Atchafalaya Basin

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This article is about a wetlands basin. For other uses of the term "Atchafalaya", see Atchafalaya (disambiguation).

The Atchafalaya Basin, or Atchafalaya Swamp, in south central Louisiana is a combination of wetlands and river delta area where the Atchafalaya River and the Gulf of Mexico converge. The Atchafalaya is unique among basins because it has a growing delta system (see illustration) with nearly stable wetlands. [Louisiana Coast]

Contents

1 Geographical features
2 Basin geology

2.1 Degradation of the buffer marshes

3 See also
4 Footnotes
5 External links

Geographical features

The Atchafalaya Basin, the surrounding plain of the river, is filled with bayous, bald cypress swamps, and marshes that give way to more brackish conditions and end in the Spartina grass marshes, near and at where it meets the Gulf of Mexico. It includes the Lower Atchafalaya River, Wax Lake Outlet, Atchafalaya Bay, and the Atchafalaya River and Bayous Chene, Boeuf, and Black navigation channel.

The basin, which susceptible to heavy flooding, is sparsely inhabited. The basin is about 20 miles in width from east to west and 150 miles in length.[Encyclopedia of Cajun Culture] With 595,000 acres, it is the nation’s largest swamp wilderness, containing nationally significant expanses of bottomland hardwoods, swamplands, bayous and back-water lakes. [Audubon Wetlands Campaign]

The few roads that cross it follow the tops of levees. Interstate 10, which crosses the basin on elevated pillars west of Baton Rouge is a continuous 18.2 mile (29,290 meters) bridge.

The Atchafalaya National Wildlife Refuge was established in 1984 to improve plant communities for endangered and declining species of wildlife, waterfowl and migratory birds. [Atchafalaya National Wildlife Refuge]

Basin geology

Geologically, the Atchafalaya has served periodically as the main channel of the Mississippi through the process of delta switching, which has built the extensive delta plain of the river. Since the early 20th century, because of manmade alterations in the channel, the Mississippi has sought to change its main channel to Atchafalaya. By law, a regulated proportion of the water from the Mississippi is diverted into the Atchafalaya at the Old River Control Structure.

For more details on this topic, see [Atchafalaya River].

Degradation of the buffer marshes

The control of the river's floods, along with those of the Mississippi, has become a controversial issue in recent decades. It is now widely suspected that the channeling of the river and subsequent lowering of siltation rates has resulted in severe degradation of the surrounding saltmarsh wetlands as well as widespread submerging of populated and agricultural lands of the bayou country. The US Geological Survey (USGS) reports that over 29 square miles (75 square kilometers) of land is lost to the sea each year.[USGS Fact Sheet: Louisiana Coastal Wetlands: A Resource At Risk]

The coastal salt marshes form a buffer zone protecting the entire coast of Louisiana from the effects of hurricanes in the Gulf of Mexico and dissipating their accompanying storm surges. The marshes depend on replenishment from deposited silt, which is now being deposited over the edge of the continental shelf, due to the artificially canalized flow of the Mississippi. From the 1950s through 1970s, the oil industry dredged deep channels into the marsh so that they could move barges in as work platforms. The edges continued to degrade, until wide shallow channels in the saltmarsh have resulted.[Loss of wetlands from the perspective of Wildfowl Magazine]

The disappearance of the delta country is considered by many environmentalists, as well as by the State of Louisiana, to be one of the most significant ecological threats in the United States. The loss of the delta lands was discussed by author Mike Tidwell in his 2003 book Bayou Farewell: The Rich Life and Tragic Death of Louisiana's Cajun Coast. [Bayou Farewell: The Rich Life and Tragic Death of Louisiana's Cajun Coast]

Footnotes

External links