Pearl River (Mississippi–Louisiana)

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For other uses, see Pearl River.
Pearl River
Pearl River at Rosemary.jpg
The Pearl River in Hinds County, MS
Origin Neshoba County, Mississippi
Mouth Lake Borgne
Basin countries U.S.
Length 444 miles (715 km)
Source elevation 400 feet (120 m)
Basin area 8,760 square miles (22,700 km2)
Pearlmsrivermap.png

The Pearl River is a river in the U.S. states of Mississippi and Louisiana. It forms in Neshoba County, Mississippi from the confluence of Nanih Waiya and Tallahaga creeks.[1] and has a meander length of 444 miles (715 km).[2] The lower part of the river forms part of the boundary between Mississippi and Louisiana. The river contains large areas of bottomland hardwood swamp and cypress swamp, providing habitat for many species of wildlife including sturgeon and black bears. There was once hope that Ivory-billed woodpeckers might survive here, but this now seems unlikely.[3] The mouth of the river provides important marsh habitat along salinity gradients; these marshes have been the subject of many scientific studies.[4][5] It is considered to be one of the most critical areas of natural habitat remaining in Louisiana.[6]

Tributaries and hydrology

Pearl River backwater in Mississippi
Pearl River
Floating saloons on the Pearl River. The "Blue Goose" (left) and "Freeman Saloon" (center), near Old Gainesville, Hancock County, Mississippi, 1907.
A Saturn V first stage is transported by the barge Pearl River down the East Pearl River on its way from Stennis Space Center, then named the National Space Technology Laboratories, to Florida for launch.

The Yockanookany and Strong rivers are tributaries on the upper section and the Bogue Chitto is a tributary on the lower section. The Bogue Chitto's mean low-water discharge is nearly six times the mean low-water discharge of the Pearl River at Jackson, Mississippi, according to a 1936 government report of the Mississippi Planning Commission.[7] Northeast of Jackson, the Ross Barnett Reservoir is formed by a 1962 dam. Average annual rainfall is about 52 inches in the upper third of the basin, and below Jackson the basin rainfall increases to 64 inches or more.[8] The Yockanookany River along with the Lobutcha, Tuscolameta, and Pelahatchie Creeks are major tributaries to the river north of Jackson.[9]

West of Picayune, about 50 miles (80 km) above the mouth, the river forks.[10] The East Pearl River empties into Lake Borgne, where the dredged Pearl River Channel meets the Gulf Intracoastal Waterway. The discharge flows eastward past Grand Island through St. Joe Pass and into the Mississippi Sound.[11] The West Pearl River flows into The Rigolets, thence into Lake Borgne.[12] Both discharges eventually reach the Gulf of Mexico. The Pearl River serves as the 115-mile (185 km) boundary between Mississippi and Louisiana[2] in its lower reach near the Gulf of Mexico.

Pearl River provides the receiving waters for the Savanna Street Sewage Treatment Plant in Jackson, Mississippi.[13] which lies about 180 miles (290 km) from the mouth of the river.

Pearl River towns

The Pearl passes near or through the following towns (in order, north to south):

Pearl River navigation

The U.S. Army Corps of Engineers has undertaken three significant navigation projects in the Pearl River Basin. In 1880, Congress authorized a 5-foot (1.5 m) navigation channel on the West Pearl River from Jackson to the Rigolets. That project was discontinued in 1922. Beginning in 1910, a channel was dredged from the mouth of the East Pearl River into Lake Borgne, a project which is maintained on an irregular basis. In 1935, the West Pearl River Navigation Project was authorized. It provided for a navigation channel from Bogalusa to the mouth of the West Pearl River. The project includes a canal with three locks. The Corps of Engineers placed the project in "caretaker" status in the 1970s because of a decline in commercial traffic. Maintenance dredging resumed in December 1988.[14] In the 1950s, underwater concrete sills were constructed to help maintain water levels in the navigation channel. This has prevented Gulf sturgeon and other migratory species from accessing upstream areas. A rock ramp constructed in 2003 helps fish navigate over one of the sills,[15] but environmental groups propose further work to mitigate the effects of the navigation project.[16]

Building dams, canals, levees and water control structures is known to have highly negative effects on wetlands and the ecological services they provide.[17][18] Increasingly, these artificial structures are being removed to allow natural river activities to resume.[19] The Pascagoula River is one of the few remaining southern rivers with natural water regimes, and is a potential model for restoring the Pearl River floodplain. At the Bogalusa, Louisiana gauge the river was recorded in 1983 and 1987 as delivering nearly 3.5 million metric tons and 2.5 million metric tons of sediment respectively.[20]

Hurricane effects

Hurricanes are a natural form of disturbance that shapes rivers and watersheds on the Gulf Coast, and has done so for thousands of years.[21][22] As one recent example, Hurricane Katrina in August 2005 caused further natural changes in the Pearl River. Bottom sediments and marsh vegetation—including uprooted cypress and oak trees—blocked the mouth of the West Pearl and other parts of the channel. The Louisiana Department of Wildlife & Fisheries and other agencies removed 27,000 cubic meters (35,000 yd³) of debris.[23] However, the accumulation of this woody debris is a natural part of floodplain ecosystems in general, and wetlands in particular, and provides vital habitat for species including fish and turtles.[24] Hence, this use of state funds to remove debris was an expenditure on an activity that is known to have negative impacts upon watersheds and wild species.

In popular culture

The journalist and poet Pearl Rivers and the country music band Pearl River named themselves after this river. In wrestling, Ahmed Johnson's finishing maneuver was known as the Pearl River Plunge.

See also

References

  1. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  2. ↑ 2.0 2.1 U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map, accessed June 13, 2011
  3. ↑ Keddy, P.A. 2008. Water, Earth, Fire: Louisiana’s Natural Heritage. Xlibris, Philadelphia. 229 p. Figure p. 169. ISBN 978-1-4363-6234-4
  4. ↑ Taylor, K. L. and Grace, J. B. (1995). The effects of vertebrate herbivory on plant community structure in the coastal marshes of the Pearl River, Louisiana, USA. Wetlands, 15, 68–73.
  5. ↑ Gough, L. G., Grace, J. B., and Taylor, K. L. (1994). The relationship between species richness and community biomass: the importance of environmental variables. Oikos, 70, 271–9.
  6. ↑ Keddy, P.A. 2008. Water, Earth, Fire: Louisiana’s Natural Heritage. Xlibris, Philadelphia. 229 p. Figure 6.1. ISBN 978-1-4363-6234-4
  7. ↑ Drainage Basin and Waterways Reports, 1936-1938. Mississippi Planning Commission. Mississippi Department of Archives and History. Series 2488 Box 19948. "Report on the Pearl River Drainage Basin". Page.1.
  8. ↑ United States Department of the Interior. Water Resources Division. U.S. Geological Survey in cooperation with Mobile District. Corps of Engineers. Department of the Army. (1967) Joseph W. Lang. "Geohydrologic Summary of the Pearl River Basin". p. 11.
  9. ↑ Speer, Paul R. et al. (1949). "Low-Flow Characteristics of streams in the Mississippi Embayment to Southern Arkansas, Northern Louisiana and Northeastern Texas." Geological Survey Professional Paper 448-G. Washington, DC: Government Printing Office. p. I-27. Google Books website
  10. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  11. ↑ Lua error in package.lua at line 80: module 'strict' not found.[dead link]
  12. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  13. ↑ Savanna Street Wastewater Treatment Plant, Risk Management Plan, Executive Summary - 2012. Accessed July 19, 2014
  14. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  15. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  16. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  17. ↑ Middleton, B. A. (ed.) (2002). Flood Pulsing in Wetlands: Restoring the Natural Hydrological Balance. Wiley, New York.
  18. ↑ Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. 978-0-521-51940-3
  19. ↑ Hughes, F.M.R. (ed.). 2003. The Flooded Forest: Guidance for policy makers and river managers in Europe on the restoration of floodplain forests. FLOBAR2, Department of Geography, University of Cambridge, Cambridge, UK. 96 p.
  20. ↑ United States Geological Survey. Suspended-Sediment Database Daily Values of Suspended Sediment and Ancillary Data. Introduction of Sediment Data Histograms. http://co.water.usgs.gov/sediment/images/la1.gif
  21. ↑ Michener, W. K., Blood, E. R., Bildstein, K. L., Brinson, M. M., and Gardner, L. R. (1997). Climate change, hurricanes and tropical storms, and rising sea level in coastal wetlands. Ecological Applications, 7, 770–801.
  22. ↑ Conner, W. H., Day, J. W., Jr., Baumann, R. H., and Randall, J. M. (1989). Influence of hurricanes on coastal ecosystems along the northern Gulf of Mexico. Wetlands Ecology and Management, 1, 45–56.
  23. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  24. ↑ Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. p. 225-227, Figure 8.14, 8.15, ISBN 978-0-521-51940-3

External links

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