The Savannah River is a major river in the Southeastern United States, forming most of the border between the states of Georgia and South Carolina. The river flows from the Appalachian Mountains to the Atlantic Ocean, for a total distance of about 301 miles (484 km).[4] The Savannah was formed by the confluence of the Tugaloo River and the Seneca River. Today this confluence is part of Lake Hartwell, a man-made reservoir constructed between 1955 and 1964.
| Savannah River Tugaloo River | |
|---|---|
 Savannah River at Augusta, with the Augusta Canal running alongside | |
 Map of the Savannah River watershed | |
| Location | |
| Country | United States |
| State | North Carolina, South Carolina, Georgia |
| Cities | Savannah, Augusta |
| Physical characteristics | |
| Source | Lake Hartwell |
| • coordinates | 34°26′37″N 82°51′22″W / 34.44361°N 82.85611°W[1] |
| • elevation | 655 ft (200 m)[2] |
| Mouth | Atlantic Ocean |
• location | Tybee Roads |
• coordinates | 32°2′16″N 80°51′0″W / 32.03778°N 80.85000°W[1] |
• elevation | 0 ft (0 m)[2] |
| Length | 301 mi (484 km) |
| Basin size | 9,850 sq mi (25,500 km2)[3] |
| Discharge | |
| • location | near Clyo, GA[3] |
| • average | 11,720 cu ft/s (332 m3/s)[3] |
| Basin features | |
| Tributaries | |
| • left | Seneca River |
| • right | Tugaloo River |
 | |
Two tributaries of the Savannah, the Tugaloo River and the Chattooga River, form Georgia's northernmost border with South Carolina. A tributary of the Tugaloo, the Tallulah River, forms the northwest branch of the Savannah and features the two-mile-long (3 km) and almost 1,000-foot-deep (300 m) Tallulah Gorge. The Savannah River's drainage basin extends into the southeastern Appalachian Mountains and the state of North Carolina, and is bounded by the Eastern Continental Divide.
Two major cities in Georgia are located along the Savannah River: Savannah and Augusta. Founded in 1733 and 1736, respectively, they were nuclei of early English settlements during the colonial period of American history.
The Savannah River is tidal at the city of Savannah. Downstream from the city, the river broadens into an estuary before flowing into the Atlantic Ocean. The area where the river's estuary meets the ocean is known as Tybee Roads. The U.S. Intracoastal Waterway flows through a section of the Savannah River near the city proper.
Name
editThe name "Savannah" comes from a group of Shawnee who migrated to the Piedmont region in the 1680s. They destroyed the Westo and occupied established Westo lands at the Savannah River's head of navigation on the Fall Line. Present-day Augusta developed near there.[5] These Shawnee were called by several variant names, which all derive from their native name, Ša·wano·ki (literally, "southerners").[6] The local variants included Shawano, Savano, Savana, and Savannah.[7]
Another theory is that the name was derived from the English term "savanna", a kind of tropical grassland, which was borrowed by the English from Spanish sabana and used in the colonial southeast. The Spanish word was borrowed from the Taino word zabana.[8] Other theories interpret the name Savannah to have come from Atlantic coastal tribes, who spoke Algonquian languages. These have similar terms meaning "southerner" or perhaps "salt".[9][10]
Historical and variant names of the Savannah River, as listed by the U.S. Geological Survey, include May River, Westobou River (for the Westo tribe), Kosalu River, Isundiga River, and Girande River, among others.[1]
History
edit_pg101_OCEAN_STEAMSHIP_CO_OF_SAVANNAH,_PIERS_34_AND_35,_NORTH_RIVER.jpg)
Early history
editThe Westo were thought to have migrated from the northeast, pushed out by the more powerful tribes of the Iroquois Confederacy, who had acquired firearms through trade. This migration, beginning in the late 16th century, resulted in the Westo Indians reaching the present area of Augusta, Georgia, in the late 17th century.[citation needed]
The Westo used the river for fishing and water supplies, for transportation, and for trade. They were strong enough to hold off the Spanish colonists making incursions from Spanish Florida. The Carolina Colony needed the Westo alliance during its early years. When Carolinians desired to expand their trade to Charleston, they viewed the Westo tribe as an obstacle. In order to remove the tribe, they sent a group called the Goose Creek Men to arm the Savanna (also known as the Savannah) Indians, a Shawnee tribe, who defeated the Westo in 1680.[citation needed]
Following this, the English colonists renamed the river as the Savannah; it was integral to early development. They founded two major cities on the river during the colonial era: Savannah was established in 1733 as a seaport on the Atlantic Ocean, and Augusta is located where the river crosses the Fall Line of the Piedmont, at the headwaters of the navigable portion of the river downstream to the ocean. The two cities on the Savannah served as Georgia's first two state capitals. In the 19th century, the sandy river channel changed frequently, causing numerous steamboat accidents.
During the American Civil War, President Abraham Lincoln proclaimed a blockade around the Confederate States of America, forcing merchantmen to use specific ports along the coast best suited for this purpose. The harbor at Savannah became one of the busiest ports for blockade runners bringing in supplies for the Confederacy until it was cut off by the reduction of Fort Pulaski and Union capture of Cockspur Island.[11]
The South Carolina-Georgia border was originally defined in the Treaty of Beaufort in 1787, which, among other things, "[reserved] all islands in [the river] to Georgia". Over time, new islands were created. Some, namely the Barnwell islands, are on the South Carolina side of the original line. In 1990, the U.S. Supreme Court decided that the new islands on the South Carolina side of the border belong to South Carolina.[12]
20th century to present
editBetween 1946 and 1985, the U.S. Army Corps of Engineers built three major dams on the Savannah for hydroelectricity, flood control, and navigation. The J. Strom Thurmond Dam (1954), the Hartwell Dam (1962), and the Richard B. Russell Dam (1985) and their reservoirs combine in order to form over 120 miles (190 km) of lakes.[13] In December 1986, an oil spill caused by an oil tanker docked at the port of Savannah resulted in approximately 500,000 US gallons (1,900,000 L) of fuel oil leaking into the river.
During the 1950s, the Savannah River Plant was constructed across 310 square miles of land on the South Carolina bank of the river northeast of Augusta, Georgia, displacing the residents of several small towns near the Savannah River. The site produced plutonium, tritium, and heavy water for the United States Atomic Energy Commission's nuclear weapons program. The facility, now called the Savannah River Site and operated by the U.S. Department of Energy, still plays an important role in the economy of the Augusta metropolitan area. Three of the site's five production reactors as well as its coal power plant discharged waste heat to the Savannah River via Pen Branch, Steel Creek, and Beaver Creek while two reactors discharged heat to the man made PAR Pond on Lower Three Runs Creek.[14] The Savannah River Plant also produced the majority of the Atomic Energy Commission's heavy water supply by processing water from the Savannah River via the Girdler sulfide process.[15] Heavy water was used as the moderator for the site's production reactors. In 1956 Clyde L. Cowan and Frederick Reines first detected neutrinos with an experiment carried out at the Savannah River Plant P-Reactor.
During their operating lifetimes, the Savannah River Plant's reactors significantly elevated the temperatures of several Savannah River tributaries. Since these reactors predate nuclear power generation and were some of the earliest large reactors in the world, this offered unique opportunities for the Savannah River Ecology Laboratory to study the impact of large-scale thermal discharge and other effects of the site's operation. Efforts to remediate the thermal discharge directly to the river, such as the construction of a lake to receive the discharge of L-Reactor [16] and cooling tower to dissipate the discharge of K-Reactor[17] had been recently implemented by the time the reactors were shut down at the end of the Cold War. The Savannah River Site now extracts tritium, but using targets irradiated at the Watts Bar Nuclear Plant in Tennessee, so the heat discharge associated with tritium production is no longer in the Savannah River basin.
The Vogtle Electric Generating Plant was constructed across the river from the Savannah River Plant, with units 1 and 2 completed in mid 1980s and units 3 and 4 completed in the early 2020s. This plant also requires water from the river, but all four units use large natural draft cooling towers to avoid large scale withdrawals or discharge. The McIntosh Combined Cycle Power Plant and Jasper Generating Station are situated further down the Savannah River which provides feed water for the mechanical draft cooling towers for their combined cycle natural gas plants.
Course
editThe Savannah River flows through a variety of climates and ecosystems during its course. It is considered an alluvial river, draining a 10,577-square-mile (27,390 km2) drainage basin and carrying large amounts of sediment to the ocean. At its headwaters in the Blue Ridge Mountains, the climate is quite temperate. The river's tributaries receive a small amount of snow-melt runoff in the winter. The majority of the river's flow through the Piedmont region is dominated by large reservoirs. Below the Fall Line, the river slows and is surrounded by large blackwater bald cypress swamps. Numerous oxbow lakes mark the locations of old river channels, which have shifted course because of earthquakes and silting.
Another prominent feature are the numerous large bluffs that line the river in some locations. Most notable of these is Yamacraw Bluff, the location selected to build the city of Savannah. The river becomes a large estuary at the coast, where fresh- and saltwater mix. River dredging operations to maintain the Port of Savannah have caused the estuary zone to move further upstream than its historical home. This is causing the rare freshwater marshland to be taken over by saltwater spartina marsh.
Tributaries include:
Ecology
editThe Savannah River Basin in the Southeast region of the U.S. has been experiencing environmental change from anthropocentric activities. The Savannah River has the fourth-highest toxic discharge in the country, according to a 2009 report by Environment America.[18] The conversion of the vegetation cover, including the urban growth, agriculture expansion, and deforestation and reforestation take place throughout the basin, especially near the lakes and tributary waters in the middle and lower Savannah Basin. The continuous change of land use such as the conversion of forest areas to other types of land cover and vice versa can significantly lead to increasing threats to the environmental systems of the region.[19]
The river supports a large variety of native and introduced aquatic species:
- Upper section - yellow perch, brook trout, brown trout, rainbow trout, smallmouth bass, largemouth bass, crappie, striped bass, hybrid striped bass, white bass, bluegill, North American river otter, American mink, North American beaver, catfish
- Middle section - largemouth bass, crappie, striped bass, spotted bass, bluegill, redbreast sunfish, catfish, American eel, North American river otter, American mink, North American beaver, shortnose sturgeon, chain pickerel, bowfin, longnose gar, snapping turtles, American alligator, water moccasin
- Lower section, estuary - largemouth bass, crappie, striped bass, spotted bass, bluegill, redbreast sunfish, catfish, American eel, North American river otter, American mink, North American beaver, shortnose sturgeon, Atlantic sturgeon, chain pickerel, bowfin, longnose gar, snapping turtles, American alligator, snakes, red drum, flounder, spotted seatrout, bull shark, tarpon, common bottlenose dolphin, West Indian manatee, diamondback terrapin
The river is one of only four in the southeast with significant populations of Hymenocallis coronaria, the shoals spider-lily. It has three populations in the primary river basin and one each in the tributaries of Stevens Creek in South Carolina and the Broad River in Georgia.[20]
Navigation
editThrough the building of several locks and dams in the first half of the 20th century (such as the New Savannah Bluff Lock and Dam, completed in 1937 during the Great Depression), and upstream reservoirs like Lake Hartwell, the Savannah River was once navigable by freight barges between Augusta, Georgia (on the Fall Line) and the Atlantic Ocean. Maintenance of this channel for commercial shipping ended in 1979, and the one lock below Augusta has been deactivated.[21]
When a large piece of equipment (a deaerator) needed to be delivered to the Vogtle Electric Generating Plant construction site in 2013, the barge travelled upstream from the Port of Savannah only to the Georgia Power's Plant McIntosh site, near Rincon, Georgia; from there, the cargo was moved by a road transporter.[22]
Crossings
editThis is a list of crossings of the Savannah River.
Dams
editSee also
editNotes
edit- ^ a b c "Savannah River". Geographic Names Information System. United States Geological Survey, United States Department of the Interior.
- ^ a b Google Earth elevation for GNIS coordinates.
- ^ a b c Water Resource Data, South Carolina, 2005 Archived March 2, 2017, at the Wayback Machine, USGS, p. 559. Gages farther downriver affected by tides.
- ^ U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map Archived March 29, 2012, at the Wayback Machine, accessed April 26, 2011
- ^ Cashin, Edward J. (1986). Colonial Augusta: "Key of the Indian Countrey". Mercer University Press. p. 4. ISBN 978-0-86554-217-4. Archived from the original on January 2, 2016. Retrieved October 13, 2016.
- ^ "Shawnee", in Webster's Collegiate Dictionary, 11th ed., 1145
- ^ Savannah River Basin Archived September 25, 2011, at the Wayback Machine, Georgia River Network.
- ^ Bright, William (2004). Native American Place names of the United States. University of Oklahoma Press. p. 424. ISBN 978-0-8061-3598-4. Archived from the original on January 2, 2016. Retrieved October 13, 2016.
- ^ Names in South Carolina, Volume 22 Archived March 19, 2012, at the Wayback Machine, Institute for Southern Studies.
- ^ Names in South Carolina, Volume 16 Archived March 19, 2012, at the Wayback Machine, Institute for Southern Studies.
- ^ Wise, 1991 p.24
- ^ Georgia v. South Carolina, 497 U.S. 376, 412 (1990).
- ^ "Army Corps of Engineers J. Strom Thurmond Lake and Dam Hydropower". Archived from the original on December 5, 2009.
- ^ Paller, Michael H.; Saul, Bruce M. (June 1986). Effects of thermal discharges on the distribution and Abundance of adult fishes in the Savannah River and selected tributaries (PDF) (Report). Nuclear Regulatory Commission. Retrieved November 23, 2023.
- ^ Bebbington, B. P.; Thayer, V.R. M. (July 1959). Production of heavy water Savannah River and Dana Plants (PDF) (Report). Atomic Energy Commission. Retrieved November 23, 2023.
- ^ Paller, 1986
- ^ Nuclear Health and Safety: Policy Implications of Funding DOE's K Reactor Cooling Tower Project (Report). Government Accountability Office. September 27, 1989. Retrieved November 23, 2023.
- ^ "Wasting Our Waterways: Toxic Industrial Pollution and the Unfulfilled Promise of the Clean Water Act" (PDF). Environment America. October 21, 2009. Archived from the original on January 11, 2020. Retrieved June 5, 2010.
- ^ Zurqani, Hamdi A.; Post, Christopher J.; Mikhailova, Elena A.; Mark, Schlautman J.; Sharp, Julia L. (March 29, 2018). "Geospatial analysis of land use change in the Savannah River Basin using Google Earth Engine". International Journal of Applied Earth Observation and Geoinformation. 69. Elsevier: 175–185. Bibcode:2018IJAEO..69..175Z. doi:10.1016/j.jag.2017.12.006. S2CID 21686203.
- ^ Markwith, Scott H.; Scanlon, Michael J. (May 11, 2006). "Multiscale analysis of Hymenocallis coronaria (Amaryllidaceae) genetic diversity, genetic structure, and gene movement under the influence of unidirectional stream flow". American Journal of Botany. 94 (2). Botanical Society of America: 151–60. doi:10.3732/ajb.94.2.151. PMID 21642217.
- ^ [1] Archived September 10, 2012, at the Wayback Machine Pavey, Rob. New Plant Vogtle parts could require dredging; Augusta Chronicle; September 3, 2009.
- ^ Massive unit 3 component delivered to Vogtle Archived March 14, 2016, at the Wayback Machine, 2013-02-26
References
edit- Stokes, Thomas, L, The Savannah (Rivers of America Series), Rinehart, 1951
- Wise, Stephen R. (1991). Lifeline of the Confederacy: Blockade Running During the Civil War.
Univ of South Carolina Press. p. 403. Url
External links
edit
- Two Historic Savannah River Ferries historical marker
- . New International Encyclopedia. 1905.