna River.[3] It is considered to be an extension of Catawissa Mountain.[11] The ridge is similar in height to mountains in the vicinity of the Wyoming Valley.[6] The ridge has a topographic prominence of up to approximately 850 feet (260 m) in places and up to 900 feet (270 m) at the Nescopeck Creek water gap.[7][12] However, it is only 400 to 500 feet (120 to 150 m) high near its western end at Mainville.[10]

Interstate 80 crosses through the water gap carved by Nescopeck Creek in Nescopeck Mountain.[13] The Susquehanna River Lowlands are in the vicinity of the ridge.[14] Large groups of small kettle holes are found along the base of the ridge.[15]

Nescopeck Mountain's official coordinates are in the United States Geological Survey quadrangle of Shumans.[1]

Streams and valleys

Catawissa Creek just upstream of where it cuts between Catawissa Mountain and Nescopeck Mountain

A creek known as Nescopeck Creek is in the vicinity of Nescopeck Mountain.[6] Additionally, Black Creek, a major tributary of Nescopeck Creek, empties into the larger creek at the base of the ridge.[7] The ridge is north of the creek for a portion of its length. There is a valley known as the Nescopeck Valley which is between Nescopeck Mountain and Buck Mountain. Nescopeck Creek flows through this valley. This valley is 20 miles (32 km) long and 5 miles (8.0 km) wide.[7] Some streams on the ridge are part of the Lehigh River watershed.[16]

A stream known as Scotch Run flows through a valley with Nescopeck Mountain on its northern edge.[17]

Nescopeck Mountain forms a water gap with Catawissa Mountain.[10] Catawissa Creek cuts through this water gap.[17] There is also a water gap carved by Nescopeck Creek through Nescopeck Mountain.[13] The mountain serves as part of the dividing line between the Susquehanna River and the Lehigh River watersheds.[16]

Geology

The geology of Nescopeck Mountain at Catawissa Creek

There are a total of three rock formations on Nescopeck Mountain in the Berwick Quadrangle, which is in Columbia County and Luzerne County. From north to south, these rock formations are the Trimmers Rock Formation (from the Devonian Period), the Spechty Kopf Formation (from the Devonian Period and the Mississippian Period), and the Onondaga Formation (from the Devonian Period). All three of these formations occur in bands that are at an angle relative to the surface. The Spechty Kopf Formation occurs at the peak of the ridge and extends to a depth of approximately 1,500 feet (460 m) below sea level. The Onondaga Formation runs from near the ridge's peak to 1,000 feet (300 m) below sea level. The Trimmers Rock Formation runs from the middle elevations of the ridge to more than 2,000 feet (610 m) below sea level.[9] In Mifflin Township, Columbia County, the peak of Nescopeck Mountain is on rock of the Lower Helderberg Formation.[17] Additionally, the Mauch Chunk Formation is found on the ridge.[18]

There are coal basins to the south of Nescopeck Mountain.[19]

During an ice age, glaciers pressed against Nescopeck Mountain and eventually moved over it, carrying gravel from the Susquehanna River.[12] The ridge was near the southern edge of the most recent period of glaciation.[3]

History and etymology

Historically, there was a Shawnee village in the vicinity of Nescopeck Mountain, where the borough of Nescopeck is in modern times.[2] Additionally, the Forks Indians arrived at the ridge in 1740 after being evicted from their lands in the Lehigh Valley.[16] As early as 1755, a pair of Moravian missionaries, Christian Seidel and Henry Frey, descended the ridge while visiting Native Americans.[20]

In 1838, a man named Mr. Butler requested permission of the Pennsylvania House of Representatives to construct a tunnel or through cut through Nescopeck Mountain for the Lehigh Coal and Navigation Company.[21] In the late 1800s and early 1900s, the Glen Summit Springs Hotel operated on top of Nescopeck Mountain. It was constructed by the Lehigh Valley Railroad Company. During its most active use, it attracted visitors from the Wyoming Valley and from the East Coast of the United States.[22] The Lehigh Valley Railroad historically passed over the ridge.[23] In the late 1800s, the ridge was prospected for coal.[8]

The top of Nescopeck Mountain was devoid of trees in the middle of the 1800s.[6] Logging has been done on the ridge in the early 2000s and plans have been made to construct communication towers on the ridge.[3] Local produce is sometimes traded over Nescopeck Mountain.[24] The mountain is almost completely undeveloped.[15]

Nescopeck Mountain is most likely named for the Shawnee village called Nescopeck. The word nescopeck itself is a corruption of neskchoppeck, which may mean "dirty waters" or "black waters".[2]

A gypsy moth infestation began on Nescopeck Mountain in the summer of 2014, causing hundreds of trees to be defoliated. The Bureau of Forestry expects to begin spraying the area in May 2015 and June 2015.[25]

Biology

Nescopeck Mountain, a forested ridge

Nescopeck Mountain is one of several mountains in Columbia County to contain undisturbed oak/mixed hardwood forests. This forest is also an Appalachian Oak Forest. Specific tree species on the ridge in Columbia County include red oak, chestnut oak, scarlet oak, black birch, American chestnut, pitch pine, red maple, and serviceberry. Other plants on the ridge include black huckleberry, lowbush blueberry, mountain laurel, sheep's laurel, bracken fern, wild sarsaparilla, and Virginia creeper.[3]

An ephemeral/fluctuating pool natural community known as the Edgewood Vernal Pools is located on and near Nescopeck Mountain. It consists of dozens of vernal pools created by glaciation. Numerous amphibian species breed in the pools and hardwood trees and hemlock are present on the southern edge of the pool system. A globally rare species of invertebrate was observed in the pools in 1990. Another system of vernal pools known as the Briggsville Vernal Pools are found north of the ridge.[15]

The Nescopeck Mountain Barrens are a ridgetop dwarf-tree forest natural community. The barrens consist of scrub oaks, hairgrass, pitch pines, little bluestems, and blueberries.[15]

Recreation

A portion of the Pennsylvania State Game Lands Number 58 is on Nescopeck Mountain.[3] Additionally, the Pennsylvania State Game Lands Number 187 contain the Nescopeck Mountain Barrens.[15] The ridge is on the northern border of the 3550-acre Nescopeck State Park.[4] Historically, there were trails leading up to the top of Nescopeck Mountain. There is high visibility from the top of the ridge and the town of Bloomsburg can be seen.[10]

The water gap where Catawissa Creek flows between Nescopeck Mountain and Catawissa Mountain was described as "attractive" by I. W. Hartman in 1912.[10] The water gap where Nescopeck Creek flows through Nescopeck Mountain is described as "impressive" in Jeff Mitchell's book Paddling Pennsylvania.[13]

See also

References

  1. ↑ 1.0 1.1 1.2 1.3 Topographic Map Ridge Features in Columbia County, Pennsylvania, retrieved December 7, 2014
  2. ↑ 2.0 2.1 2.2 2.3 Walter M. Brasch (1982), Columbia County Place Names, p. 156
  3. ↑ 3.0 3.1 3.2 3.3 3.4 3.5 3.6 The Pennsylvania Science Office of The Nature Conservancy (2004), Columbia County Natural Areas Inventory 2004, retrieved December 7, 2014
  4. ↑ 4.0 4.1 Pennsylvania Department of Conservation and Natural Resources, Nescopeck State Park, retrieved December 9, 2014
  5. ↑ Nescopeck Township, Nescopeck Township, retrieved December 9, 2014
  6. ↑ 6.0 6.1 6.2 6.3 6.4 William Darby (1845), Universal gazetteer: a dictionary, geographical, historical, and statistical, of the various kingdoms, states, provinces, seas, mountains, etc., in the world, p. 509
  7. ↑ 7.0 7.1 7.2 7.3 7.4 Thomas Francis Gordon (1832), A Gazetteer of the State of Pennsylvania, pp. 54,317
  8. ↑ 8.0 8.1 John Gosse Freeze (1888), A History of Columbia County, Pennsylvania: From the Earliest Times, p. 51
  9. ↑ 9.0 9.1 Jon D. Inners (1978), Bedrock geologic map of the Berwick quadrangle, Luzerne and Columbia counties, Pennsylvania, retrieved December 10, 2014
  10. ↑ 10.0 10.1 10.2 10.3 10.4 I. W. Hartman (May 2, 1912), "IRON ORE FURNACE AT MAINVILLE First in Columbia County, Was Built in the Year 1815 Southsider's Prosperous Residents Supposed Hidden Coal in the Mountain Still Unmined", Democratic Sentinel, retrieved December 10, 2014
  11. ↑ Charles B. Trego (1843), A geography of Pennsylvania, p. 51
  12. ↑ 12.0 12.1 Edward Higginson Williams (1917), Pennsylvania Glaciation, First Phase: Materials for a Discussion of the Attenuated Border of the Moraine Described in Volume Z of the Second Geological Survey of Pennsylvania, p. 
  13. ↑ 13.0 13.1 13.2 Jeff Mitchell, Paddling Pennsylvania: Canoeing and Kayaking the Keystone State's Rivers and Lakes, p. 89
  14. ↑ General Geology Report, Volumes 70–72, 1978, p. 56
  15. ↑ 15.0 15.1 15.2 15.3 15.4 Pennsylvania Natural Heritage Program (Western Pennsylvania Conservancy) (2006), A NATURAL AREAS INVENTORY LUZERNE COUNTY, PENNSYLVANIA Update – 2006, retrieved December 10, 2014
  16. ↑ 16.0 16.1 16.2 Robert S. Grumet (June 26, 2013), Manhattan to Minisink: American Indian Place Names of Greater New York and Vicinity, University of Oklahoma Press, pp. 107–108
  17. ↑ 17.0 17.1 17.2 J. H. Beers (1915), Historical and biographical annals of Columbia and Montour counties, Pennsylvania, p. 
  18. ↑ Bureau of Topographic and Geologic Survey (1941), Mineral Resource Report M, p. 
  19. ↑ Manufactures of the United States in 1860, p. 
  20. ↑ Hazard's Register of Pennsylvania, Volume 15, 1835, p. 139
  21. ↑ Pennsylvania House of Representatives (1838), Journal, Volume 49, Part 1, p. 232
  22. ↑ Pamela C. Turfa (July 13, 2003), "A place of cool retreat: an area resort widely known in late 19th century offered escape to the mountains", The Times Leader, retrieved December 10, 2014
  23. ↑ Joseph Kubic, Darlene Miller-Lanning (2012), Mountain Top, Arcadia Publishing, p. 9
  24. ↑ Mia Light, "Regional farmers enjoy good summer for crops", Republican & Herald, retrieved December 9, 2014
  25. ↑ Tom Ragan (October 5, 2014), "Gypsy moth infestation on Nescopeck Mountain", Standard-Speaker, retrieved December 9, 2014

External links

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Coordinates: 41°00′25″N 76°13′16″W / 41.007°N 76.221°W