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Cave Run Lake: A River Runs Through It EarthCache

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Hidden : 4/27/2010
Difficulty:
1 out of 5
Terrain:
1 out of 5

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Geocache Description:

Landowner ermission obtained from US Army Corps of Engineers, Louisville District Cave Run Lake: Anthony Orr, Park Manager 150 Kentucky Hwy 826 Morehead, KY 40351 (606)784-9709


WATERSHEDS: A watershed refers to land that is drained by an interconnected system of rivulets, streams, rivers, lakes, and groundwater. Water from a watershed eventually drains into a common destination. Both rain and snow contribute to the watershed. Watersheds can range in size from just a few square miles to many hundreds, even millions of square miles.

Watersheds are important as habitats for many creatures, and as a source of drinking and recreational water for many communities. Because one watershed can often be connected to another watershed that lies "downstream," the environmental quality of one watershed can affect other watersheds. As more communities rely on watersheds for their drinking water, the preservation of watersheds is becoming more urgent.

To function properly, a watershed needs to be maintained in a fairly undisturbed state, especially near watercourses. This undisturbed habitat helps to keep unwanted pollutants and excess soil and runoff from reaching the water course. The preservation of watershed habitats is recognized as a priority by local, regional, and national governments.

Watershed

Licking River Watershed

FLOODS: Flooding, although it usually carries a negative connotation, is a natural process and is simply the response of a natural system (a river system) to the presence of too much water during an interval of time. When this happens, water must move out of the channel (the bed or deeper part) and out onto the surrounding area, known as the floodplain.

Floods are caused by a variety of factors, both natural and man-made. Some obvious causes of floods are heavy rains, melting snow and ice, and frequent storms within a short time duration. When humans build homes and towns near rivers, the result has been the disastrous consequences of floods. Floods have historically killed more people than any other natural disaster. Because of this, humans have attempted to manage floods using a variety of methods.

ALLUVIUM: One positive result of flooding, or streams leaving their banks, is the deposition of silt, clay, gravel and organic matter in floodplains. This material is called alluvium. Alluvium results in very fertile soils. The Licking River floodplain that is now underwater above the dam was fertile farmland resulting from the deposit of alluvium. Many farmers and residents were displaced when the dam was constructed. Now the dam prevents flooding of land below the dam which also includes fertile alluvial farmland residing in the floodplain of the river.

FLOOD INTERVENTION HAZARD ASSESSMENT: Because of the potential of a flood to destroy life and property, men and women have, for centuries, developed ways to prepare for and fight this natural disaster. One common way to manage floodwaters is to construct dams to stop excess water from inundating dry areas. Another way is to divert floodwaters away from populated areas to planned areas of flood storage. To this end, flood control reservoirs are kept partially empty so that they can catch floodwaters when the need arises. These reservoirs then release the water at a slower rate than would occur under flood conditions; hence, reservoirs give the soil time to absorb the excess water. About one-third of reservoirs in the United States are used for this purpose.

Flood Intervention

HISTORY OF FLOOD CONTROL DAMS: Around 2950-2750 B.C, the ancient Egyptians built the first known dam to exist. The dam was made of rubble masonry walls on the outsides and filled with 100,000 tons of gravel and stone. The dam was not watertight and water flowed through the structure quickly eroding it away.

The second type of dam known to have been built was an earth dam called Nimrod's Dam in Mesopotamia around 2000 BC. Around 100 AD the Romans were the first civilization to use concrete and mortar in their gravity dams. Both of these types of dams were watertight methods of construction.

The evolution of flood control dams is too extensive to cover here, but you get the idea. Mankind has been using dams for flood control a very long time.

CAVE RUN LAKE: So, this Earthcache brings you to Cave Run Lake. A river runs through it. That river is the Licking River. The head (beginning) of the river is in Magoffin County. The mouth of the river empties into the Ohio River across from Cincinnati. Early explorers called the river "Great Salt Creek" because of the many salt licks found along its banks. Indians called it "Nepernine" (salt seeping waters).

Construction of a flood control dam on the river by the Louisville District of the Corps of Engineers began in 1965 and was completed in 1973. The dam was constructed with the primary purpose of flood control, but the resulting lake provides an alluring source of recreation as well.


The dam controls runoff from an 826 square mile drainage area or watershed. Water is held back by the dam and released gradually so that flooding does not occur downstream. There is a good diagram at the posted coordinates showing how this works along with lots of other interesting information. When I was a kid living at Zilpo (upriver from the dam), there were times when we could not go to school because floodwaters came across the road.

I hope you will take time to walk around a bit here to experience and learn more about flood control dams. An "emergency spillway" 650 ft. wide and 23 ft. lower than the top of the dam is located at N 38 06.729 W 83 31.959. This is a safety measure that would prevent water from overtopping the dam.

I also hope that you will consider what the land above the dam was like before it was flooded. Imagine the Licking River flowing through that area and fertile fields in the floodplains where farmers most often grew corn. Imagine all of the streams and rivulets draining rainwater from the land and into the river. In a way, all of that is still there. A lot of it is just underwater now.

Please email answers to the following questions to me to get credit for this Earthcache:


  1. The watershed directly around Cave Run Lake primarily consists of what type of land?
  2. What natural occurrence would have caused flooding in this area?
  3. What type of land did the dam flood in order to provide flood control downstream?
  4. How many river miles is it to the Ohio River from the dam?
  5. Without proper controls, a manmade dam could negatively impact the river downstream. What two mechanisms does the dam incorporate to lessen its effect on temperature and turbulence downstream?

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