Pearl River (Mississippi–Louisiana)
Template:Short description Template:Use American English Template:For other uses Template:Infobox river The Pearl River is a blackwater river<ref>Singh, Shatrughan, et al. "Hydrological and Biogeochemical Controls of Seasonality in Dissolved Organic Matter Delivery to a Blackwater Estuary." Estuaries and Coasts, vol. 42, no. 2, 2019, p. 440. JSTOR website Retrieved 23 July 2025.</ref> in the U.S. states of Mississippi and Louisiana. It forms in Neshoba County, Mississippi from the confluence of Nanih Waiya and Tallahaga creeks,<ref name="prbdd-topog">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> and has a meander length of Template:Convert.<ref name=NHD>U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map, accessed June 13, 2011</ref> The lower part of the river forms part of the boundary between Mississippi and Louisiana.
The river watershed contains large areas of bottomland hardwood swamp and cypress swamp, providing habitat for many species of wildlife, including sturgeon and black bears. As recently as 2008, the endangered Ivory-billed woodpecker was reportedly sighted here.<ref name="collins2017">Template:Cite journal</ref> The mouth of the river creates important marsh habitat along salinity gradients, which has been the subject of many scientific studies.<ref>Template:Cite journal</ref><ref>Template:Cite journal</ref> It is considered to be one of the most critical areas of natural habitat remaining in Louisiana.
Mississippi's capital and largest city, Jackson, is located along the upper reaches of the river. Most of the towns along the river, starting with Philadelphia, Mississippi in the north, are within the boundaries of that state.
Tributaries and hydrology
The Yockanookany and Strong rivers are tributaries on the upper section of the river north of Jackson: the Lobutcha, Tuscolameta, and Pelahatchie creeks also feed in as tributaries in this region.<ref>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</ref> In 1924 the Tuscolameta Creek received 24-mile channelization and Yockanookany River received a 36-mile canal, which was completed in 1928.<ref>Dunbar, J.B. and Coulters, F.J. (1988). Geomorphic investigation of the Shoccoe Dam Project Area / (Record no. 14869). Vicksburg, Miss.: Geotechnical Laboratory, U.S. Army Engineer Waterways Experiment Station, p. 51.</ref>
Northeast of Jackson, the Ross Barnett Reservoir was 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, contributing to the greater discharge of the Bogue Chitto as noted below.<ref>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.</ref>
The Bogue Chitto River is a major tributary on the lower section. The Bogue Chitto's mean low-water discharge to the lower river is nearly six times that of the mean low-water discharge of the Pearl River at Jackson, Mississippi, according to a 1936 government report of the Mississippi Planning Commission.<ref>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.</ref> West of Picayune, about Template:Convert above the mouth, the river forks.<ref name="usgs">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
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.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The West Pearl River flows into The Rigolets, thence into Lake Borgne.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Both discharges eventually reach the Gulf of Mexico. The Pearl River serves as the Template:Convert boundary between Mississippi and Louisiana<ref name=NHD/> 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.<ref>Savanna Street Wastewater Treatment Plant, Risk Management Plan Template:Webarchive, Executive Summary - 2012. Accessed July 19, 2014</ref> which lies about Template:Convert from the mouth of the river. The river below Jackson has historically suffered from pollution<ref>United States, Conference on interstate pollution of the Pearl River (Louisiana-Mississippi), New Orleans, Louisiana, October 22, 1963. [New Orleans, Louisiana]: [Dept. of Health, Education and Welfare, United States]. 1963.</ref> from municipal and industrial sources, however the waters are home to the ringed sawback turtle.<ref>Gaillard, Daniel L., et al. "High Connectivity Observed in Populations of Ringed Sawbacks, Graptemys Oculifera, in the Pearl and Bogue Chitto Rivers Using Six Microsatellite Loci." Copeia, vol. 103, no. 4, 2015, pp. 1075–85. JSTOR website Retrieved 23 July 2025.</ref>
Towns on the river
The following towns (in order, north to south) developed on or near the Pearl River:
- Philadelphia, Mississippi
- Pearl River, Mississippi - named after the river.
- Carthage, Mississippi
- Jackson, Mississippi
- Flowood, Mississippi
- Pearl, Mississippi - named after the river.
- Georgetown, Mississippi
- Rockport, Mississippi
- Monticello, Mississippi
- Columbia, Mississippi
- Bogalusa, Louisiana
- Picayune, Mississippi
- Pearlington, Mississippi - named after the river.
- Pearl River, Louisiana - named after the river.
Navigation
The lower river was navigable from Brashear's Stand on the Natchez Trace to the mouth.<ref>Yancey M. Quinn, Jr. "Jackson's Military Road". 41. (November 1979). Journal of Mississippi History. p. 340.</ref> For the year 1827 the enrolled and licensed tonnage for Pearl River shipping was 750 tons.<ref>The American Annual Register for the years 1827-1829. (1830). New York: E. & G.W. Blunt. p. 593.</ref> The customhouse at Pearl River which was ten miles inland at the small town of Pearlington, Mississippi was later changed,<ref>State of Mississippi. (1844). Laws of the State of Mississippi. Jackson: C.M. Price and S. Rohrer. pp. 371-2 Retrieved 27 January 2016. Google Books website</ref> but in 1904 the district reported a total of 358 vessels and 19,869 tons.<ref>United States. Dept. of Commerce. Bureau of Navigation. (1904). Annual Report of the Commissioner of Navigation. Washington, DC: Government Printing Office. p.337</ref> The U.S. Army Corps of Engineers has undertaken three significant navigation projects in the Pearl River Basin. In 1880, Congress authorized a Template:Convert 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.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> 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 was designed in 2003 to help fish navigate over one of the sills, but was never constructed.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Environmental groups propose further work to mitigate the effects of the navigation project.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Building dams, canals, levees and water control structures is known to have highly negative effects on wetlands and the ecological services they provide.<ref>Middleton, B. A. (ed.) (2002). Flood Pulsing in Wetlands: Restoring the Natural Hydrological Balance. Wiley, New York.</ref><ref>Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. 978-0-521-51940-3</ref> Increasingly, these artificial structures are being removed to allow natural river activities to resume.<ref>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.</ref> 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.<ref>United States Geological Survey. Suspended-Sediment Database Daily Values of Suspended Sediment and Ancillary Data. Introduction of Sediment Data Histograms. https://co.water.usgs.gov/sediment/images/la1.gif</ref>
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.<ref>Template:Cite journal</ref><ref>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.</ref> As one recent example, Hurricane Katrina on August 29, 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.<ref>Template:Cite news</ref> 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.<ref>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, Template:ISBN</ref> 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.Template:Citation needed
History
Following the Louisiana Purchase a number of houses were built on the East Pearl River; historians speculate when Thomas Jefferson outlawed the slave trade in the Orleans Territory, slave traders moved to Spanish-controlled Pearl, the next major navigable river east of the U.S.-controlled Mississippi.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
As of 1812, the land between the Pearl River and the Perdido River below the 31st parallel was legally transferred to the United States from Spain.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
See also
- List of rivers of Louisiana
- List of rivers of Mississippi
- 1979 Easter flood
- South Atlantic-Gulf Water Resource Region
References
Further reading
- Keddy, P.A. 2008. Water, Earth, Fire: Louisiana's Natural Heritage. Xlibris, Philadelphia. 229 p. Figure 6.1. Template:ISBN (Self-published)
External links
Template:Sister project Template:NSRW Poster
- Template:GNIS
- Heinrich, P. V., 2005, Contrasting Pleistocene and Holocene Fluvial Systems of the Lower Pearl River, Louisiana and Mississippi, USA. Geological Society of America Abstracts with Programs, Vol. 37, No. 2, p. 41.
- Heinrich, P. V., 2006, Pleistocene and Holocene Fluvial Systems of the Lower Pearl River, Mississippi and Louisiana, USA. Gulf Coast Association of Geological Societies Transactions. vol. 56, pp. 267–278. (Contains geologic map of Lower Pearl River Valley)
- Heinrich, P. V., R. P. McCulloh, and J. Snead, 2007, Bogalusa 30 x 60 minute geologic quadrangle. Louisiana Geological Survey, Baton Rouge, Louisiana.
- Heinrich, P. V., R. P. McCulloh, and J. Snead, 2004, Gulfport 30 x 60 minute geologic quadrangle. Louisiana Geological Survey, Baton Rouge, Louisiana.
- Pages with broken file links
- Pearl River (Mississippi–Louisiana)
- Rivers of Louisiana
- Rivers of Mississippi
- Borders of Mississippi
- Borders of Louisiana
- Rivers of St. Tammany Parish, Louisiana
- Rivers of Neshoba County, Mississippi
- Rivers of Leake County, Mississippi
- Rivers of Hinds County, Mississippi
- Rivers of Rankin County, Mississippi
- Rivers of Copiah County, Mississippi
- Rivers of Lawrence County, Mississippi
- Bodies of water of Marion County, Mississippi
- Rivers of Washington Parish, Louisiana
- Rivers of Pearl River County, Mississippi
- Rivers of Hancock County, Mississippi
- Drainage basins of the Gulf of Mexico