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French Broad Watershed EarthCache

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Geocaching HQ Admin: It has now been over 30 days since Geocaching HQ submitted the disabled log below and, unfortunately, the cache owner has not posted an Owner maintenance log and re-enabled this geocache. As a result, we are now archiving this cache page.

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Hidden : 4/6/2009
Difficulty:
1 out of 5
Terrain:
1 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Handicapped accessible-all areas paved or concrete at the overlook.



Douglas Dam
Douglas Dam


The above coordinates will take you to a shelter overlooking Douglas Dam. The area has parking, bathrooms and picnic area. The water falling on the mountain side not only forms branches and creeks but is fast moving and causes erosion. This erosion carries soil and other material from the mountain side and deposits it on the valley floor. The water cuts a channel in the valley floor forming a river. This produces a relatively flat area with a large water supply which is greatly prized by humans. The same process is occurring on the other side of the mountain creating a different watershed.

Each watershed has its own characteristics. Some watersheds are very large like the Mississippi basin which includes many smaller watersheds. Generally small watersheds combine into progressively larger watersheds until they empty into the ocean. Watersheds have boundaries which are ridges or mountains which separate one watershed from another. Terrain is also important. The steeper the watershed is determines how fast the water flows and how much erosion occurs. Soil type is another important factor. Sandy soil soaks up water and reduces surface runoff. Clay is tighter and soaks up less water increasing runoff and erosion.

In an area where the boundaries are close together a dam may be built. At the above coordinates the boundaries are close enough to allow the construction of Douglas Dam across the French Broad River.

The French Broad flows through the Appalachian Mountains which are the oldest mountains in the world. The Appalachian Mountains were old before the Rockies were formed and the French Broad is a very old river. It is so old it is practically devoid of fossils. It is actually the third oldest river in the world. Only the Nile in Egypt and the New River in West Virginia are older.

The French Broad begins near Rosman, North Carolina and flows 116 miles through North Carolina into Tennessee. The Tennessee section travels 102 miles until it meets the Holston River just east of Knoxville. Where these two rivers meet it becomes the Tennessee River and a new watershed.

Douglas Dam has a long and interesting history and shows an important use of the French Broad watershed. In 1933 the federal government initiated a golden era of dam construction in the United States, a wave of construction that included the Grand Coulee Dam and the Hoover Dam. The same year the Roosevelt administration established the Tennessee Valley Authority (TVA) to provide much needed hydroelectric energy to the Tennessee Valley area.

During World War II electrical power was needed for national defense purposes, specifically for the Manhattan Project atomic weapons plants in Oak Ridge TN. The Manhattan Project resulted in the development of the first nuclear weapons, and the first-ever nuclear detonation, at the Trinity test of July 16, 1945.

In 1941 President Roosevelt asked Congress to approve funding for Douglas Dam in east Tennessee. After the attack on Pearl Harbor funding was quickly approved and the dam was built as a rush project. Douglas Dam was built in 12 months and 17 days.

According to TVA "the construction of Douglas set a world record for project of equivalent size." TVA directs operations of more than 50 dams in parts of Alabama, Virginia, Kentucky, Georgia, North Carolina, Mississippi and Tennessee. Tennessee, in the East South Central region of the United States, lies between the Mississippi River on the west and the backbone of the Blue Ridge province of the Appalachian Mountains on the east. The French Broad river in the southeastern United States, rising in western North Caroline near the foot of the Blue Ridge Mountains. It flows north past Asheville and then northwest into eastern Tennessee, where it joining the Holston River near Knoxville to form the Tennessee River. The total length of the French Broad River is 250 miles. The Tennessee River, is a tributary of the Ohio River. The Tennessee River is formed by the confluence of the Holston and French Broad rivers, just east of Knoxville, TN. It flows 652 mile in a great U shape, south into Alabama, then turning north to pass through western Tennessee and Kentucky, where it joins the Ohio River near Paducah. The river has a drainage basin of some 39,000 miles Since the establishment of the TVA in 1933, the river has been extensively dammed for navigation, flood control and power production.

Douglas Dam is a hydroelectric power generation facility consisting of 4 electric generation units with combined production capacity of 165,600 kW. kW is a measure of power - kilowatt. The electrical generator is a device that converts mechanical energy to electrical energy, generally using electromagnetic induction.

In addition to power generation, a secondary purpose of Douglas Dam is flood control of the French Broad River. The Douglas reservoir extends 43 miles upriver from the dam through the foothills of the Great Smoky Mountains. Douglas Lake has over 513 miles of shoreline and has a water surface of approximately 30,000 acres. Flooding storage capacity is 1,081,000 feet of water. Under normal conditions, Douglas stores spring rainwater for the release during the dry summer and fall months to maintain adequate depth for navigation on the Tennessee River and to generate electricity. Water levels begin dropping in the late summer to provide space for the next spring's rain. The water level in Douglas Reservoir varies about 41 feet in a normal year.

One problem encountered by dams involves the natural processes of erosion and sediment transport. Erosion occurs naturally in the environment when water transports solids like sediments, soil, and rock. This affects the water on both the upstream and downstream side of the dam.

All dams and reservoirs trap sediments above the dam. These sediments, especially gravel and cobble, collect behind the dam. This buildup of sediments will fill the reservoir over time. Some dams may use low level outlets to combat this problem.

Below the dam water carries away the easily erodible materials and this changes the streambed. The streambed is said to be armored with rocks. The effect tends to make the streambed deeper and narrower. The river tends to become a straight single channel.

As far as Ecological Impacts - one of the issues of hydroelectric power generation is a reduction of dissolved oxygen in the dam tailwaters. Three systems are used at Douglas Dam to improve oxygenation.

1. Turbine venting - injection of oxygen at the turbines.

2. Surface water pumps - pumps that push surface water downward to the turbines.

3. Water pulsing - release of water through turbines to maintain some water flow at all times.

The reservoir remains an integral unit in the overall water control system in the Tennessee Valley. The water used to generate power at Douglas is used again and again at the nine TVA hydroelectric plants located along the Tennessee River from Knoxville to Paducah, KY.

Douglas Lake is a popular recreational destination for up to 2 million visitors a year. Primary uses are fishing, boating, water skiing, camping, hiking and wildlife viewing. Birdwatchers enjoy the fall migration of shore birds, wading birds and other waterfowl that flock to Douglas from late July to early October. The birds rest and feed in the muddy shoreline and areas of shallow water exposed as the level of the reservoir is lowered to prevent spring flooding downstream. In addition to a number of private campgrounds, TVA maintains the Douglas Dam Headwater Campground and the Douglas Dam Tailwater Campground for public use.

The above coordinates will take you to a shelter overlooking Douglas Dam. The area has parking, bathrooms and picnic area.

To claim credit for the cache find, you must do the following:

Take a picture of yourself with your GPSer and the Dam visible in the background. Post this picture with your log.

Then email me with the answers to the following questions. This information can be obtained from the information boards at the overlook.

1. What is the Dam height?

2. What is the Dam Length?

3. What are the 4 TN Valley Watershed Visitors Centers?

Handicapped accessible with restrooms, vending machines, parking and picnic areas.

Additional Hints (No hints available.)