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Guntersville Dam EarthCache

Hidden : 8/26/2008
Difficulty:
3 out of 5
Terrain:
3.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:


HYDROLOGIC MODIFICATIONS

Guntersville Dam

The following cache will bring you to the Southern side of Guntersville Dam. Here you will find a man made Hydrologic Modification.

Whether you notice it or not, water is continuously on the move all around us. It’s falling to the land in the form of precipitation. It’s moving across landscapes making its way to streams. Streams are running to rivers and rivers are running to oceans. Water is the ultimate recycled element thanks to the hydrologic cycle, which constantly moves water from the atmosphere–down to the planet’s surface and then back into the atmosphere. When built the Guntersville Dam site was chosen for the solid bedrock below. After creating a new channel for the river to flow while the dam was under construction, the site was excavated of all top soil, down to the limestone bedrock that would give the dam the strength it would need to withstand the flood waters that raged through this valley. Damming the river to control these floods, has for the time, slowed the rivers natural ability to meander through the valley below the dam and opening up the flood plain below for agricultural development. The main area subject to these floods is the Lacey Springs area south of Huntsville. Looking at a aerial photo, you can see evidence of where the river once flowed.


Visual evidence of the land shaping powers of water.


Before human modifications, water "percolates" through many different elements, sand and dirt, rocky and grassy areas, before reaching waterways like creeks, streams and rivers. Each of these, help filter out pollutants, sometimes they act as holding areas, creating standing water waiting to go through the system. Man has since come along and made hydrologic modifications, working around this natural flow, and forcing water more directly into waterways, creating a large reservoir, Guntersville Lake. Depending on Rain fall, the amount of water passing over the dam will vary. All so if the turbines are on the water flow here will change from day to day, in an attempt to control flooding both up river and down. Water will still have its way and each day continues to chance the face of our Earth.

Guntersville Dam was part of President Franklin Delano Roosevelt's New Deal project, the Tennessee Valley Authority. Construction started in 1935 and was completed in 1939.Guntersville lake now provides almost 890 miles of shoreline and 67,900 acres of water surface. The dam itself is 94 feet high and stretches 3,979 feet across the Tennessee River. The Dam has two locks to handle commercial shipping and recreational boating. The larger of Guntersville’s two locks was built in 1965 to handle the growing river traffic. Guntersville lake has a flood-storage capacity of 162,000 acre-feet. The generating capacity of Guntersville is 140,400 kilowatts of electricity.

The building of this dam not only brought precious jobs to the area in the 1930's, it also brought electricity and the end of flooding in the Tennessee Valley. It also brought with it numerous recreational opportunities, including boating on the river and lake, fishing, hiking, camping and many other outdoor activities, forever changing the landscape in this region of Alabama.




** Note Since 911, security is much stiffer around all dams. Several areas are now off limits. So please be aware and observe any No trespassing sings. As a whole TVA Land is Public. The TVA Police are aware of this cache and still may question you if they see you. So don’t be surprised. If there is an issue, Captain Patterson on the TVA Police does know about this Earth Cache.




Meander From Wikipedia, the free encyclopedia

A hypothetical stream bed following a tilted valley. The maximum gradient is along the down-valley axis represented by a hypothetical straight channel. Meanders develop, which lengthen the course of the stream, decreasing the gradient.

A meander in general is a bend in a sinuous watercourse, also known as an oxbow loop, or simply an oxbow. A stream of any volume may assume a meandering course, alternatively eroding sediments from the outside of a bend and depositing them on the inside. The result is a snaking pattern as the stream meanders back and forth across its down-valley axis. When a meander gets cut off from the main stream, an oxbow lake is formed.


To log this cache, you will have to complete a few requirements. All requirements must be done with in 14 days of logging or it will be deleted.
1) Take a picture of yourself or your geocaching group with the dam in the background.
2) Calculate the flow rate in "Feet Per Second" for Tennessee River at this location. This may be done by measuring a distance along each of the rivers banks, floating an object from your starting point to the ending point, and recording the time it takes the object to float the distance. Once the "Distance" and "Time" are determined, calculate the "Feet Per Second".






Additional Hints (No hints available.)