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Cane Run Watershed EarthCache

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Difficulty:
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Cane Run Watershed drains northern Lexington from New Circle Road through Lexmark and UK's Cold Stream Farm, past the Kentucky Horse Park. Underground elements of the watershed flow to Royal Spring in Georgetown with surface flows entering North Elkhorn Creek downstream of Great Crossing. The watershed involves both urban and rural landscapes and serves as a water supply for our homes, farms and wildlife.

Cane Run has been selected by the State Watershed Framework Process as one of five priority watersheds in Kentucky for restoration and management. Cane Run is a showcase for watershed improvements.

Cane Run Creek Watershed is located in the southern part of Scott County and the north/central part of Fayette County. The actual basin is comprised of 26,186 acres and is situated in the Outer Bluegrass Hills of the Bluegrass Physiographic Region. Cane Run Creek flows north/west a distance of 17.4 miles to its confluence with North Elkhorn Creek. Photobucket

A watershed is a drainage basin. It’s an extent of land where water from rain or snow melt drains downhill into a body of water, such as a river, lake, reservoir, estuary, wetland, sea or ocean. The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from which water drains into those channels, and is separated from adjacent basins by a drainage divide.

The drainage basin acts like a funnel, collecting all the water within the area covered by the basin and channeling it into a waterway. Each drainage basin is separated topographically from adjacent basins by a geographical barrier such as a ridge, hill or mountain, which is known as a water divide.

Cane Run Watershed is part of a Karst region. A karst region is a special type of landscape that is formed by the dissolution of soluble rocks, including limestone and dolomite. Karst regions contain aquifers that are capable of providing large supplies of water.

More than 25 percent of the world's population either lives on or obtains its water from karst aquifers. In the United States, 20 percent of the land surface is karst and 40 percent of the groundwater used for drinking comes from karst aquifers. Natural features of the landscape such as caves and springs are typical of karst regions. Karst landscapes are often spectacularly scenic areas. Examples include the sinkhole plains and caves of central and eastern Kentucky.

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Common geological characteristics of karst regions that influence human use of its land and water resources include ground subsidence, sinkhole collapse, groundwater contamination, and unpredictable water supply.

Other terms that are used to describe a drainage basin are catchment, catchment area, catchment basin, drainage area, river basin, water basin and watershed.

In the technical sense, a watershed refers to a divide that separates one drainage area from another drainage area. However, in the United States and Canada, the term is often used to mean a drainage basin or catchment area itself. Watersheds drain into other watersheds in a hierarchical form, larger ones breaking into smaller ones or sub-watersheds with the topography determining where the water flows. Photobucket

Understanding geomorphology is essential in understanding how watersheds interconnect. In hydrology, the drainage basin is a logical unit of focus for studying the movement of water within the hydrological cycle, because the majority of water that discharges from the basin outlet originated as precipitation falling on the basin. A portion of the water that enters the groundwater system beneath the drainage basin may flow towards the outlet of another drainage basin because groundwater flow directions do not always match those of their overlying drainage network. Measurement of the discharge of water from a basin may be made by a stream gauge located at the basin's outlet. Rain gauge data is used to measure total precipitation over a drainage basin, and there are different ways to interpret that data. If the gauges are many and evenly distributed over an area of uniform precipitation, using the arithmetic mean method will give good results. In the Thiessen polygon method, the watershed is divided into polygons with the rain gauge in the middle of each polygon assumed to be representative for the rainfall on the area of land included in its polygon. These polygons are made by drawing lines between gauges, then making perpendicular bisectors of those lines form the polygons. The isohyetal method involves contours of equal precipitation are drawn over the gauges on a map. Calculating the area between these curves and adding up the volume of water is time consuming.

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Drainage basins are important elements to consider also in ecology. As water flows over the ground and along rivers it can pick up nutrients, sediment, and pollutants. Like the water, they get transported towards the outlet of the basin, and can affect the ecological processes along the way as well as in the receiving water source.

Modern usage of artificial fertilizers, containing nitrogen, phosphorus, and potassium, has affected the mouths of watersheds. The minerals will be carried by the watershed to the mouth and accumulate there, disturbing the natural mineral balance.

The catchment is the most significant factor determining the amount or likelihood of flooding.

Catchment factors are: topography, shape, size, soil type and land use (paved or roofed areas).

Catchment topography and shape determine the time taken for rain to reach the river, Catchment size, soil type and development determine the amount of water to reach the river.

Topography Topography determines the speed with which the runoff will reach a river, clearly rain that falls in steep mountainous areas will reach the river faster than flat or gently sloping areas.

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Shape Shape will contribute to the speed with which the runoff reaches a river. A long thin catchment will take longer to drain than a circular catchment.

Size Size will help determine the amount of water reaching the river, as the larger the catchment the greater the potential for flooding.

Soil type Soil type will help determine how much water reaches the river. Certain soil types such as sandy soils are very free draining and rainfall on sandy soil is likely to be absorbed by the ground. However, soils containing clay can be almost impermeable and therefore rainfall on clay soils will run off and contribute to flood volumes. After prolonged rainfall even free draining soils can become saturated, meaning that any further rainfall will reach the river rather than being absorbed by the ground.

Land use Land use will contribute to the volume of water reaching the river, in a similar way to clay soils, only faster. Rainfall on roofs, pavements and roads will be collected by rivers with almost no absorption into the groundwater.

Local concern for overall quality of water in Cane Run Creek and the entire Elkhorn Creek Watershed, prompted an Inter-county Consortium to request assistance inventorying resource concerns and promoting programs to protecting the Elkhorn Creek. Developing an ecosystem based assistance plan for the Cane Run Watershed is critical, for the majority of the watershed is the recharge area for Royal Spring. This two county shared watershed is the primary drinking water source for the city of Georgetown.

Currently there is an on going state funded project to clean up and protect the Cane Run watershed. "Cleaning up streams and protecting our natural resources are vitally important to Kentucky and its citizens, and this project represents the kind of stewardship necessary for the long-term interests of this great commonwealth." Photobucket

To get credit for this EC, post a photo of you (I do not accept pictures of just a hand) at the posted coordinates and with Cane Run Watershed marker in the background just like in the picture above and please answer the following questions.

1. Estimate the width of the watershed at the posted coordinates starting from the top of the high ground to the east and to the western high ground.

2. How many watersheds in Kentucky have been selected for restoration and management?

3. Looking at the nearby farm field determine, using your best judgment, what kind of soil do you this water shed is on?

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Cav Scout has earned GSA's highest level

Do not log this EC unless you have answered the questions and have a picture ready to post! Logs with no photo of the actual cacher ( human face included) logging the find or failure to answer questions or negative comments will result in a log deletion without notice. Exceptions will be considered if you contact me first (I realize sometimes we forget our cameras or the batteries die). You must post a photo at the time of logging your find. If your picture is not ready then wait until you have a photo.

Sources of information for the EarthCache quoted from the Kentucky Geology information website. I have used sources available to me by using the library, internet, research, and asking questions to get information for this earth cache. I am by no means a geologist. Like most people I use whats available to me to get geological information just like 99.9 percent of the geocachers who create these great Earth Caches. I enjoy Earth Caches and want people to get out and see what I see every time I go and explore this great place we live in.

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