Skip to main content

Old River Lock & Control Structure (Lettsworth, LA)

 

The Old River Control Structure (ORCS) and its connecting satellite facilities combine to form one of the most impressive flood control complexes in North America. Located along the west bank of the Mississippi River near the confluence with the Red River and Atchafalaya River nearby, this structure system was fundamentally made possible by the Flood Control Act of 1928 that was passed by the United States Congress in the aftermath of the Great Mississippi River Flood of 1927 however a second, less obvious motivation influenced the construction here.

The Mississippi River’s channel has gradually elongated and meandered in the area over the centuries, creating new oxbows and sandbars that made navigation of the river challenging and time-consuming through the steamboat era of the 1800s. This treacherous area of the river known as “Turnbull’s Bend” was where the mouth of the Red River was located that the upriver end of the bend and the Atchafalaya River, then effectively an outflow channel for the Mississippi River, began at the downriver end. An artificial channel was dug in 1831 to enable the river to bypass this bend in the river, which resulted in the southern arm of the former Turnbull’s Bend becoming the new outflow connection to the Atchafalaya River, a setup that gradually led to an ever-increasing amount of water flowing down the former channel, known as the “Old River”, rather than continuing within its natural channel. It is this waterway, a former segment of the Mississippi River, that the Old River Control Structure is named for. 

Through the mix of human intervention and natural evolution, the Mississippi River’s flow gradually diverted more and more into the Atchafalaya River basin over the ensuing decades, ranging from about 10% diversion in 1900 to about 30% by 1950. The U.S. Army Corps of Engineers recognized that in addition to the ever-present flood threat along the river, they concluded that the river was beginning to change course down the Atchafalaya basin, a process that once completed could not be reversed. The response to this dual threat was the construction of the Old River Control Structure system, work on which began in the 1950s. The Low Sill Control Structure and the Overbank Structure were the first two components to enter operation in 1964. The Low Sill Structure is the primary means by which water distribution is regulated, while the Overbank Structure is only used in times of high water levels. The Low Sill Structure helps maintain the 30% diversion rate for Mississippi River flow into the Atchafalaya basin. Situated a few miles south of the main control structures, the Old River Lock was built in 1963 to allow navigation between the lower Mississippi River, and the Red River & Atchafalaya River by way of the Old River channel. 


The Old River Lock is spanned by this bridge along LA Highway 15, a few miles south of the main Old River Control Structure complex

The initial 1960s construction was successful in keeping the Mississippi River at bay, until the spring of 1973 when record flooding inundated the Mississippi Delta, with water levels reaching comparable levels to the Great Flood in 1927. As more water was diverted initially to keep river levels downstream stable, scouring began to occur at the Low Sill Control Structure, threatening its structural integrity. The U.S. Army Corps was able to keep the structure intact by dumping loads of medium-sized stone (or “riprap”) against the downstream side of the structure, preventing its collapse. Had the structure failed, it's believed that the Mississippi River would have permanently changed course that day.

In the aftermath of the near-failure of the original structure, the U.S. Army Corps built the Old River Auxiliary Structure a short distance downriver in the ensuing decade. Made operational in 1986, this structure enables the complex to handle a higher volume of discharge while providing needed redundancy across the system to avoid the overtaxing of any one entity. At the same time, the need for a low-cost energy source for rural northeastern Louisiana led to the construction of the Sidney Murray Hydroelectric Station, made operational in 1990. This power station is unique among hydroelectric power plants in that it relies solely on the Mississippi River’s natural flow and elevation drop through the ORCS, thereby eliminating the seed for a dam & reservoir system. 


The Low Sill Control Structure was built as the main water diversion structure in the ORCS complex and is crossed by LA Highway 15.

From north to south, the five key components of the ORCS are the Murray Hydroelectric Station, the Overbank Structure, the Low Sill Control Structure, the Auxiliary Control Structure, and the Old River Lock & Bridge. All five of these primary structures carry LA Highway 15 as the most direct route between LA Highway 1 near Simmesport and US Highways 84 & 425 in Vidalia. The drive along Highway 15 in this area is a quite interesting experience as most of the highway in the area is built atop the Mississippi River levee. When combined with the unique presence of the control structures, it’s one of my favorite drives in rural Louisiana.

The collective capacity and engineering of the ORCS has helped ensure that the Mississippi River would remain within its artificial banks for the last 60 years. It has become an indispensable location for ensuring the stability of the lower Mississippi River’s flowrate across Louisiana in the event of flooding and has also served as a man-made barrier that has kept the river in its banks by limiting the amount of water diverted out of the river into the Atchafalaya basin. While it is seen as a great example of water management and flood control, there are those who warn that the Mississippi River will not be able to be tamed forever and that one day the river will ultimately win in its gradual diversion into a new main channel along the current Atchafalaya River. If this were ever to happen, the Atchafalaya Basin and the communities along it would become permanently inundated while the Mississippi River across Louisiana would largely dry up, leaving the economic centers of Baton Rouge and New Orleans permanently cut off from the river. Without the river flowing through, the economy of Louisiana would collapse, without any short-term hope of revival. The economic importance of keeping the Mississippi River in its banks is perhaps the single greatest motivation behind the decades of investment made by the federal government since the Great Flood of 1927. Approaching 100 years since that event that changed the way we view the river and its relationship with the cities along it, there are those who argue that time is running out to prepare for the inevitable permanent changing of the mouth of the Mississippi River. It is said that Mother Nature always prevails in the end. Time will tell whether they are right. 

The following photos from my visit to the Old River Lock in February 2023 showcase various vantage points of the lock from ground level nearby. Click on each photo to see a larger version.

The following photos from my February 2023 visit to the Old River Lock showcase the northbound crossing of the lock & bridge on LA Highway 15. Click on each photo to see a larger version.

The following photos from my February 2023 visit to the Old River Lock showcase the southbound crossing of the lock & bridge on LA Highway 15. Click on each photo to see a larger version.

The following photos from my visit to the Old River Control Structure in February 2023 showcase various vantage points of the auxiliary control structure at the south end of the complex from ground level nearby. Click on each photo to see a larger version.

The following photos from my February 2023 visit to the Old River Control Structure showcase the northbound crossing of the structures on LA Highway 15. Click on each photo to see a larger version.

The following photos from my February 2023 visit to the Old River Lock showcase the southbound crossing of the structures on LA Highway 15. Click on each photo to see a larger version.

Dashcam video of the northbound drive over the Old River Lock & Bridge on LA Highway 15 was filmed in February 2023 for the 'roadwaywiz' YouTube channel and is available for viewing at the link below:

Dashcam video of the northbound drive over the Old River Control Structure on LA Highway 15 was filmed in February 2023 for the 'roadwaywiz' YouTube channel and is available for viewing at the link below:

Dashcam video of the southbound drive over the Old River Control Structure on LA Highway 15 was filmed in February 2023 for the 'roadwaywiz' YouTube channel and is available for viewing at the link below:

Dashcam video of the southbound drive over the Old River Lock & Bridge on LA Highway 15 was filmed in February 2023 for the 'roadwaywiz' YouTube channel and is available for viewing at the link below:

How To Get There (Old River Lock):

How To Get There (Old River Control Structure):

Bridges, Crossings, and Structures of the Lower Mississippi River
Next Crossing upriver: Natchez-Vidalia Bridge (Natchez, MS)
Next Crossing downriver: John James Audubon Bridge (New Roads, LA)
Nearby Flood Control Structure: Morganza Control Structure (Morganza, LA)
Return to the Bridges of the Lower Mississippi River Home Page
__________________________________________________

Comments

Popular posts from this blog

I-40 rockslide uncovers old debates on highway

The Asheville Citizen-Times continues to do a great job covering all the angles of the Interstate 40 Haywood County rock slide. An article in Sunday's edition provides a strong historical perspective on how the Pigeon River routing of Interstate 40 came about. And perhaps most strikingly, in an article that ran just prior to the highway's opening in the fall of 1968, how engineers from both Tennessee and North Carolina warned "...that slides would probably be a major problem along the route for many years." On February 12, 1969, not long after the Interstate opened, the first rock slide that would close I-40 occurred. Like many other Interstates within North Carolina, Interstate 40 through the mountains has a history prior to formation of the Interstate Highway System and was also a heated political battle between local communities. The discussion for a road that would eventually become Interstate 40 dates back to the 1940's as the idea for interregional high

Interstate 210 the Foothill Freeway

The combined Interstate 210/California State Route 210 corridor of the Foothill Freeway is approximately 85.31-miles.  The Interstate 210/California State Route 210 corridor begins at Interstate 5 at the northern outskirts of Los Angeles and travels east to Interstate 10 in Redlands of San Bernardino County.  Interstate 210 is presently signed on the 44.9-mile segment of the Foothill Freeway between Interstate 5 and California State Route 57.  California State Route 210 makes up the remaining 40.41 miles of the Foothill Freeway east to Interstate 10.  Interstate 210 is still classified by the Federal Highway Administration as existing on what is now signed as California State Route 57 from San Dimas south to Interstate 10.  The focus of this blog will mostly be on the history of Interstate 210 segment of the Foothill Freeway.   Part 1; the history of Interstate 210 and California State Route 210 Interstate 210 (I-210) was approved as a chargeable Interstate during September of

White Rock Road; the historic highway corridor serving Mariposa County since the 1850s

White Rock Road is a twenty-eight-mile-long highway corridor which begins at the Chowchilla River in Merced County and ends at Old Highway 18 in Mariposa County near the town site of Bridgeport.  The portion of White Rock Road between the Merced County and Mariposa County line to Bridgeport (via the town site of White Rock) is one of the oldest continuously used highway corridors in California.  Once known as the "Mariposa River Road" the corridor was developed in the 1850s as one of the two primary highways to the mining communities of Mariposa County.   White Rock Road was bypassed in 1918 when Legislative Route Number 18 was completed between Merced and Mariposa.  The corridor was for time known as Mariposa and Le Grand Road prior to the construction of Mariposa Creek Dam (formerly Mariposa River) in 1948.  Following construction of the dam the roadway took the name it has now and was extended through Merced County to the Chowchilla River.  Much of modern White Rock Road i