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Ensor Sink Natural Area Park Across Drainage Culvert

Ensor Sink Natural Area

a facility of the City of Cookeville
Department of Leisure Services and Public Facilities

Visited June 2002

Click images to zoom in (~100-400 kB each)

View across drainage canal, which flows to left to the sink hole, towards the park with information sign kiosk.

Approximate Location (Yahoo Maps)

Aerial View (At lower right of small image, Terraserver)


Ensor Sink Natural Area Sign 1

Text from Sign Number 1:

Ensor Creek Natural Area was established to preserve the natural beauty of the land surrounding Ensor Sink, to provide recreational opportunities for the community and to educate people about the role of sinkholes and caves in the stormwater drainage of the city.

Ensor Sink is a large sinkhole located in the center of the natural area. See Sign 2 for more information about sinkholes.

This project was funded in part by a grant from the Local Parks and Recreation Fund (LPRF) administered by the Recreation Resources Division, Tennessee Department of Environment and Conservation. This project, which was also funded by the City of Cookeville, is in compliance with Section 504 of the Rehabilitation Act of 1973 (ADA of 1990) and Title VI of the Civil Rights Act of 1964.

DANGER
Beware of flooding


Ensor Sink Natural Area Sink Beyond Fence Rapidly rising water and strong currents make Ensor Sink Natural Area unsafe during heavy rain.

Stay safe. Do not enter the fenced-in area at any time.

Ensor Sink Natural Area was opened to the public in October, 2000.

City Council Members
Charles Womack, Mayor
Richard Grogan, Vice Mayor
Steve Copeland, Councilman
Dwight Henry, Councilman
Harold Jackson, Councilman

Jim Shipley, City Manager

Understanding sinkholes

Ensor Sink Natural Area Sign 2 Text from Sign Number 2:

About Ensor Sink

Ensor Sink is a sinkhole with a large opening where Breedings Mill Branch canal drains into an inaccessible cave. The opening is called "swallet," a place where water is "swallowed" into the earth.

Except during periods of heavy rain, it does not look like water is draining into the swallet. That is because the water that flows down the Breedings Mill Branch canal and under the Clover Hill Drive Bridge normally sinks into loose rocks a short distance beyond the concrete canal. The water then flows underground until it joins the permanent pool of water just inside the Ensor Sink swallet. During heavy rain when there is a much larger volume of water flowing, the excess water flows above ground down the rock-lined channel that leads to the swallet. See trail map on Sign 1 for water flow.

Ensor Sink Natural Area Eroded Area Under Rock

Sinkholes, caves and karst

Sinkholes are common in Tennessee where the rock below much of the surface of the land is limestone.

As rainwater seeps down into the earth's surface and comes into contact with limestone, chemical reactions cause the limestone to slowly dissolve. As water continues to flow through holes that were created as the limestone dissolved, the holes become larger. Some small holes eventually become caves.

"Karst" refers to a geographic area with soluble rock, like limestone, underneath it. Karst is characterized by sinkholes, caves and an underground drainage system.

Cookeville is built on karst, and there are two, known, major cave systems beneath the City of Cookeville. Ensor Sink is part of one of those systems, and the other includes several caves in the Capshaw Cave system. See maps on Sign 3.

Ensor Sink Natural Area Low Point of the Sink

Sinkholes or "sinks"

Sinkholes, also called "sinks" are the characteristic landform of karst. Most sinks, known as "solution sinkholes," form as the limestone dissolves, creating sunken areas in the land surface. Other sinks, known as "collapse sinkholes," form when caves collapse and suddenly drop a portion of the land surface above.

The outer edges of sinkholes are normally round or oval, and their bottoms are either bowl or funnel shaped. When water drains into a sinkhole, it works like a funnel to feed the water into caves and underground streams below. Litter and pollutants that are in the water are also carried underground.

For generations, people have thoughtlessly dumped their trash into sinkholes and streams. Ensor Sink is no exception.

Based on the trash items they found, cavers who explored the Tires-To-Spare Cave determined that the water flowing into that cave came from Ensor Sink. They named the cave "Tires-To-Spare" because they found over 30 tires in it. They also found a shopping cart that had come all the way from a store at the northern end of the Breedings Mill Branch canal on Willow Avenue.

Ensor Sink Natural Area Tree Fallen on Fence

DANGER

Beware of flooding!

Ensor Sink and other sinkholes can be dangerous when it rains. Flooding has been forceful enough to take large, heavy trash items like grocery carts, office chairs, bedsprings, bicycle frames and tires deep into the underground cave system. That is why the channel and sinkhole are enclosed by a fence.

When flooding occurs, the strong, flowing water can rise even higher than the fence. So, stay safe. DO NOT ENTER FENCED-IN AREA AT ANY TIME.

DO NOT STAY IN ENSOR SINK NATURAL AREA DURING HEAVY RAINS.

Photographs of flooding, on Sign 2, by R.C. Finch

Where water drains
from this area of Cookeville


Ensor Sink Natural Area Sign 3 Text from Sign Number 3:

All of the rain that falls onto the land area shown in blue on these maps flows to the same point. This area shows several small, subwatersheds within Cookeville city limits. The darker blue subwatershed drains into Ensor Sink. See Sign 4 for more information about watersheds and subwatersheds.

Stormwater flows above ground in streams and rivers, and below ground through sinkholes to caves and underground streams. See Sign 2 for more information about karst.

Subwatersheds that flow into Pigeon Roost Creek

Ensor Sink drains an 816 acre area.

Water that flows into Ensor Sink drains through an inaccessible cave that eventually connects to Tires-To-Spare Cave.

At the downstream end of Tires-To-Spare Cave, all of the water that has drained from the subwatersheds around Ensor Sink and all of the water that has drained from the subwatersheds around the Capshaw Cave system, flow together. See Sign 4 for more information about subwatersheds.

From this point, the water drains into Arnent Cave then resurfaces at the headwaters of Pigeon Roost Creek. Pigeon Roost Creek flows into Falling Water River, which drops over Burgess Falls into Center Hill Lake. The City of Cookeville draws its public water supply from Center Hill Lake.

Work by members of the Upper Cumberland Grotto of the National Speleological Society is gratefully acknowledged. (Similar Upper Cumberland Grotto site)

Basins, watersheds and subwatersheds


Ensor Sink Natural Area Sign 4 Text from Sign Number 4:

How water flows

Water flows from the highest point to the lowest point because of gravity. So when a drop of rain falls onto your roof, it joins with the other drops, then flows down off your roof and onto the ground. Some of the water soaks into the soil. The water that does not soak into the soil continues to flow over land into a stream or sinkhole, then into a river.

The land area these combined raindrops drain from is called a "watershed." A watershed is the land unit that drains into a sinkhole, stream, lake, river or other body of water. Water can be poured onto the ground anywhere in a watershed, and it will flow into the lowest body of water to a single point in the watershed.

Basins, watersheds and subwatersheds

Basins include watersheds and smaller subwatersheds. As you can see from the map at left, the state of Tennessee spans over three major basins. These three basins include 56 smaller watersheds, but these can be divided into much smaller watersheds, or subwatersheds.

Rain from watersheds and subwatersheds within a basin all flow into the same body of water. The geographic boundaries of watersheds are their highest elevation points. They do not stop at state and county borders.

Ensor Sink Natural Area Rock Creek Bed Before Sink

The Caney Fork Watershed

Most of Putnam County is located in the Caney Fork Watershed, which is part of the Cumberland River Basin. All of White and DeKalb Counties are in the Caney Fork Watershed, as are parts of Putnam, Smith, Cumberland, Wilson, Cannon, Warren, Van Buren, Bledsoe and Sequatchie Counties.

Ensor Sink Natural area is in a subwatershed of the Caney Fork Watershed.

For a detailed map of highlighted subwatersheds, see other sign.

You and your watershed

Most of us who live in Cookeville live in the Caney Fork Watershed. Keeping the Caney Fork Watershed healthy is vital to our environment, economy and future generations.

Scientists and community leaders now recognize that the best way to protect water resources is to manage them withing each watershed. Each person's and business' activities within the watershed affects the quality of the drinking water supply within the watershed and downstream from the watershed. People's activities also impact the quality of water that fish and wildlife need to survive, and the quality of water for recreational use.

There are many things you can do to protect your watershed. Support the preservation of natural "green" areas in your community and reduce the amount of paved surfaces. Also, support preserving natural areas around environmentally sensitive features like streams and sinkholes.

For more information about how you can reduce water pollution and protect your watershed, contact the Cookeville-Putnam County Clean Commission.

Ensor Sink Natural Area End of Drainage Canal

What's in rainwater runoff?

Rainwater that flows over the ground into streams and lakes is called "runoff." Runoff can carry sediments, heavy metals, organics, nutrients, bacteria and viruses, herbicides and insecticides, and oils and greases that can pollute water above ground and below ground.

When rainwater "runs off" across solid surfaces such as parking lots and roads, most of the pollutants that are on those surfaces wash off and are carried into sinkholes and streams. When rainwater runs off across land that is covered with plants and soild, less pollutants are washed into sinkholes and streams. Thus, water that has fallen onto natural areas usually has fewer pollutants in it by the time it flows into bodies of water.

Polluted runoff does not stop at property lines. So, if you dump used motor oil on the ground or use too much fertilizer on your lawn, those pollutants wash into your neighbor's property and eventually into a sinkhole or stream.

Be a good neighbor. Keep your watershed clean.


Thanks to Cookeville, Tennessee for the park, trails and informative signs.

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