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Hales Bar Dam

1913 establishments in TennesseeBuildings and structures in Marion County, TennesseeDams completed in 1913Dams in TennesseeDams on the Tennessee River
Industrial buildings and structures on the National Register of Historic Places in TennesseeNational Register of Historic Places in Marion County, TennesseeTennessee Valley Authority dams
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Tylerholcombhalesbar

Hales Bar Dam was a hydroelectric dam once located on the Tennessee River in Marion County, Tennessee, United States. The Chattanooga and Tennessee River Power Company began building the dam on October 17, 1905, and completed it on November 11, 1913, making Hales Bar one of the first major multipurpose dams and one of the first major dams to be built across a navigable channel in the United States. It began operation on November 13, 1913. On August 15, 1939, the Tennessee Valley Authority, which had been established by the President Franklin D. Roosevelt administration to develop and regulate flood control and hydropower in the Valley, assumed control of Hales Bar Dam after purchasing TEPCO's assets through Eminent Domain. It had conducted a lengthy court battle that went all the way to the US Supreme Court. The TVA worked for two decades trying to fix a leakage problem that had plagued Hales Bar since its construction. But, after continued leakage and determining that expanding the dam's navigation lock would be too expensive, TVA decided to replace the dam. It built Nickajack Dam 6 miles (9.7 km) downstream. Hales Bar Dam ceased operation on December 14, 1967.

Excerpt from the Wikipedia article Hales Bar Dam (License: CC BY-SA 3.0, Authors, Images).

Hales Bar Dam
Serodino Road,

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Latitude Longitude
N 35.046666666667 ° E -85.539444444444 °
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Hale's Bar

Serodino Road
37340
Tennessee, United States
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Marion Memorial Bridge
Marion Memorial Bridge

The Marion Memorial Bridge was a 4-span metal truss bridge that formerly carried U.S. Route 41 in Marion County, Tennessee over the Tennessee River and Nickajack Lake. It was built in 1929. The main span was 369 feet (112 m), and the bridge had a total length of 1,870 feet (570 m). The bridge was listed on the National Register of Historic Places on October 25, 2007. The bridge featured an unusual truss configuration that is a hybrid of the Parker and K-Truss configurations. The bridge was replaced by a new concrete and box girder span that opened in November 2014, slightly delayed from its target completion date of August 2013 by conditions encountered in the construction of the replacement bridge footings. Since the construction of the new bridge's footings involved blasting within 30 feet (9.1 m) of the Marion Memorial Bridge, state officials closed the bridge to vehicle and pedestrian traffic on January 9, 2012, with traffic being re-routed to the Interstate 24 bridge south of the span. The metal trusses of the bridge were demolished and removed by June 2015. The bridge was delisted from the National Register in June 2016. Some people in the community expressed the desire to preserve the bridge in some way. Tennessee Department of Transportation officials said the bridge was costly to maintain, citing as an example the repainting cost of $1 million.This bridge was built before the construction Nickajack Dam, a few miles downriver. The higher mean pool of the new reservoir necessitated raising the bridge from its original height. A bridge of similar design in Meigs County, Tennessee, that carried Tennessee Highway 58 across the Hiwassee River was imploded in November 2007, along with another similar bridge that carried Highway 58 over the Tennessee River in Roane County.

Sequatchie Valley
Sequatchie Valley

Sequatchie Valley is a relatively long and narrow valley in the U.S. state of Tennessee and, in some definitions, Alabama. It is generally considered to be part of the Cumberland Plateau region of the Appalachian Mountains; it was probably formed by erosion of a compression anticline, rather than rifting process as had been formerly theorized. The Sequatchie River drains the valley in Tennessee, flowing south to southwest from the southern part of Cumberland County, Tennessee to the Tennessee River near the Alabama border. Geologically, the Sequatchie Valley continues south of the Tennessee River into central Alabama. The Tennessee River flows through the Alabama portion of the valley to the vicinity of Guntersville, Alabama. The valley continues south of Guntersville, where it is called Browns Valley, drained by Browns Creek (Thornbury 1965:148). Although this whole valley is geologically the same, the name Sequatchie is commonly used only for the Tennessee portion of the valley, through which the Sequatchie River flows. A distinctive feature of the Sequatchie Valley is its straightness. From its northern end to its geological southern end at Browns Valley, the valley is almost perfectly straight. It is over 150 miles (240 km) long in the geologic sense and about 65 miles (105 km) long as the valley of the Sequatchie River. Its width is about 3–5 miles (5–8 km). The valley is bounded on either side by escarpments of the Cumberland Plateau. The portion of the plateau east of the valley is relatively narrow and known as Walden Ridge in Tennessee. To the west the plateau is simply called the Cumberland Plateau. In Bledsoe County, Tennessee a section of the west side escarpment is called Little Mountain, which also marks the Tennessee Valley Divide. In Alabama the plateau to the east of the valley is called Sand Mountain, while that to the west is Gunters Mountain. At its northern end, the Sequatchie Valley is marked by a more mountainous portion of the Cumberland Plateau known as the Crab Orchard Mountains. Between the main Crab Orchard Mountains and the Sequatchie Valley there is another valley, called Grassy Cove, located several miles north of Sequatchie Valley. Grassy Cove is a karst valley which, through underground erosion, should eventually become part of Sequatchie Valley (Thornbury 1965:149). Another, smaller karst valley, Bat Town Cove, is forming northeast of Grassy Cove, which may also grow and eventually become part of Sequatchie Valley. The Tennessee section of Sequatchie Valley contains the towns of Pikeville, Dunlap, Whitwell, Jasper, and, on the Tennessee River, South Pittsburg. Towns in the Alabama portion of the geologic valley include Bridgeport, Scottsboro, Guntersville, and, around the southern end, Blountsville.

WTNW

WTNW (820 AM, "Music Radio 820") was a radio station broadcasting a variety hits format, licensed to Jasper, Tennessee, United States. The station originally signed-on the air in 1986 playing an adult contemporary format as WAPO, taking the former call-letters of what is now WGOW-AM in Chattanooga. The station switched to an all gospel format around 1990, before changing owners and call-letters in 1993. The station featured weekday programming, the John & Heidi Show mornings with hosts John and Heidi Small from 6:00am to 10:00am Central Time. Maddy Jones and Maddy in the Midday from 10:00am until 2:00pm, and The B-Side With Joshua Wayne afternoons from 2:00pm until 6:00pm. Logan Carmichael covered news and local events and could also be heard on weekends, and the station featured its own locally produced and hosted bluegrass show, Cold Mountain Bluegrass, hosted by Kyle Holland on Saturday mornings from 8:00am–10:00am Central Time. Sundays were dedicated to a variety of Southern gospel and various religious paid programming. WTNW was also the flagship station for Marion County High School Warriors football broadcasts each fall. WTNW was owned by Shelton Broadcasting System.On Saturday, December 31, 2016, a fire destroyed the historic house at 4306 Main Street in Jasper which housed the transmitting equipment, offices, and studios of WTNW.The station filed for authorization with the FCC to go silent for an undetermined time, which was granted on January 30, 2017. The FCC cancelled WTNW's license on March 12, 2019, due to the station having been silent since January 1, 2017.